Tuesday, 21 July 2015

Reports of the Trace Fossil Climactichnites found in Central Texas

The title for this posting is based in part on a poster presentation at a recent Geological Society of America Conference:  the South-Central Section - 49th Annual Meeting held on March 19 and 20,  2015.  Lydia G. Roundtree of the University of Texas of the Permian Basin at Odessa, Texas presented a paper entitled “New Locality of the Trace Fossil Climactichnites in Central Texas” in which she noted that “The occurrence of Climactichnites is mostly confined to the north eastern part of North America.” and reported that “A possible new location of the tracks has been found in the central region of Texas. This new location is currently being researched by students at the University of Texas of the Permian Basin.”

See: https://gsa.confex.com/gsa/2015SC/webprogram/Paper254211.html

Unfortunately, she has not uploaded her poster and it is not possible to see the tracks.  Further, the  abstract does not give the rock type, age of the rocks or the exact location.   I am curious to see the results of the promised further investigations.  It will be an exciting development if her tracks are confirmed as Climactichnites. 

Interestingly, Lydia Roundtree  is not the first to report Climactichnites from Texas.   When I researched Cambrian rocks in central Texas I was taken to various publications describing the rocks from the Llano region of Texas.    A quick reading of a few of the publications disclosed that in 1977 Virgil E. Barnes and W. Charles Bell reported, when describing the Cambrian Hickory Sandstone Member of the Riley Formation,  that “Climactichnites(?) trails 4 inches wide are exposed in the bed of the Treadgill Creek (between 237 and 239 feet in line of section); such trails have not been seen elsewhere in the Llano region.”

[Virgil E. Barnes and W. Charles Bell, 1977, The Moore Hollow Group of Central Texas, Report of Investigations No. 88, Bureau of Economic Geology, The University of Texas at Austin, at page 77]

In addition, I believe that there are other references to Climactichnites from Texas in this and earlier reports.   At pages 123 and 124 of  the 1977 publication  Barnes and Bell   refer to “Climactonites” in combination with  Cruziana from the Hickory Sandstone Member.   I believe that they are misspelling Climactichnites as Climactonites.    In two earlier publications by the same authors, when describing the same rocks, they also refer to Climactonites.  See:

“These fossils occur above sandstone which is barren except for lebenspuren, such as Cruziana, Climactonites, and various other forms.”
W. Charles Bell and  Virgil E. Barnes,  1972
Cambrian History, Llano Region, in Virgil E. Barnes, W. Charles Bell, S.E. Clabaugh, P.E. Cloud, Jr., R. V. McGehee, P.U. Rodda and Keith Young, Geology of the Llano Region and Austin Area, Field Excursion, Guidebook Number 13, Bureau of Economic Geology, The University of Texas at Austin, at page 24

“These fossils occur above sandstone which is barren except for Lebenspuren, such as Cruziana, Climactonites, and various other forms.”
W. Charles Bell and  Virgil E. Barnes,  1962
Cambrian History, Llano Region, in Geology of the Gulf Coast and Central Texas, and Guidebook of Excursions, published by the  Houston Geological Society for the 1962 Annual Meeting of the Geological Society of America, Edited by E. H. Rainwater and R. P. Zingula, at page 79
archives.datapages.com/data/hgssp/data/013/013001/pdfs/79.pdf

By far the best reference to the environment of the Hickory Sandstone, and one that confirms that Bell and Barnes were identifying Climactichnites,  is a Masters  thesis submitted to the University of Texas at Austin in 1975 by Frank Gary Cornish entitled “Tidally influenced deposits of the Hickory Sandstone, Cambrian, Central Texas”.   He places the trackway Climactichnites in context with other trace fossils and in an environment that sounds much like that of the Nepean Formation of the Potsdam Group.   Part of his abstract is as follows:

“ The six lithofacies of the Hickory Sandstone were deposited as nonbarred tidally-influenced or estuarine-related equivalents to deposits of Holocene environments. Outer estuarine tidal channel-shoal deposits display abundant channel fills of large-scale foresets, parallel bedded sandstone, and minor siltstone. Trilobite trackways (Cruziana) and resting traces (Rusophycus) occur in these deposits, associated with U-shape burrows (Diplocraterion and Corophioides). Deposits of open coast sandy tidal flats display upward-fining character, medium-to large-scale festoon crossbedding, abundant small-scale ripple bedforms of all types, and mudcracks. These deposits include the U-shape burrows, Corophiodes, and the trackway, Climactichnites. Deposits of inner estuarine tidal channels and tidal flats display upward-fining character, wavy-lenticular bedding, bimodal paleocurrent patterns, and the resting trace, Pelecypodichnus. All of these deposits prograded as a unit until sea level rise shut off sediment supply. Progradation of tidal channel and shoal sediments was renewed. These deposits are festoon crossbedded hematitic sandstone with wavy-lenticular bedding and abundant fossil debris. Storm energy funneled through tidal channels deposited crossbedded sandstone onto the nearshore inlet-influenced shelf. Final Hickory deposits and initial Cap Mountain deposits were storm-dominated, burrowed and laminated calcitic shelf sands.

Frank G. Cornish’s thesis can be downloaded from a link at: http://repositories.lib.utexas.edu/handle/2152/20401

A photograph of Climactichnites, a specimen found in Gillespie County, appears at page 43 as Plate II D of his thesis.  It looks very much like Climactichnites to me.  

Mr. Cornish mentions at page 9 of his thesis that “The trace fossils Cruziana and Climactichnites were first recognized by Bell and Barnes (1961).”  This is a reference to the following paper:

Bell, W.C. and Barnes, V.E., (1961), Cambrian of central Texas: Internat. Geol. Cong., 20th, Mexico, 1956, El Sistema Cambrica, su paleogeographic y el problema de su base, Tomo III, p. 484-503.   (I have not yet found that paper.)

I view the identification of Climactichnites from Cambrian rocks of Texas as an exciting find, as Climactichnites has wider range than I had expected and is not just confined to  eastern  North America .

Christopher Brett
Perth, Ontario

Update:  July 23, 2015

I located Frank Cornish in Corpus Christi, Texas where he is the principal of Imagine Resources, LLC, a company that specializes in generating South Texas oil and gas prospects.   Frank has generously  given me permission to reproduce his photo of the trace fossil Climactichnites on my blog.  His photo is reproduced below.





It certainly looks like the surface trace Climactichnites wilsoni Logan 1860– a trackway consisting of lateral ridges between which are undulating transverse bars and furrows.

In the text of his thesis Frank Cornish provides this description for the photo: Portion of the Epichnial trail, Climactichnites, from middle rippled unit of burrowed sandstone facies, section GI-CR, Gillespie County, scale:   bar=5 cm.  

Unfortunately, he no longer has the ichnofossils from his thesis.  However, he does have the original negatives for the photographs appearing in his thesis.

++++++++
Added July 30, 2015:

Frank Cornish mentioned that the trace fossil Climactichnites wilsoni was found in the Cambrian Hickory Sandstone of Texas in an article published in Palaios in 1986, where he commented:

“The upper, burrowed unit is usually intensely bioturbated and has a massive if mottled appearance resulting from an extremely high density of Diplocraterion habichi burrows.  Other trade fossils in this facies are Climactichnites wilsoni and Planolites monatus.  No body fossils are present.  The trace fossils are dominated by Diplocraterion, ....  The vertical sequence of sedimentary structures, sedimentary textures, and biogenic structures demonstrates that this lithofacies accumulated on moderate-energy intertidal sand flats and intertidal sand bars...””

Frank G. Cornish, 1986,
The Trace-Fossil Diplocraterion: Evidence of Animal-Sediment Interactions in Cambrian Tidal Deposits, Palaios, Vol. 1, No. 5 (Oct., 1986), pp. 478-491 at page 481

++++++++++++++++++++++++++++
Those with a  new found  interest in the Hickory Sandstone should look at the following field trip guide:

www.geology.sfasu.edu/TASGuidebook2013.pdf
R. LaRell Nielson and Chris A. Barker, 2013
Geology of the Western Llano Uplift, Fredericksburg to Mason, Texas
Texas Academy of Science, 2013, Field Trip, 36 pages.

Stop 2 covers “Exposures of the Cambrian Hickory Sandstone are seen along Crab Apple Creek...  The Hickory Sandstone at this location contains excellent sedimentary structures such as mudcracks, a wide variety of ripple marks and trough cross bedding.”   Crab Apple Creek is in Gillespie County, and this stop could be at the outcrops that appear as  photographs in Plate II in Frank Cornish’s thesis and are the “middle rippled unit of burrowed sandstone” where he found Climactichnites.

Figure 07 in the field trip guide is a photograph with the caption “ Exposures of the Hickory Sandstone along Crab Apple Creek contain well developed trough cross-bedding, ripple marks and mudcracks deposited during the Cambrian System in a beach environment.”   

Figure 08 in the field trip guide shows “Ripple Marks in Hickory Sandstone along Crab Apple Creek” in Gillespie County  and looks like the outcrop that appears as the photograph in Plate IIG in Frank Cornish’s thesis, which he identified as “slightly sinuous bifurcating current ripples from the middle rippled unit of burrowed sandstone facies, Section G1-CR, Gillespie County."

Figure 09 in the field trip guide shows “Mudcracks in Hickory Sandstone along Crab Apple Creek south east of Enchanted Rock Natural Area.” and looks like the outcrop that appears as the photograph in Plate IIC in Frank Cornish’s thesis, which he identified as“Mudcracks form middle rippled unit of burrowed sandstone facies, section GI-CR, Gillespie County.”

++++++++++++++++

Not surprisingly, the Dresbachian (late Cambrian) age attributed to the Hickory Sandstone of Texas overlaps the Furongian (late Cambrian) age attributed to the rocks of Ontario, Quebec, New York, Missouri and Wisconsin where Climactichnites has been reported.   (What I find truly interesting is that in the late 1800's Charles Doolittle Walcott identified the sandstones of the Llano area of Texas as Upper Cambrian and called them Potsdam sandstone as he had sandstones in New York, Missouri and Wisconsin.)

Thursday, 16 July 2015

Burrows or Not Burrows - Part 2

Below are photographs of three more specimens from the Potsdam Group sandstones.

Specimen 6 -  Same sandstone as produced the Protichnites trackways mentioned in my blog posting from July 9, 2013 - Likely the Nepean Formation of the Potsdam Group





The specimen is about three feet wide and over four feet long.  The photograph was taken using the zoom feature on my camera.

In the upper left corner the chevron pattern and absence of lateral ridges suggest that this could be the burrowing trace fossil Climactichnites youngi as the bars in the photograph  compare favourably with the bar bifurcations  in Figures 11 A & B  in Getty and Hagadorn, 2009, with Figures 23,  41 and 48 in Yochelson and Fedonkin, 1993, and with the photographs of Climactichnites youngi in Figures 3.B and 3.C in Seilacher and Hagadorn 2010.   Another interpretation is that the outcrop records wave interference ripples.   (Interfering waves can make just about any pattern, including chevrons.   See for example figure 3.C in Hagadorn and Belt, 2008 .)   

I expect that most people would want to get a closer look at the specimen before making a positive identification.     Unfortunately this specimen is at the top of an unstable blast pile at an active quarry, doesn’t meet my three basic criteria for collecting (1. Can I lift it; 2. Will it fit in the trunk of a Hyundai Accent; 3. Can I park my car close enough that I can carry it to the car), and will probably be crushed into gravel by the middle of next week. 

Specimen 7 - Greyish, pink and buff sandstone, a loose specimen, found where the Hannawa Falls Member of the Covey Hill Formation of the Potsdam Group outcrops  


 





This is interesting as it looks like a trackway, lacks chevrons, arguably has a ridge at  each edge (but not the prominent ridges for Climactichnites wilsoni), but the rock may not be the Nepean Formation.   It was a loose specimen found in a part of a quarry where only the Hannawa Falls Member of the Potsdam outcrops.  The trackway is consistently 5 inches (12 cm) wide and compares favourably with the photographs of Climactichnites youngi in figure 3.B and 3.C in Seilacher and Hagadorn 2010.   If it is Climactichnites, and the rock is not Nepean Formation, then it is out of time as all previous specimens of Climactichnites from the Potsdam Group have been found in the Nepean Formation or the equivalent Cairnside in Quebec or Keeseville in New York State.   The specimen lacks barred chevrons,  but Getty and Hagadorn 2008 define Climactichnites youngi as “Burrows occurring within beds (may be inclined to and crosscut bedding) or at bed interfaces, consisting of undulating bars and furrows that are often oriented at a high angle to the direction of travel. Lateral ridges absent.” and provide the description “Transverse bars straight, sinusoidal, V-, U-, or stitch-shaped.  Straight bars can be perpendicular or at an angle to direction of travel; V- and U-shaped bars most often open in direction of travel. Bars often exhibit bifurcation  and sometimes have backwards-pointing lateral extensions ....”

Sir William Logan originally proposed that the Climactichnites wilsoni trackway was produced by "some species of giant mollusc" (Logan, 1860) and  "a species of mollusk"  (Logan, 1863); a view that is now commonly accepted.  Most now agree that a molluscan origin appears likely.

Specimen 8 - Greyish purple sandstone, a loose specimen,  the Hannawa Falls Member of the Covey Hill Formation of the Potsdam Group, the same sandstone as Specimens 1 and 2 from my last blog posting


 

 

 


This meandering pattern compares favourably with the meandering burrows of slug-like bulldozers that others have found in the Cambrian.  (Under mat mining?)

Christopher Brett
Perth, Ontario

References and Suggestions for Further Reading:

Ellis L. Yochelson and Mikhail A. Fedonkin, 1993,   
Paleobiology of Climactichnites, an Enigmatic Late Cambrian Fossil
Smithsonian Contributions to Paleobiology • Number 74
 Smithsonian Institution Press ,Washington, D.C. 1993
http://www.sil.si.edu/smithsoniancontributions/Paleobiology/pdf_lo/SCtP-0074.pdf

Patrick Ryan Getty  and J. Whitey Hagadorn, 2008,
Reinterpretation of Climactichnites Logan 1860 to Include Subsurface Burrows, and Erection of Musculopodus for Resting Traces of the Trailmaker
Journal of Paleontology 82(6):1161-1172.

Patrick Ryan Getty  and J. Whitey Hagadorn, 2009,
Paleobiology of the Climactichnites Tracemaker, Paleontology, Volume 52, pp. 753-778

James W. Hagadorn and Edward S. Belt (2008),
Stranded in Upstate New York: Cambrian Scyphomedusae from the Potsdam Sandstone, Palaios, v. 23, p. 424–441,  doi:10.2110/palo.2006.p06-104r

Adolf Seilacher and J. Whitey Hagadorn 2010
Early Molluscan Evolution: Evidence from the Trace Fossil Record
PALAIOS, September 2010, v. 25, p. 565-575,
doi: http://dx.doi.org/10.2110/palo.2009.p09-079r

M. Gabriela Mángano  and Luis A.  Buatois,  2015,
The trace-fossil record of tidal flats through the Phanerozoic: Evolutionary innovations and faunal turnover, in  McIlroy, D., ed., ICHNOLOGY: Papers from ICHNIA III:Geological Association of Canada, Miscellaneous Publication 9, p. 157-177

Sören Jensen,  Luis A. Buatois  and M. Gabriela Mángano , 2013,
Testing for palaeogeographical patterns in the distribution of Cambrian trace fossils, Chapter 5 in  Early Palaeozoic Biogeography and Palaeogeography, Geological Society, London, Memoirs 2013, volume 38, p. 45-58
doi: 10.1144/M38.5

Sir William E. Logan, 1860,
On the Tracks of an Animal lately found in the Potsdam Formation,  read before the Natural History Society of Montreal in June, 1860, published in volume V of The Canadian Naturalist and Geologist,  Pages 279-285

Sir William E. Logan,  1863,
Geology of Canada, Geological Survey of Canada, Report of Progress from its commencement to 1863, at pages 107-108, 

Tuesday, 30 June 2015

Burrows or Not Burrows?

Adolf  Seilacher (1925 – 2014) was a German palaeontologist who made major contributions to the study of trace fossils.  He is credited with advancing the concept that trace fossil assemblages are far from random, that the range of associated trace fossils is constrained by the environment of the trace-making organisms, and that the sedimentary environment  at its time of deposition can be deduced by noting the fossils that are in association with one another.  He taught at both the University of Tübingen and Yale University, wrote numerous papers, and authored a text book entitled Trace Fossil Analysis that I find helpful.   While his text book is designed to be used as a course book in conjunction with real material (including representative specimens and plaster casts), the book is so informative and well written that one cannot help but learn something every time it is opened.  There is however one comment in the book with which I disagree, namely Professor Seilacher’s introductory sentence to Plate 58 dealing with Synsedimentary Structures.   He states:

“The repetitive patterns of ordinary depositional structures, such as ripple marks in sand and sun cracks in mud, are too familiar from modern environments to be mistaken for fossils in the fossil record.”   

(Adolf  Seilacher, 2007, Trace Fossil Analysis,  Springer;  226 pages at page 166)

That statement is just not true:  I have no problem making those mistakes.  While there are many specimens that are obvious ripple marks or obvious sun cracks (what others call mud cracks or desiccation cracks), there are specimens where it is not clear whether one is looking at a trace fossil.

Below I provide a few problematic examples from the Potsdam Group sandstones and March Formation sandstone.  I periodically look at outcrops of  Potsdam Group sandstone and March formation sandstone in Lanark County and south of Perth down towards Kingston.   The outcrops are composed of any or all of (oldest to youngest):

(A) pink to brick red to burnt umber to greyish purple to almost  black (mostly) aeolian and (minor) fluvial sandstones – the Hannawa Falls Member of the Covey Hill Formation of the Potsdam Group;
(B)  white to buff to grey-green  fluvial and alluvial sandstones  and conglomerate (with minor aeolian sandstone) – the Chippewa Bay member of the Covey Hill Formation of the Potsdam Group; 
(C)  white to buff  marginal and shallow marine sandstones – the Nepean Formation of the Potsdam Group;
(D) white to buff to grey to black to green to maroon sandstones and siltstones - the March Formation

Below are photographs of specimens of those rocks.

Specimen 1.   Greyish purple sandstone, definitely the Hannawa Falls Member of the Covey Hill Formation of the Potsdam Group





When I first looked at the sample I assumed that I was looking at desiccation cracks, because the linear features on the surface intersect at almost right angles.  However if you look closely you will see (a) that the linear features are tubes that cross over one another, and (b) that the tubes pinch and swell.  This suggests that the linear features are backfill burrows. 

While the sample appears to be light grey, the rock is actually a darker grey purple colour.  I took the photograph near noon on a bright sunny day, and the sunlight washed out the photograph.

Sanford and Arnott 2010 report that the Hannawa Falls Member is divisible into two units:
- a lower unit of probable fluvial origin that is composed of brick-red shale, pink to maroon sandstone and quartz pebble to cobble conglomerate
- a dominant upper unit of eolian origin composed of red to pink quartz arenite containing a basal quartz-cobble conglomerate
Both units outcrop at this location.   It is not clear whether Specimen 1 is a sample from the lower or upper unit.

Hagadorn,  Collette  and  Belt  2011 discuss the rock and trace fossils in the Hannawa Falls Member in upstate New York, reporting that they examined mainly eolian beds but also found a minor subaqueous facies which they interpret as flooding in coastal dunes.   I assume that they were looking at the upper unit of the Hannawa Falls Member.  Based on trilobites found in underlying and overlying formations, they assign deposition of the Hannawa Falls Member in upper New York State to from early to mid-middle Cambrian time, which I assume to be the age of comparable rocks in Ontario.  They found Arenicolites U-shaped burrows in the subaqueous facies and Protichnites trackways, Diplichnites trackways, and Diplopodichnus trackways in the eolian beds. 

Specimen  2.   Greyish purple sandstone,  the Hannawa Falls Member of the Covey Hill Formation of the Potsdam Group




This is a polygonal pattern.   Many polygonal patterns are sun cracks (desiccation cracks).   Some polygonal patterns are trace fossils.  This one looks more like burrowing than a desiccation pattern.

Specimen 3.    Loose specimen of sandstone at quarry, either  Chippewa Bay member or Nepean Formation







To me this looked like either really bad burrows or poor desiccation cracks.  I passed this photograph to a geologist who has worked on these rocks and his comment was that the specimen “might include some burrows but much of the surface is reminiscent of the blocky texture produced by microfaulting of a water-stabilized sand dune surface.”  Not something that I can identify.

Specimen 4  - March Formation sandstone



When I saw this specimen I thought ‘mud cracks’ – the term that I had been using since high school.  I showed the specimen to two geologists and they told me that it couldn’t be a mud cracks because sand doesn’t shrink that much and it must be a  microbial mat shrinkage feature.  I sent the photo to a geologist who has written extensively on microbial mats and he told unless I could find the top slab and underlying slab (in order to ensure that no mud was present) I couldn’t identify this as microbial mat shrinkage feature.

Specimen 5.   Same sandstone as produced the Protichnites trackways mentioned in my blog posting from July 9, 2013 - Likely the Nepean Formation of the Potsdam Group




I have been assuming that this photograph shows ripple marks.   However, there is a chance that it could be the burrowing trace fossil Climactichnites youngi as the bars in the photograph, particularly the J-hooks at the end of the bars, compare favourably with the bar bifurcations  in Figure 5.3 in Getty and Hagadorn, 2008, and with Figure 43 in Yochelson and Fedonkin, 1993,
My suggestion notwithstanding, the ripple marks in the Potsdam can be quite variable, and the photograph is more likely to record ripples than to be a trace fossil.       

Christopher Brett
Perth, Ontario           


References and Suggestions for Further Reading:

Bruce V. Sanford and Robert W.C. Arnott, 2010
Stratigraphic and structural framework of the Potsdam Group in eastern Ontario, western Quebec, and northern New York State.  Geological Survey of Canada, Bulletin 597, 85 pages
publications.gc.ca/collections/collection_2010/nrcan/M42-597-eng.pdf

David G. Lowe,  Robert W. C. Arnott, and Bruce V. Sanford, 2013, 
Before the Great North American Carbonate Bank: A Complex Cambrian-Lower Ordovician Transgressive History Recorded in Siliciclastic Strata of the Potsdam Group, Southeast Laurentia
 Adapted from extended abstract prepared in conjunction with oral presentation at AAPG Annual Convention and Exhibition, Pittsburgh, Pennsylvania, May 19 -22, 2013
http://www.searchanddiscovery.com/pdfz/documents/2013/50859lowe/ndx_lowe.pdf.html   

Ellis L. Yochelson and Mikhail A. Fedonkin, 1993,    
Paleobiology of Climactichnites, an Enigmatic Late Cambrian Fossil
Smithsonian Contributions to Paleobiology • Number 74 
 Smithsonian Institution Press ,Washington, D.C. 1993
http://www.sil.si.edu/smithsoniancontributions/Paleobiology/pdf_lo/SCtP-0074.pdf

Patrick Ryan Getty  and J. Whitey Hagadorn, 2008,
Reinterpretation of Climactichnites Logan 1860 to Include Subsurface Burrows, and Erection of Musculopodus for Resting Traces of the Trailmaker
Journal of Paleontology 82(6):1161-1172. 
http://dx.doi.org/10.1666/08-004.1

J. Whitey Hagadorn, Joseph H. Collette  and Edward S. Belt,  2011,
Eolian-aquatic deposits and faunas of the middle Cambrian Potsdam Group: Palaios, v. 26, p. 314-334.       


Friday, 5 June 2015

Hunting for Whales in Eastern Ontario - Part 2

In my last posting I mentioned that Professor J. W. Dawson of McGill University had described the finding in 1882 of two vertebrae, a part of another, and a fragment of a rib of a Humpback whale in a ballast pit at Welshe's, on a line of the C. P. Railway, 3 miles north of Smith's Falls.  The bones were found in gravel at a depth of 30 feet and about 50 feet from the original face of the pit.

Last month I decided to visit the location.   I have to admit that I was not expecting much, based on my background research.   That is what I found: no historical plaque celebrating the finding of the Humpback whale, no train station, no train tracks, and little evidence that a gravel pit was close to the abandoned rail line.   I suspect that over time most of the gravel and sand was dug up and taken away.

I should note that Dawson misspelt the location: it is Welsh’s Station, rather than Welshe’s  (and certainly not Walsh Station as shown on the current official plan for Montague Township). 

Welsh’s Station is shown on the following extract that I’ve taken from a map of  Montague Township that appeared in the  Illustrated Atlas of Lanark County (maps from surveys under the direction of H.F. Walling,  Published by D. P. Putnam, Prescott, Canada West, 1868).






Illustrated Atlas of Lanark County, 1880; H. Belden & Co., Toronto.
http://digital.library.mcgill.ca/countyatlas/searchmapframes.php

Numogate, which appears on the map, still exists.  The road that runs from Smith’s Falls through Numogate is now Highway 15.  The road just south of Welsh’s Station, between Concession VII and Concession VIII is now called Ferguson Tetlock Road.    The railroad line identified on this extract as the Main Line of the Canada Central Railway, had become a line of C. P. Railway when Professor Dawson penned his article on the finding of the humpback whale.   Regrettably, the tracks have been torn up.   However, the track ballast identifies where the rail line used to run.  

The following is an extract from the map that is Schedule A to the Official Plan of the Township of Montague. 





This extract  provides the current names of the roads, shows the abandoned line of the Canadian Pacific Railway, misspells Welsh’s Station as Walsh Station, and shows a sand and gravel pit (marked with a “P”) off highway 15 just south of Numogate.  I visited that sand and gravel pit.  It appears to have been abandoned many years ago, and little if any sand or gravel is left to be taken from the pit.    Below is a photograph of the pit.





Dr.  A. P. Coleman  of the Ontario Bureau of Mines, and a professor of geology at the University of Toronto, visited the location in 1901.  He found more than I did.   Here is his description:

“The finding of bones of a whale near Smith's Falls in 1882 attracted much attention at the time. The bones, which were sent to Sir William Dawson and are now in the Peter Redpath museum at Montreal, consist of two vertebrae and a rib, the largest vertebra 11 inches in diameter and 7 inches in length ; the other 10 by 4.  It has been determined as Megaptera longimana, a species still common in the gulf of St. Lawrence and sometimes ranging some distance up the river. The bones are in good   preservation, but white and brittle from the loss of organic matter. Associated with them were shells of Macoma fragilis, a species common in the Saxicava sand. The find was made in a C. P. R. gravel pit at Welch's, three miles north of Smith's Falls, and, according to the railway levels, at a height of 440 feet above the sea. ...

    At present the gravel pit at Welch's shows a face of 52 feet consisting of coarse sand and gravel with many larger stones, the latter generally subangular or only partially rounded. Since the gravel pit has not been in use for some years the stratification is not well seen, sand having run down from above. No shells were found, but this was to be expected, since they tend to crumble when long exposed to the weather. The sand and gravel have not the look of the Saxicava sand near Ottawa, but are much coarser and less perfectly stratified; nor do they seem to have been formed on a beach. They run as a ridge having a general direction about 15 degrees east of north, not far from the same as the striae shown on well polished Potsdam sandstone a few hundred yards to the west, where 12 degrees east of north was observed. The gravel ridge has somewhat the look of a moraine and includes a shallow kettle hole with no outlet, just to the east of the highest part. The deposit seems to be a kame rather than a beach, the many large subangular boulders suggesting ice action. The ridge is not long enough or distinct enough to be an esker.

    The bones are said to have occurred 30 feet below the surface of the gravel, but apparently the carcass of the whale was enclosed in a beach deposit formed against the flank of the ridge in post-glacial times. As the level of the track at Welch's is 431 feet above sea, and the gravel rises at its highest part 52 feet higher as determined by hand levels the summit of the ridge is 483 feet above the sea. but the old beach probably 40 feet lower.”

A. P. Coleman, 1901, Sea Beaches of Eastern Ontario, Report of the Bureau of Mines, 1901, Province of Ontario, pages 215-227  at pages 216 and 2017.

The sand and gravel pit may  also have been described by A. Ledoux of the Ontario Bureau of Mines in 1918, as follows:

“There is some gravel near Smiths Falls which was extensively used by the railway companies as ballast....   The gravel pit owned by George Kerfoot, Smiths Falls, is in the township of Montague, lot 26, concession 8.  It is about 3.5 miles north of Smiths Falls, near the tracks of the Canadian Pacific railway.  The average dept of the pit is 10 feet, below which clay is found.  The material is about two parts of gravel to one of sand... There is an estimated reserve of three acres.”

A. Ledoux, 1918, Sand and Gravel in Ontario, Report of the Bureau of Mines, 1918, Province of Ontario, at page 61.

Two years ago Victoria Lee of the Ontario Geological Survey issued a report on the aggregate resources of Lanark County that included the gravel pits in the Township of Montague.  She discounts the Township of Montague as a significant source for sand and gravel, but does list eight licensed pits in the Township of Montague, including the pit south of Numogate, which is identified as pit 133 in her report and on her maps.   She describes the pit as covering 16.6 hectares, with a face height of 2-6 meters, with 20 -30 percent gravel and mentions that the “Pit has been developed in an ice-contact deposit.”    Below is part of her map showing the location of the licensed pit.  Interestingly, she shows two sand and gravel deposits close to what was Welsh’s Station: the first south of Numogate and the second northwest of Numogate.   




 (Victoria L. Lee,  2013, Aggregate resources inventory of the County of Lanark, southern Ontario: Ontario Geological Survey, Aggregate Resources Inventory Paper 189, 85 p.   
Her report can be downloaded from:
http://www.geologyontario.mndmf.gov.on.ca/mndmfiles/pub/data/imaging/ARIP189/ARIP189.pdf   )      
       
Map P2622 published three decades earlier by the Ontario Geological Survey shows four pits south of Numogate, including one to the north of Victoria Lee’s Licensed Pit 133 and just south of Ferguson Tetlock Road.  I did not find that pit.




G.A. Gorrell ;S. Margeson ;J. Lindablom ;R. Trotter, 1985,  Sand and gravel assessment, Lanark County, south half, Map P2622
URL: http://www.geologyontario.mndmf.gov.on.ca/mndmfiles/pub/data/imaging/P2622/P2622.pdf   

Christopher Brett
Perth, Ontario

Friday, 24 April 2015

Hunting for Whales in Eastern Ontario

I expect that everyone in Eastern Ontario with an interest in geology is aware that the Champlain Sea was a brackish arm of the Atlantic Ocean that flooded the depressed St. Lawrence Lowland following the retreat of the glaciers,  that leda clay, the cause of many landslides in Eastern Ontario, was deposited in the Champlain Sea, that numerous fossil fish have been found at Green’s Creek at the east end of Ottawa in nodules in the leda clay, and that fossils of seals and whales have been found in Champlain Sea deposits.   Those people will also have visited the Canadian Museum of Nature/Victoria Museum in Ottawa, probably on numerous occasions, and will have admired the fossils from the Champlain Sea on display at the museum.  This posting expounds on the whales that have been found in the Champlain Sea, with particular emphasis on those found in Eastern Ontario.

Five species of whales, four species of seals, walrus, and numerous species of fish are known to have existed in the Champlain Sea because of fossils that have been found in Ontario, Quebec, New York State and Vermont in the sediments left by the Champlain Sea .   In a paper published in 2014, when commenting on the mammals in the Champlain Sea, Richard Harington and his co-authors stated:

“Several species of whale, particularly those adapted to cool inshore conditions, lived in the Champlain Sea. Approximately 80% of whale specimens recorded from Champlain Sea deposits are white whales. Other whale species represented are humpback, bowhead, finback, and harbor porpoise.  Seals, particularly those adapted to breeding on pack ice, such as harp and bearded , and those adapted to breeding on land-fast ice, such as ringed , also lived in the Champlain Sea. An open coastal water species, the harbor seal has likewise been found near the southern margin of the sea.  Walruses, which tend to follow the pack-ice edge, have also been reported. These marine mammal fossils suggest the former presence of Arctic to boreal waters, with sea ice generally present.”  [Scientific Names and Citations Omitted.]
   
[C. Richard Harington,  Mario Cournoyer,  Michel Chartier, Tara Lynn Fulton,  Beth Shapiro, 2014,  Brown bear (Ursus arctos) (9880 ± 35 BP) from late-glacial Champlain Sea deposits at Saint-Nicolas, Quebec, Canada, and the dispersal history of brown bears, Canadian Journal of Earth Sciences, 2014, 51(5): 527-535,    http://dx.doi.org/10.1139/cjes-2013-0220 ]
       
Below I’ve provided information on ten of the whales found in Eastern Ontario.  Where available, I’ve used the reports by those who first described the specimens.   While I’ve entitled this posting “Hunting for Whales in Eastern Ontario”  I might more accurately have used the title “Happening Upon Whales in Eastern Ontario” as only two of the fossil whale occurrences in Ontario appear to have been found by someone out looking for fossils.   (Both Walter Billings, an architect, and Dr. Mark McElhinney, a dentist, who found two of the specimens,  were active members of  The Ottawa Field-Naturalists' Club.  Walter Billings in particular was well known as a collector of fossils.)  All of the rest of the fossils appeared while excavating sand and gravel, excavating clay for brick, or digging  wells.   I noticed a similar pattern when looking at the fossils of seals and walrus found in Champlain Sea sediments and the fossil whales found in the Champlain Sea deposits in Quebec, Vermont and New York State.   While a few specimens have been found when looking for fossils, the vast majority, and the most complete specimens, have been found by chance when excavating sand and gravel, excavating clay for brick, digging  wells or digging on farms.   However, I don’t expect that will stop me or anyone else from going out to look for a whale.
       

1.)  White Whale (Beluga) found at Cornwall, Ontario in 1870 


In a paper read before the Natural History Society, Montreal, on October 31, 1870  Elkanah Billings, Palaeontologist to the Geological Survey of Canada, described the finding of this fossil.  He then submitted an abstract of his talk where he mentioned:

"Several months ago, Mr. Charles Poole, of Cornwall, wrote to the Secretary of the Society that a large skeleton, resembling that of an Icthyosaurus, had been found in that neighborhood, by the men engaged in excavating clay for brick. In another letter he stated that Mr. T. S. Scott, architect, of this city, had procured the lower jaws. On receipt of this information, Mr. Billings called upon Mr. Scott, who very liberally presented the jaws to the Geological Museum. Mr. Billings then went up to Cornwall, and obtained from Mr. Poole the bones which were in his possession. These were discovered in the Postpliocene clay about sixteen feet below the surface. They are those of a small whale closely allied to the White Whale, Beluga leucas, which lives in the Northern seas, and at certain seasons abounds in the Gulf and lower parts of the St. Lawrence. The lower jaws are nearly perfect. The skull and upper jaws are much damaged and some  of the parts lost. Thirty-five of the vertebras, the two shoulder blades, most of the ribs, and a number of small bones were collected. The length of the animal was probably about fifteen feet. The lower jaws have the sockets of eight teeth upon the right side and of seven on the left. The number of teeth in the upper jaw could not be ascertained. ... The Cornwall locality is about half a mile from the railway station, sixty feet above the St. Lawrence, and over two hundred feet above the level of the sea.”
   
[Billings, Elkanah, 1870 , Canadian. Naturalist and Quarterly. Journal of  Science, vol. V, pp. 438-439)     https://archive.org/details/canadiannaturali05natu ]

Thirty-seven years later J.F. Whiteaves commented, when reviewing the White Whale specimens in the collection of the Geological Survey of Canada, that “By far the most perfect of these is the fine specimen from Cornwall in the museum of the Geological Survey  of Canada. It is a nearly perfect skeleton of an adult individual,  which, as now mounted, is a little more than twelve feet in length, though a few of the vertebrae are missing.” [Whiteaves, J.F., 1907,  Notes on the Skeleton of a White Whale,  Ottawa Naturalist, vol. xx, No. 11, pp. 214-216 page 214 ]

2.)  Humpback Whale found north of Smiths Falls, Lanark County, Ontario in 1882

 

 J. W. Dawson of McGill University in Montreal described the finding of this fossil as follows:

“These [bones]  were found, as I am informed by Archer Baker, Esq., General Superintendent of the Canada Pacific Railway, "in a ballast pit, at Welshe's, on the line of the C. P. Railway, three miles north of Smith's Falls, and thirty-one miles north of the St. Lawrence River, in the Township of Montague, County of Lanark. They occurred in gravel at a depth of 30 feet from the surface, and about 50 feet back from the original face of the pit.
... The bones secured consist of two vertebrae and a fragment of another with a portion of a rib, and others are stated to have been found. They are in good preservation, but have become white and brittle through the loss of their animal matter. On comparison with such remains of whales as exist in the Peter Redpath Museum, and with the figures and descriptions of other species, I have little doubt that they belong to the Humpback whale,... The larger of the two vertebrae, a lumbar one, has the centrum eleven inches in transverse diameter, and is seven inches in length. The smaller, a dorsal, is ten inches in its greater diameter, and four in length. Through the kindness of Mr. Baker the specimens have been deposited in the Peter Redpath Museum”

[ J. W. Dawson, 1883, On portions of the Skeleton of a Whale from gravel on the line of the Canada Pacific Railway, near Smith's Falls, Ontario, American Journal of Science, ser. 3, vol. XXV, p. 200)   https://archive.org/details/mobot31753002153036    The Canadian Naturalist and Quarterly Journal of Science, New Series,  Volume 10 pages 385-387
http://www.biodiversitylibrary.org/item/31810#page/405/mode/1up    ]
   

3.) White Whale (Beluga) found at Williamstown, Glengarry County,  about 10 miles north-east of Cornwall in 1901

Oliver P. Hay, of the Carnegie Institution in Washington, described the finding of this fossil as follows:
“ In Professor Perkins's paper just cited it is stated that Edward Ardley, assistant curator at Redpath Museum, McGill University, Montreal, had found here a few bones of a white whale, the hyoid, a few phalanges, and rib fragments. ... . From Mr. Ardley, through Mr. Arthur Willey, curator of Redpath Museum, the present writer has learned that these bones were dug up from a depth of 14 feet, in a well sunken in the Leda clay. Under the surface soil was a band of sandy clay containing shells of Saxicava and Mya. Beneath this was a stiff blue clay showing stratification and containing shells of Leda.”

[Oliver P. Hay, 1923,  The Pleistocene of North America and its vertebrated animals from the states east of the Mississippi River and from the Canadian provinces east of longitude 95 degrees,  Published by the Carnegie Institution of Washington, Washington, D.C., 499 pages, at pages 17-18.
https://archive.org/stream/pleistoceneofnor00hayouoft#page/16/mode/2up

4.) White Whale (Beluga) found in Pakenham Township, Lanark County  in 1906


J.F. Whiteaves,  staff  palaeontologist with of the Geological Survey of Canada, described the finding of this fossil as follows:   

“On the 5th of September, 1906, a skeleton, which is obviously  that of a very young individual of this same White Whale or Beluga, was found by Mr. Patrick Cannon, while digging a well on his farm, on lot 21 of the 11th concession of Pakenham, Lanark Co., Ont. The Rev. J. R. H. Warren, of the village of Pakenham, informs the writer that this skeleton was embedded in blue clay, fourteen feet below the surface, and that only a portion of it was dug out. In digging the well, he adds, some depth of blue clay was first bored through, then a mixture of clay and shells, in which the skeleton was found, was struck, and the excavation ended in more blue clay. The well has since been incased or lined with stone, and now contains a considerable depth of water, so that it may be somewhat difficult to dig out the remainder of the skeleton.

The bones that have been exhumed so far, from this excavation, with samples of the mixture of clay and shells in which they were found, have been kindly lent to the writer by Mr. Cannon. The former consist of a nearly perfect skull (with only a few of the teeth missing) and one of the tympanic bones, with most of the cervical vertebrae and three of the dorsals with some of their epiphyses. Or, as interpreted more definitely by Mr. L. M. Lambe, ot the skull, the left tympanic, the atlas, axis, third, fourth and fifth cervical vertebrae, and the second, third and fourth dorsal, with some of their epiphyses.”

[Whiteaves, J.F., 1907,  Notes on the Skeleton of a White Whale,  Ottawa Naturalist, vol. xx, No. 11, pp. 214-216 page 215    https://archive.org/details/ottawanaturalist20otta ]
   
Photographs of the Cranium (top view showing the blow hole) and mandibles for the White Whale (Beluga) found near Pakenham are Figure 28 at page 45 in the Royal Ontario Museum’s 1984  publication by Frances J.E. Wagner entitled Fossils of Ontario Part 2: Macroinvertebrates and Vertebrates of the Champlain Sea  https://archive.org/details/fossilsofontario02bolt

A photograph of the Cranium and lower jaws of the whale found near Pakenham  appears as Figure 5 at page 53 in Harington, C.R.  and Occhietti, S., 1988, Inventaire systématique et paléoécologie des mammifères marins de la Mer de Champlain (fin du Wisconsinien) et de ses voies d’accès,  Géographie physique et Quaternaire, vol. 42, n̊ 1, 1988, p. 45-64.
http://www.erudit.org/revue/gpq/1988/v42/n1/032708ar.html?vue=resume

In addition, a photograph of the Cranium and lower jaws appears in a history of Pakenham published by Verna Ross McGiffin (V. R. McGiffin, 1963, Pakenham, Ottawa Valley Village, 1823-1860, Mississippi Publishers, Pakenham, Ontario.)   

5.)  White Whale (Beluga) found in Ottawa East, Carleton County [Now falling within the City of Ottawa, Ontario]


In 1910, Mr. Lawrence M. Lambe, paleontologist with  the Geological Survey Branch of the Department of Mines, Canada reported  that Mr. A. Penfold  had presented to the Survey a caudal vertebra of Delphinapterus leucas, Pallas  which he had found at Ottawa East, at a depth of 25 feet, while digging a well.

[ L. M. Lambe, 1910, Summary Report of the  Geological Survey Branch of the Department of Mines, Canada. for 1909, at  p. 273  https://archive.org/details/summaryreportofg1909geol ]

6.)  White Whale (Beluga) found in 1913 at  Nepean Township, Carleton County [Now falling within the City of Ottawa, Ontario] 

In 1914, Mr. Lawrence M. Lambe of the Canadian Geological Survey, stated that  Walter Billings of Ottawa had presented to the Survey a caudal vertebra of Delphinapterus leucas found in Pleistocene gravel on lot 15, concession 5, of Nepean township. The locality is near Jock River, a stream which flows northeasterly and enters Rideau River about 11 miles south of Ottawa.
   
[Lawrence. M. Lambe, 1914, Summary Report of the  Geological Survey Branch of the Department of Mines, Canada. for 1913, at page 299.]
   

7.)  White Whale (Beluga) found in 1924 at a Sand Pit 5 miles South of Ottawa [Now falling within the City of Ottawa, Ontario]


Charles Mortram Sternberg, Assistant Biologist (the equivalent to a curator) to the National Museum of Canada, mentions:

“Scapula and four vertebrae of D. leucas from sand pits, 5 miles south of Ottawa, presented by Dr. Mark McElhinney in 1924.”

[C. M. Sternberg, 1951, White Whale and Other Pleistocene Fossils From the Ottawa Valley,
National Museum of Canada Bulletin 123, pages 259-261 at 259.]

8.)  Two White Whales (Belugas) found in 1948 at a Sand Pit  near Uplands Airport 5 miles South of Ottawa [Now falling within the City of Ottawa, Ontario]


Charles Mortram Sternberg, Assistant Biologist to the National Museum of Canada, mentions:

“On June 19, 1948, Mr. S. G. Carr-Harris telephoned the National Museum that the skull and partial skeleton of some fossil had been dug out of the R.R. Foster sand pit near Uplands Airport, about five miles south of Ottawa, by Mr. J. B. Rolland, the shovel operator.  The specimen, which proved to be the skeleton of a White Whale (Delphinapterus leucas), consisted of a splendidly preserved skull (minus lower mandibles), 20 vertebrae, several ribs, a scapula, humerus, radius, and various other bone fragments.  It is probable that the complete skeleton  was present originally but that part of it was removed with excavated material before the specimen was discovered.   The specimen was preserved near the center of a thick bed of fairly clear sand.  A few days later the lower jaw of a smaller individual was recovered from the same locality.”

[C. M. Sternberg, 1951, White Whale and Other Pleistocene Fossils From the Ottawa Valley,
National Museum of Canada Bulletin 123, pages 259-261 at 259.]

9.) Bowhead Whale Found at White Lake, near Arnprior, Renfrew County, Ontario in 1975   


This whale was found in by Clyde Kennedy who was looking for campsites of Paleo-Indians.   In the summer of 1975 he identified the sand and gravel deposit owned by John Hanson of White Lake village as an ancient shore surface that was worth investigating.   In an article published in 1977 in the Arnprior newspaper The Chronicle he mentions “Confirmation of this conclusion came on October 10,1975 when Allan Jones, while taking sand from the pit about eight miles southwest of Arnprior, found bones from the right fore fin of a bowhead whale.  Allan found some of the bones at the pit and others the next day when he was spreading sand he had delivered to a schoolyard in Renfrew.  Identification of the bones was made by Dr C R Harington, National Museum of Natural Sciences... [who ] told me the bones were from a mature bowhead whale, the mammal was probably between 40 to 65 feet long and weighed between 40 and 70 tons.” 

Further bones were found at the pit in 1977.  In the article Clyde Kennedy states “ I learned that Terry Bandy, while loading sand at the Hanson Pit on September 23 this year, had found three pieces of a large bone. His father, Glen Bandy, a Glasgow Station area farmer, kindly showed me the pieces, which totalled about seven feet in length.  I informed Dr Harington who visited White Lake with me and identified the find as a whale rib.  It was once longer than seven feet for a missing piece was not found... [On a subsequent visit, with further digging, we found and] completed the exposure of the nine-foot bone with trowels and paint brushes. I guessed it was a whale jawbone, which was later confirmed by Dr Harington.”
       
[Clyde C.  Kennedy, Nov 30, 1977, Whales bones found, The Chronicle.
http://www.historymuseum.ca/cmc/exhibitions/archeo/kichisibi/k300c-clydeswhale.shtml ]

Photographs showing the bones being dug up can be seen in this article.

A drawing of the skeleton of the bowhead whale showing the parts recovered at White Lake  appears as Figure 7 in Harington and Occhietti, 1988, at page 55.

+++++++++++++++++++++++++++++++++++++++++++++

A Map Showing  Localities Where Fossils of Whales, Seals and Walrus have been Found in Champlain Sea Deposits


On the following map I’ve plotted the localities where fossils of whales, walrus and seals  have been found in Champlain Sea sediments.   I believe that I’ve plotted all of the whales and walrus. There were numerous fossil seals found at locations in Ottawa and Montreal, and I may not have them all.








 That map is based on Figure 4 that is found in the following paper:
Steadman, D.W., Kirchgasser, W.T. and Pelkey, D.M., 1994. A Late Pleistocene white whale (Delphinapterus leucas) from Champlain Sea sediments in northern New York, p. 339-345. In E. Lending, ed., Studies in Stratigraphy and Paleontology in Honor of Donald W. Fisher. New York State Museum Bulletin 481, 380 p.    Their drawing is said to be modified from the following two papers:

C. R. Harington et Serge Occhietti, 1988, Inventaire systématique et paléoécologie des mammifères marins de la Mer de Champlain (fin du Wisconsinien) et de ses voies d’accès,  Géographie physique et Quaternaire, vol. 42, n̊ 1, 1988, p. 45-64.
http://www.erudit.org/revue/gpq/1988/v42/n1/032708ar.html?vue=resume

C. R. Harington,  1989, Marine Mammals of the Champlain Sea, and the problem of whales in Michigan. Geological Association of Canada, Special Paper 35: 225-240.

I have not yet been able to find Harington, 1989.

Steadman,, Kirchgasser, and Pelkey’s Figure 4 plots fossil records of the White Whale (Beluga) from the Champlain Sea, shows the shoreline of the Champlain Sea at its maximum extent,  overlying major modern bodies of water including Lake Ontario, the St. Lawrence River, the Ottawa River and Lake Champlain.  To their map I’ve added the localities of the occurrences of the Humpback Whale, Bowhead Whale, Finback Whale,  Harbour Porpoise and seals referenced in Harington, C.R. and Occhietti, S., 1988.

I also added the occurrences of Walrus fossils found at Saint Julienne de Montcalm, Quebec  and St. Nicolas, Quebec mentioned in:

M.A. Bouchard, C.R. Harington and J.-P. Guilbault, 1993,  First evidence of walrus (Odobenus rosmarus L.) in Late Pleistocene Champlain Sea sediments, Quebec, Can. J. Earth Sci. 30, 1715-1719   http://www.nrcresearchpress.com/doi/pdf/10.1139/e93-150

Jean-Pierre Guilbault, 2013, New Acquisition: A walrus skull from St. Nicolas, Bulletin of the MPE, March 2013, pages 1-2  http://www.mpe-fossils.org/resources/Bulletin_MPE_April_9_2013.pdf


I also added the additional occurrences of  White Whales  referenced in:
C. Richard Harington, Serge Lebel, Maxime Paiement, Anne de Vernal, 2006,  Félix: a Late Pleistocene White Whale (Delphinapterus Leucas) Skeleton From Champlain Sea Deposits at Saint-Félix-de-Valois, Québec, Géographie physique et Quaternaire, Volume 60, No,  2,  p. 183-198    http://id.erudit.org/revue/gpq/2006/v60/n2/016828ar.html?lang=es

To my knowledge Félix, found north of Montreal, and Charlotte, the state fossil of Vermont, are the only whale fossils from the Champlain Sea  that are referred to by a person’s first name.

Christopher Brett
Perth, Ontario   





Tuesday, 17 March 2015

Dr. Edward Van Cortlandt, M.D., (1805-1875) of Bytown and Ottawa, Surgeon, Field Naturalist, Museum Curator and Amateur Geologist



    “ This gentleman is well known in scientific and other circles as a mineralogist, geologist, botanist and physician of considerable repute in the Province, and as one who has done much to advance the interests of the Ottawa country, in the capital of which he has resided for many years. ... He has, at great expense, had constructed the best private archaeological and geological museum in Canada, an object of great attraction to all who visit Ottawa; ” 

    ( Henry James Morgan, 1862, Sketches of Celebrated Canadians: And Persons Connected with Canada,  Hunter and Rose, Co., London, 779 pages at page 750)

In earlier postings I mentioned three amateur geologists  who were instrumental in collecting mineral and fossil specimens in Upper Canada/Canada West in the years preceding Confederation and who provided assistance to the Geological Survey of Canada.  These were Dr. James Wilson, M.D.,  (1798-1881) of Perth, Sheriff Andrew Dickson (1797 - 1868) of Pakenham and Dr. Andrew Fernando Holmes, M.D.,  (1797 -1860) of Montreal. 

Another individual who helped by collecting specimens and educating the populace on geology  was Dr. Edward Van Cortlandt, M.D., (1805-1875)  of Bytown/Ottawa.    Edward Van Cortlandt (sometimes spelt van Cortland or van Courtland or Vancortlandt) was born in Newfoundland to a military family.   Later his family moved to Quebec.   He studied medicine with the military in Quebec and later in London, England where he passed the examinations of the Apothecaries Hall and Royal College of Surgeons.  He arrived in Bytown in 1832 as the medical officer for the troops, before setting up in private practice (while continuing his association with the military).  He practiced medicine in Bytown and Ottawa for 43 years until his death in 1875.  His funeral took place with full military honours.

Dr. Van Cortlandt is generally considered to have been the best physician in the Bytown/Ottawa area of his era, was known as a friend of the poor,  but appears to have had a blunt/brusque manner.   He was a true field naturalist and had  interests in geology, archeology and botany, and wrote articles and gave talks on those subjects.     He maintained a  museum in  his home with collections of minerals, fossils, Indian artifacts, and birds and animals that he had shot, that was considered to be one of the best in Canada.  He was an active member of the Bytown Mechanics Institute, the Bytown Mechanics' Institute and Athenaeum , the Silurian Society of Ottawa, and the Ottawa Natural History Society.   In addition to maintaining the museum in his own home, for at least a six year period he was the curator of the museum of the Ottawa Natural History Society. 

 An obituary published in the local press on his death mentions:

“The Doctor is considered to be the first physician in medical skill in this part of the country.  He was a man of quick perceptions, and rather a blunt manner but underneath lay a warm heart to the poor, of which his talent was always at their command.   Another characteristic of the man was in what he believed to be his duty, he feared not the face of man.  One instance of the above was a letter published by us in the “Banner,” some years back against the County Fathers for their treatment of prisoners in the jail, termed Calcutta Black Hole. The poor have lost a warm friend and Ottawa has lost her best physician.”

(Quoted in Andrew Wilson, 1875, A History of Old Bytown and Vicinity, Now the City of Ottawa, at page 58)

In 1903, Dr.  H. Beaumant Small described Dr. Van Cortlandt as follows:

“Dr. Van, as he was generally known, acquired a large practice, and his reputation spread far and wide.   ... He was odd and eccentric in his manner and his dress – brusque, sharp and even rough in his speech. ... He was impetuous and quick-tempered; ever ready to imagine a slight and equally prepared to resent a fancied grievance.  Beneath the rough exterior there was kind and sympathetic nature, and many instances were recited of his kindness and generosity to the poor.  He himself worked long and hard, yet acquired but little of this world’s wealth. ... My own distinct recollections are of his rapid and sprightly walk, and his habit of snatching boys caps as he passed them by...
    ... He was the first surgeon to the General Hospital, and had full charge of that institution for many years.  He was consulting surgeon at the Protestant Hospital, and held that position at the time of his death.  He was surgeon to the gaol, coroner and surgeon to the field battery.
     In addition to his professional reputation, he was known as a geologist of marked ability, and contributed papers and lectures on the subject.  He studied the mineralogy and paleontology of this district, and accumulated a really valuable collection, for which he had fitted up a room in his residence.”

(Dr. H. Beaumont Small, 1905, Medical Memoirs of Bytown, An Address delivered  before the Ottawa Medico-Chirurgical Society, Nov. 5, 1903, Montreal Medical Journal 34, No. 8: 549-560 at pages 556-557).
http://eco.canadiana.ca/view/oocihm.8_05178_206/2?r=0&s=1
http://www.biodiversitylibrary.org/

Because he was an influential citizen, there is a fair amount written about Dr. Van Cortlandt.   The best description of his life is provided in a fifteen page pamphlet entitled “Dr. Edward Van Cortlandt Surgeon, 1805-1875" written by Margaret E. Moffatt and published in 1986 by The Historical Society of Ottawa .    She mentions that it was Dr. Van Cortlandt that alerted the authorities to the 1834 outbreak of Cholera in Bytown, and that in 1847 when a typhus epidemic broke out in Bytown Dr.  Van Cortlandt was one of the physicians who looked after the diseased immigrants.  She also points out that “In several issues of the Bytown Gazette, starting in January 12, 1836, Dr. Van Cortlandt placed an advertisement stating that he would vaccinate for small pox, free of charge.  He was thus one of the first of our public-spirited physicians trying to persuade the people of Bytown to take advantage of medical advancements.”

Dr. Van Cortlandt’s Lectures and Papers


Above I mentioned that Dr. Van Cortlandt was an active member of the Bytown Mechanics Institute, the Bytown Mechanics' Institute and Athenaeum,  the Silurian Society of Ottawa, and the Ottawa Natural History Society.    He gave lectures to each of those bodies.
               
Dr. Van Cortlandt’s geological papers that survive are:
   
An epitome of a lecture on Ottawa productions –  delivered before the Bytown Mechanics' Institute and Athenaeum on Tuesday, November 15, 1853,
1853 - Published under the Auspices of the Institute, The Citizen, Bytown
https://archive.org/details/cihm_55512
1853 - Published in The Canadian Journal of Industry, Science and Art, Volume II, pages 112-6
1854 - Published by George Sparks, Bookseller, Montreal with the title The Productions of the Ottawa District of Canada   https://archive.org/details/cihm_35799

Observations on the Building Stone of the Ottawa Country  –  an Abridgement of a Lecture
Delivered before the Ottawa Silurian Society, the 15th November, 1858 - Published under the auspices of the Ottawa Silurian Society, and by order of the city council.

https://archive.org/details/cihm_47986
   
An Essay on the Native Compounds and Metallurgy of Iron, Especially in Connection With The Ottawa Valley;  read before the Natural History Society of Ottawa, on Friday, December 28th,
 1866
1867 - published by The Ottawa Citizen, Ottawa     https://archive.org/details/cihm_40500

The lecture on Ottawa Productions is interesting.   Not only did it enjoy three printings, but it discusses iron deposits in the Ottawa valley, graphite deposits in Hull and in Eastern Ontario, Galena deposits near Kingston and on the Ottawa, native copper deposits in Canada,  briefly mentions other refractory materials and minerals, and describes various trees of the Ottawa.

His lecture entitled  Observations on the Building Stone of the Ottawa Country discusses granite, syenite, Potsdam sandstone, Chazy sandstone, Calciferous Sand Rock, limestone, and marble.

+++++++++++++++++++++++++++++++++++
   
A number of Dr. Van Cortlandt’s articles and speeches on other topics have been preserved and are available, including:

Notice of an Indian Burial Ground, The Canadian Journal of Industry, Science and Art, 1853, volume I, pages 160-161. This describes his two day dig in 1843 close to Bytown and the items that he found including bones, a few implements and weapons.

Fishes of the Ottawa, a Digest of an essay on the fishes of the Ottawa River, and its tributaries and some of the contiguous lakes – read before the Natural History Society on Friday, 24th November, 1865.   Ottawa Citizen, Nov. 29, 1865. 
 [He is also suspected to have written:  Notes on the lakes and lake fishes in the vicinity of Ottawa, Canada West No. 1 — Minnow lake by a member of the Isaac Walton Club (Dr. Edward Van Cortlandt?) Ottawa Citizen, June 21, 1865.]

An Essay on Entozoa, read before the Ottawa Natural History Society on Friday, 24th of February, 1865    https://archive.org/details/cihm_23265

Other lectures that he gave, which are no longer available, are:

The Herpetology of the Ottawa - A  Zoological Lecture in 1865before the Mechanic’s Institute and Athenaeum  by Dr. Van Courtlandt  [Herpetology is the branch of zoology concerned with the study of amphibians.]

The Phenomena of Vegetation, a lecture on March 15, 1853 before the Bytown Mechanic’s Institute and Athenaeum.

In addition to lectures given to the institutes of Ottawa Dr. Van Cortlandt gave lectures before medical associations and to the troops at the barracks at Ottawa.  For example, he delivered an address on Entozoa on September 15, 1870 at the Annual Meeting of the Canadian Medical Association in the City Ottawa, Province of Ontario
[Canada Medical Journal and Monthly Record of Medical and Surgical Science, Volume 7, 1871, at  Page 133]       

He also wrote numerous letters on various topics.    He was one of the first to write on acid rain. In a recent book, Don Nixon comments:

“Dr. Van Cortlandt predicted rust staining in 1860, after he saw that some of the stone that was being selected [for the Parliament Buildings] contained ferrous and ferric oxides, ... In what must have been one of the earliest references to acid rain he wrote to the Editor of the Ottawa Citizen ‘as rain water and the atmosphere are more or less charged with acid, it is greatly to be feared from this cause alone, that the iron spots which permeate the stone will run, and not only irreparably disfigure the front of this otherwise magnificent structure ...’ ”

[Nixon, Don, 2012, The Other Side of the Hill, Don Nixon Consulting Inc., Carleton Place, Ontario at page 303]

Another interesting contribution was a submission to the Commission Appointed to Enquire into the Condition of Navigable Streams.   Professor Jamie Benidickson noted that “Dr. E. Van Cortland, the city of Ottawa’s health officer, criticized the threefold impact of lumber mill refuse on spawning grounds, on navigation and on public health. Notwithstanding limitations in the scientific foundations on which it rested, this was a rare early attempt to consolidate a range of community concerns over industrial interference with water quality.”
[Benidickson, Jamie, 2010, Cleaning Up after the Log Drivers’ Waltz : Finding the Ottawa River Watershed, Les Cahiers de droit, Volume 51, Number 3-4, September-December 2010, p. 729-748]

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Dr. Van Cortlandt’s Geological Specimens and Assistance to the Geological Survey of Canada

Dr. van Cortlandt is remembered today principally for the “cabinet” (i.e. museum) in his home and the archeological specimens from his collection that are now found in museums in Canada (principally the McCord Museum and the Redpath Museum, both in Montreal).  He is also mentioned in connection with archeological specimens from the “cabinet” of the Ottawa Natural History Society that he curated which later found there way into the collection of the Geological Survey of Canada and later the Canadian Museum of Civilization –  now the Canadian Museum of History.   The  geological specimens in his cabinet were also quite stunning.

There are three references to fossils from Dr. Van Cortlandt’s cabinet  in papers published by Elkanah Billings.   Note that the third fossil is named after Dr. Van Cortlandt.

Comarocystites Punctatus
“Dr. E. Van Cortlandt has kindly sent me from his cabinet two of the best specimens of C. Punctatus that I have yet seen, both of which have both of which have the mouth furnished with six valves, and it thus appears that the number is as variable as it is in the Crinoid Caryocrinus ornatus” 

[E. Billings, 1858, On the Cystitdeae of the Lower Silurian Rocks of Canada, in
Figures and Descriptions of Canadian Organic Remains,  Decade III.  Plate V, Geological Survey of Canada] 
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Glyptocrinus Ramulosus, Billings
...
“A highly interesting specimen in the cabinet of Dr. Van Cortlandt of the city of Ottawa, consists of the inside of a cup two inches and a-half in length  and one inch and seven-eighths in diameter, at the base of the free arms.  It had been completely embedded in the stone, but by some means the body has been completely extracted, leaving all the plates lining the cavity in their natural position.”



[E. Billings, 1857, Report for the Year 1856 of E. Billings, Esq., Palaeontologist addressed to Sir William E. Logan, Provincial Geologist, Geological Survey of Canada, Report of Progress
For the Years 1853-54-55-56 at page 259
E. Billings, 1859, On the Crinodeae of the Lower Silurian Rocks of Canada, in Figures and Descriptions of Canadian Organic Remains,  Decade IV, pages 57- 58,  plate. VII, figs. 2a-f; plate VIII, figs. la-e , Geological Survey of Canada ]

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Carabocrinus vancortlandti, Billings
   
“The species is dedicated to Dr. E. Vancortlandt, of the City of Ottawa, whose zeal in the advancement of science has been productive of many beneficial results. The only specimen known belongs to his cabinet, and has been kindly communicated by him to us for
description.”

Plate II. Figure 4 exhibits a view of the posterior side of the specimen, and is provided below:

Locality and formation. — Trenton limestone ; Township of McNab, near Arnprior.

[Billings, E, 1859, On the Crinoideae of the Lower Silurian Rocks of Canada, Figures and Descriptions of Canadian Organic Remains. Decade IV,  Geological Survey of Canada, page 32, Plate II, Figure 4. ]

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Sir William Logan thanked Dr. van Cortlandt for his assistance to the Survey as follows:

“I have in addition to express our obligations to many persons who have either presented specimens of Canadian organic remains to the Survey, or lent them to the palaeontologist for comparison or description. ... Dr. E. vancortlandt ... of Ottawa;” 

[Logan, W.A., 1863, Geology of Canada, Geological Survey of Canada, Report of Progress from Its Commencement to 1863;  Preface, pages xii-xiii]

++++++++++

Sir William Dawson, in a Lecture of the Popular Course of Montreal Natural History Society, winter of 1857-58, mentions a number of geological collections that benefitted him, including the collections of Dr. Holmes, Dr. Wilson of Perth, Rev. Mr. Bell, Sheriff Dickson,  Dr. Van Cortlandt and the Silurian Society of Ottawa.

[Dawson, W., 1858, Things to be Observed in Canada, and especially in Montreal and its Vicinity,  The Journal of Education for Lower Canada, Second Volume, page 40 at 43
Dawson, W., 1859, Things to be Observed in Canada, and especially in Montreal and its Vicinity, The Canadian Naturalist and Geologist, Volume III, page 1 at pages 10 and 11.]

++++++++++++++++++++++++++++++++++++
Dr. Henri-Marc Ami, Assistant Paleontologist to the Geological Survey of Canada,  also mentioned Dr. Van Cortlandt’s collection on two occasions.  First he commented on fossils from the Trenton limestone, as follows:

“Trenton Formation – The very numerous and highly fossiliferous exposures of this formation about Ottawa, from which the late Mr. E. Billings,  the late Dr. Van Cortlandt, and many members of the Field Naturalists’ Club obtained a splendid series of fossils... prove still a rich hunting ground for palaeontologist.”

[Ami, Henri M. 1884, Report of the Geological Section for the Season of 1883, Ottawa Field Naturalists’ Club, Transactions No. 5, page 118 at 119]

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Second, he commented on Dr. Van Cortlandt’s specimens from the Pleistocene deposits, as follows:
          
“The collections of the late Dr. E. Van Cortland show that he also devoted considerable attention to these interesting deposits, ...”

[ H. M. Ami,  1887, The Great Ice Age and Subsequent Formations at Ottawa, Ontario.
The Ottawa Naturalist, The  Transactions of the Ottawa Field-Naturalists' Club.
Vol. III., page 65 at page 66]

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Dr. Van Cortlandt’s Influence on David Ross McCord

Dr. Van Cortlandt’s cabinet, with its archaeological and geological specimens, is said by a number of sources to have been an object of great attraction to those  who visited Ottawa.  His collection is said by at least two sources to have influenced David Ross McCord, who in 1919, presented his extensive collection of artifacts to McGill University.  In 1921 the McCord National Museum was opened to house the collection. 

Moira T. McCaffrey writes:

“At the age of fourteen, David had an experience that may have marked his life forever.  As a reward for good conduct and prizes obtained at school, he was invited to accompany his father on a steamer trip to Ottawa.   While there, they visited [his father’s] schoolmate Dr. Edward VanCortlandt. He showed them“his cabinet,” which was crammed with archaeological artifacts, and promised to aid David with his geological studies.”

[Moira T. McCaffrey, 1999, Rononshonni - The Builder: David Ross McCord’s Ethnographic Collection, in Collecting Native America, 1870-1960, Edited  By Shepard Krech III and Barbara A. Hail,   Published by the Smithsonian Institution
 https://books.google.ca/books?isbn=1588344142] 

Where Are Dr. Van Cortlandt’s Specimens Today?


Interestingly, the archaeological artifacts in Dr. Edward Van Cortlandt’s “cabinet” eventually entered the collection of McGill.   Both the 1879 and 1880 Annual Calendars of McGill College and University mention that the Ethnology  part of McGill’s  Museum of Geology and Natural History displayed “ the collection of the late Dr. Van Cortland of Ottawa, purchased from his heirs”.

It is not clear whether  the three archeological specimens in the collection of the McCord Museum
( Pot   ACC1337 ; Pipe bowl  ACC4459B ; Pipe bowl  ME937.22) with the tag line “Gift of Dr. Van Cortlandt” that  can be viewed online at
  http://www.mccord-museum.qc.ca/en/keys/collections/ 
 were part of the collection purchased by McGill from his heirs.

It is also not clear whether McGill  purchased any of  his fossil, mineral and rock specimens.

At least two specimens collected by Dr. Van Cortlandt are in the collection of the Geological Survey of Canada.   Percy Raymond, Paleontologist, Geological Survey of Canada, mentions that one of the prizes of  Dr. Van Cortlandt’s collection, which he (Raymond) identifies as a new species and names Lebetodiscus Loriformus,  was by 1915 in the collection of the Museum of the Geological Survey, as follows:

Lebetodiscus Loriformus, Raymond

“This specimen has long been knows to the collectors about Ottawa as one of the prizes of Dr. Van Cortlandt’s collection. (Now in the Museum of the Geological Survey, No. 1414).    It  has always been considered as an abnormal, long-rayed specimen  of Agelacrinites dicksoni, and there can be no doubt that it is  very closely related to that species, but since it forms one of  the "connecting links" with the species of the later formations,  I propose to give it a new name. It may be described briefly  as a Lebetodiscus with rays so long that each one nearly touches its neighbor, all rays contra-solar, and equally spaced, the outer border of small plates narrow, supra-oral structure apparently  as in L. dicksoni. This species is believed to be ancestral to the very long rayed forms for which Hall erected the genus Streptaster.

The holotype is 23 mm. in greatest diameter, and is from the Trenton at Ottawa, Ontario. Probably from the "Cystid beds," about 180 feet below the top of the formation. It is No.1414 in the Victoria Memorial Museum.”

[Raymond, Percy E. 1915, Revision of the Canadian Species of “Agelacrinites”, The Ottawa Naturalist, Volume XXIX, pages 53 -62  at 56, Plate I, Figure 6]




This is the photo of the Holotype from Raymond's paper.

Lawrence Lambe, Assistant Palaeontologist to the Geological Survey,  when discussing the coral Protarea Vetusta, Hall, mentions that it “occurs in the Trenton formation at and in the vicinity of Ottawa, Ont. ... The specimens in the possession of the Geological Survey were collected at Ottawa by Dr. Van Cortlandt, at Ottawa, by H. M. Ami, 1882, ...”

[Lambe, Lawrence M., 1899, A Revision of the Genera and Species of Canadian Palaeozoic Corals, Contributions to Canadian Palaeontology, Volume IV, Part I, Geological Survey of Canada at page 90]




++++++++++++++++++++++++++++++++

Dr. Van Cortlandt’s Influence on the Rocks Used to Construct Canada’s Parliament Buildings  

       
An intriguing  piece of information that I found in my research is that Dr. Van Cortlandt may have influenced the choice of stone used to construct the exterior of Canada’s Parliament Buildings.   I have deliberately used the word “may” because there is some confusion surrounding the exact nature of Dr. Van Cortlandt’s contribution.  

I suspect that everyone is aware that the primary stone used to construct the exterior walls of the Parliament Buildings is Nepean sandstone, a buff coloured sandstone.  Some will also be aware that Potsdam sandstone, a reddish sandstone, is used for the  window and door trims of the Library of Parliament,  that Ohio sandstone is used for much of the remainder of the trim, and that the cornerstone is white marble from Pontiac County, Quebec.   Very little limestone was used in the construction of the Parliament Buildings.   [For ease of reference I’ve used the terms Nepean sandstone and Potsdam sandstone the way the terms are being used for the ongoing restoration of the Parliament Buildings.]
   
One of the first sources that I found linking  Dr. Van Cortlandt and the stones of the Parliament Buildings is the online Dictionary of Canadian Biography which mentions that:     “He published, ... in 1860, a significant brochure entitled Observations on the building stone of the Ottawa country. In the latter, Van Cortlandt claims to have earlier called to the attention of Lord Elgin  the location of the stone from which the parliament building was constructed.”
[Courtney C. J. Bond, “VAN CORTLANDT, EDWARD,” in Dictionary of Canadian Biography, vol. 10, University of Toronto/Université Laval, 2003–, accessed February , 2015, http://www.biographi.ca/en/bio/van_cortlandt_edward_10E.html. ]

Another much earlier source that credits Dr. Van Cortlandt is Henry James Morgan who commented: “He was the first to point out the locality of the stone with which the parliamentary buildings are being erected. To this he drew the attention of the Earl of Elgin, a circumstance which tended, perhaps more than anything else, to give to Ottawa favourable publicity.”

[ Henry James Morgan, 1862, Sketches of Celebrated Canadians: And Persons Connected with Canada,  Hunter and Rose, Co., London, 779 pages at page 750.]  
      
Nevertheless, when I looked at Dr. Van Cortlandt’s own writings, I was left in doubt.  The first clues are found in the text of Dr. Van Cortlandt’s paper entitled Observations on the Building Stone of the Ottawa Country  –  a Lecture delivered before the Ottawa Silurian Society of Ottawa on the 15th November, 1858.  (Perhaps 1859? The date is changed in pen on the cover.)  In the text of his paper, when covering sandstone, he does discuss what we would now call Nepean sandstone, but he discounts it as a building stone because it is “so extremely dense that no tool can be tempered sufficiently to work it”, though he does conclude that “This stone exists on both sides of the Ottawa in Templeton, Stony Swamp and various other situations in inexhaustible quantities, and in some instances advantageously stratified.”  Much later in his paper Dr. Van Cortlandt , when discussing Trenton Limestone, draws attention to an outcrop of a dark limestone of a “very superior compact description” below Mr. Blythe’s Cabinet warehouse, and continues: “I was the first person to call who sent a specimen of this stone, together with one of sandstone of a lightest green colour, hitherto unnoticed by the Board of Works, and who called their attention to them.  If it is discovered on further examination and investigation to realize my expectations, and is adjudged worthy of consideration as a building stone, and deserves a place in the new Parliamentary buildings, I shall be rewarded amply in knowing that I have been the humble instrument of saving several thousand pounds of public money since this stone is on public property.”

The second clue is in the Postcript to Dr. Van Cortlandt’s paper, where he states:
“Since these pages were sent to press, the author has had the gratification of finding that the most proximate favourable locality pointed out by him, has been selected for procuring a portion of the stone to be used in the new Parliament Buildings, and deems it requisite to call the attention of the proper authorities to the paramount necessity which exists...for exercising care and caution in the selection of the material.  It is a fact well knows to geologist, that the Trenton Limestone is frequently rendered more or less objectionable as a building stone, if indescriminatley selected ... Both these attributes are clearly illustrated in the stone at the base of the promontary below Mr. Blythe’s...”.

I understand the references in the text of the paper and in the postscript to mean that Trenton Limestone from the locality identified by Dr. Van Cortlandt would be used to construct the Parliament Buildings.   This  makes sense when you realize that it was initially intended to construct the Parliament Buildings out of limestone.   Later, is was decided to use sandstone.   However, while Dr. Van Cortlandt is taking credit for a source for  limestone,  I  note that he sent a sample of limestone and a sample of sandstone to the Board of Works.  

Interestingly, support for Dr. Van Cortlandt having  influenced the choice of Nepean Sandstone can be found in  a recent book by Dr. Don Nixon entitled The Other Side of the Hill that was published in 2012 by Don Nixon Consulting Inc. Of Carleton Place, Ontario and that is available from the Ottawa Public Library.  He mentions that an 1858 “story in the Ottawa Banner of April 22 where Dr. Van Cortlandt called public attention to the existence of a quarry of compact sandstone on Lot 24, 22nd Concession Templeton about four miles away, and said that if the stone was carefully selected quite free from iron stains that it would be in demand for the new Parliament Buildings.” and that “In November 1859, Van Cortlandt gave a lecture on building stones and showed some beautiful specimens of sandstone from Nepean, Templeton, Pembroke, and the Calumet.  It may have been that Fuller [the chief Architect for the Parliament Buildings]  attended the lecture and started thinking about sandstone because it was about that time... that he started looking for a different stone.”

[Nixon, Don, 2012, The Other Side of the Hill, Don Nixon Consulting Inc., Carleton Place, Ontario at page 78]

While Dr. Don Nixon’s research suggests that Dr. Van Cortlandt influenced the choice of Nepean sandstone as the primary stone used to construct the Parliament Buildings, the extent of his contribution is still  not clear.  However, it is clear from Dr. Nixon’s research that it was Dr. Van Cortlandt who was responsible for the selection of marble from the Portage du Fort quarry in Pontiac County, Quebec for use as the cornerstone for the Parliament Buildings.    Dr. Nixon notes that “Upon its arrival, the big block of stone was paraded up and down the streets. The wagon halted at Dr. Van Corlandt’s house, and everyone gave him three hearty cheers of appreciation.” [Nixon, Don, 2012, The Other Side of the Hill,  page 67]

Conclusion


Dr. Van Cortlandt saw many changes over his lifetime.  When he arrived at Bytown it was a small lumber town of secondary importance to Perth and there were barracks on what we now call Parliament Hill.  By the time he died Ottawa had become the nation’s capital with a population  seven times that of Perth and the Parliament Buildings had been constructed.    While it has been 140 years since his death, his name is still mentioned.  Archaeological specimens from his collection can be found in the collection of the McCord Museum and the Redpath Museum.  The fossil Carabocrinus vancortlandti, Billings is still referenced in scientific papers.   There has been recent debate in the various journals concerning the location of his dig reported in his paper  Notice of an Indian Burial Ground.   He was also years ahead of his time in predicting acid rain and the affect of industrialization on spawning grounds, on navigation and on public health.   And if he did contribute to Nepean Sandstone being used as the stone for the exterior of the Parliament Buildings, it was a lasting contribution.

Christopher Brett
Perth, Ontario



Friday, 30 January 2015

When Magnetite is not Fe3O4

It has to be over ten years since I signed up to receive The Alchemist Newsletter from ChemWeb.com.   Over that period the newsletter has notified me of many interesting developments in many different fields.   Each issue of the newsletter provides a series of well written, short summaries of recent developments with links to the articles or press releases.  I’d encourage anyone with an interest in chemistry to sign up.   Not only is it interesting, but it’s free.

An issue of The Alchemist Newsletter from December was particularly enlightening as a summary with the  deceptive  title “Rust never sleeps” details developments in determining the atomic structure of the surface of magnetite .   Interestingly Magnetite, which I think of solely as the magnetic iron ore, has an increasingly prominent role in catalysis, hydrogen production, spintronics, and drug delivery systems.    Further, the  properties of magnetite are governed by missing iron atoms in the sub-surface layer.  The surface of magnetite is not Fe3O4 but instead  is Fe11O16.

The Alchemist Newsletter links to the following press release:
http://www.eurekalert.org/pub_releases/2014-12/vuot-tfd120314.php

That press release mentions:

“Perhaps the most surprising property of the magnetite surface is that single atoms placed on the surface, for instance gold or palladium, stay perfectly in place instead of balling up and forming a nanoparticle. This effect makes the surface an extremely efficient catalyst for chemical reactions...

Instead of a fixed structure of metal atoms with built-in oxygen atoms, one rather has to think of iron-oxides as a well-defined oxygen structure with little metal atoms hiding inside. Directly below the outermost atomic layer, the crystal structure is rearranged and some iron atoms are absent.

It is precisely above such places of missing iron atoms that other metal atoms attach. These iron-vacancy-sites are regularly spaced, and so there is always some well-defined distance between gold or palladium atoms attaching to the surface. This explains why magnetite surfaces prevent these atoms from forming clusters.”


If you are like me one of the things that you remember from your first geology course is that Magnetite has the formula Fe3O4 and that Hematite has the formula Fe2O3.   It’s a bit of a shock to think that the formulas change at the surface.

That article made me ask myself which mineral formulas I could still remember.   There were thirty-one in total (and only five were native elements).

Christopher Brett
Perth, Ontario

Journal Reference:

R. Bliem, E. McDermott, P. Ferstl, M. Setvin, O. Gamba, J. Pavelec, M. A. Schneider, M. Schmid, U. Diebold, P. Blaha, L. Hammer, G. S. Parkinson. Subsurface cation vacancy stabilization of the magnetite (001) surface. Science, 2014; 346 (6214): 1215 DOI: 10.1126/science.1260556