The Principles of Stratigraphical GeologyMarr, J. E. (John Edward)
Science
The Principles of Stratigraphical Geology
Marr, J. E. (John Edward)
Geology, Stratigraphic
Kr., _Idothea entomon_ Lin., _Idothea Sabinei_ Kr., two species of
Lysianassida, _Pontoporeia setosa_ Stbrg., _Halimedon brevicalcar_
Goës, an Annelid, a Molgula, _Yoldia intermedia_ M. Sars, _Yoldia_ (?)
_arctica_ Gray, and a Solecurtus[39]. "The temperatures were taken by
a centigrade thermometer. Again we read of the results of dredging off
Cape Chelyuskin. "The yield of the trawling was extraordinarily
abundant; large asterids, crinoids, sponges, holothuria, a gigantic
sea-spider (Pycnogonid), masses of worms, crustacea, etc. _It was the
most abundant yield that the trawl-net at any one time brought up
during the whole of our voyage round the coast of Asia_, and this from
the sea off the northern extremity of that continent[40]."
[Footnote 38: For a discussion as to the value of plants as indices of
climate see Seward, A. C., Sedgwick Essay for 1892.]
[Footnote 39: Nordenskjöld, A. E., _The Voyage of the Vega_, Vol. I.
Chap. IV.]
[Footnote 40: _Ibid._ Chap. VII.]
Amongst the marine invertebrates reef-building corals and mollusca
perhaps furnish the best evidence of climatic conditions. The
coral-reefs of the Jurassic rocks with large gastropods and
lamellibranchs clustered around them have been appealed to in proof of
the existence of sub-tropical conditions during their formation;
further back in time we find evidence of climate furnished by the
fossils of the Silurian rocks of the Isle of Gothland in the Baltic
Sea. Of these, Lindström writes "_The fauna had a tropical character_.
In consideration of the great numbers of Pleurotomariae, Trochi,
Turbinidae and the large Pteropods the assumption of a tropical
character of the fauna may seem justifiable[41]."
[Footnote 41: Lindström, G., _On the Silurian Gastropoda and Pteropoda
of Gotland_, Stockholm, 1884, p. 33.]
Structure may give some indication of climate even though the organism
is not allied to living species. The bark of trees in arctic regions
is often thicker than in more temperate regions, and the leaves of
arctic plants often have special characters to enable them to resist
the long periods during which they are deprived of water, though the
fact that desert-plants frequently shew similar modifications deprives
this test of any particular value except as a means of corroborating
conclusions reached from other evidence[42]. The shells of arctic
mollusca may become stunted, but this is not by any means universal,
and the same result may be brought about by other abnormal conditions,
as for instance the increase of salt in a water area by evaporation.
[Footnote 42: For an account of the modifications of the leaves of
arctic plants, see Warming, Eug., _Om Grønlands Vegetation_,
Meddelelser om Grønland, 12th part, p. 105.]
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