A Guide to the Study of Fishes, Volume 1 (of 2)Jordan, David Starr
History
A Guide to the Study of Fishes, Volume 1 (of 2)
Jordan, David Starr
Fishes; Fishes -- Bibliography; Zoology -- History
"There is no evidence from either a geologic or a biologic standpoint
for believing that the oceans have ever communicated across the
Isthmian regions since Tertiary time. In other words, there is no
evidence for these later passages which have been established upon
hypothetical data, especially those of Pleistocene time.
"The numerous assertions, so frequently found in literature, that the
two oceans have been frequently and recently connected across the
Isthmus, and that the low passes indicative of this connection still
exist, may be dismissed at once and forever and relegated to the domain
of the apocryphal. A few species common to the waters of both oceans in
a predominantly Caribbean fauna of the age of the Claiborne epoch of
the Eocene Tertiary is the only paleontologic evidence in any time upon
which such a connection may be hypothesized.
"There has been a tendency in literature to underestimate the true
altitude of the isthmian passes, which, while probably not intentional,
has given encouragement to those who think that this Pleistocene
passage may have existed. Maack has erroneously given the pass at 186
feet. Dr. J. W. Gregory states 'that the summit of the Isthmus at one
locality is 154 feet and in another 287 feet in height.' The lowest
isthmian pass, which is not a summit, but a drainage col, is 287-295
feet above the ocean.
"If we could lower the isthmian region 300 feet at present, the waters
of the two oceans would certainly commingle through the narrow Culebra
Pass. But the Culebra Pass is clearly the headwater col of two streams,
the Obispo flowing into the Chagres, and the Rio Grande flowing into
the Pacific, and has been cut by fluviatile action, and not by marine
erosion, out of a land mass which has existed since Miocene time. Those
who attempt to establish Pleistocene interoceanic channels through this
pass on account of its present low altitude must not omit from their
calculations the restoration of former rock masses which have been
removed by the general levelling of the surface by erosion."
[Illustration: FIG. 182.--_Xenocys jessiæ_ Jordan and Bollman.
Galapagos Islands. Family _Lutianidæ_.]
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