Name:
Desmostylus
(Chain pillar).
Phonetic: Dez-moe-sty-lus.
Named By: Othniel Charles Marsh - 1888.
Synonyms: Desmostylella, Vanderhoofius
coalingensis.
Classification: Chordata, Mammalia,
Paenungulata, Desmostylia, Desmostylidae.
Species: D. hesperus (type),
D. coalingensis, D. japonicus
Diet: Herbivore.
Size: 1.8 meters long.
Known locations: Pacific coastlines of North
America, Russia and Japan.
Time period: Chattian of the Oligocene through to
Tortonian of the Miocene.
Fossil representation: Multiple specimens.
Often
described as hippopotamus-like because of its heavily built quadrupedal
body, Desmostylus is a peculiar mammal.
Palaeontologists are still
unsure how Desmostylus is related to other mammals
with theories
covering a wide range of options from being related to elephants, to
hippopotamuses to just being a separate side branch of mammals that
left no modern descendants.
Desmostylus
is widely believed to have been a semi aquatic animal in that it
regularly entered the water, but would return to land to rest. The
remains of Desmostylus are known from across most
of the northern
Pacific Rim from Japan and Russia to the west coast of the United
States. This pattern of fossils led to the idea that Desmostylus
followed the coastlines to spread out into new territories, however
a 2003 study has cast serious doubt upon this. The study in
question conducted by Mark T. Clementz, Kathryn A. Hoppe and Paul
L. Koch used isotope analysis (of oxygen, carbon and strontium)
of tooth enamel from Desmostylus and concluded
that it actually lived
in freshwater systems. This reveals a picture of Desmostylus
living
around estuaries and the immediate freshwater systems, however it
does not explain the fossil distribution as rivers tend to run into the
ocean not run parallel to it. It is perhaps possible that early on
Desmostylus was a marine creature that spent more
time on the coast,
but once a range was established and new mammals such as sirenians
(sea cows) began to become more common during the Miocene,
Desmostylus were outcompeted and pushed into
freshwater ecosystems.
Desmostylus
is believed to have fed upon soft aquatic plants that it may have
rooted up with its specialised teeth. The anterior lower jaw teeth
were also enlarged into tusks and grew into a shovel-shaped arrangement
similar to the prehistoric gomphothere elephants (think
Gomphotherium).
Two more tusk-like teeth grew down from the upper
jaw. The back teeth have a cylindrical arrangement which was the
inspiration for the name Desmostylus which means
‘chain pillar’ The
lower foreleg was also adapted to work best in the water since the
bones were fused together to make a rigid appendage. Although this
would have been cumbersome on land, since the entire leg would have
to be turned to turn the foot, this would have made it easier for
Desmostylus to push itself along while in the water.
Further reading
- Notice of a new fossil sirenian, from California. - American Journal
of Science 25 (8): 94–96. - O. C. Marsh - 1888.
- Notes on a New Fossil Mammal. - Journal of the College of Science,
Imperial University, Tokyo, Japan 16. - S. Yoshiwara & J.
Iwasaki - 1902.
- Notes on Desmostylus japonicus - S. Tokunaga
& C. Iwasaki -
1914.
- A review of the Sirenia and Desmostylia. - University of California
Publications in Geological Sciences 36 (1): 1–146. - Roy Herbert
Reinhart - 1959.
- Summary of taxa and morphological adaptations of the Desmostylia. -
Island Arc 3 (4): 522–537. - Norihisa Inuzuka, Daryl P. Domning
& Clayton E. Ray - 1984.
- A paleoecological paradox: the habitat and dietary preferences of the
extinct tethythere Desmostylus, inferred from
stable isotope analysis.
- Paleobiology 29 (4): 506–519. - Mark T. Clementz, Kathryn A. Hoppe,
Paul L. Koch - 2003.
- Discovery of a desmostylian tooth from Kitami City, northeastern
Hokkaido, Japan. - Memoir of the Fukui Prefectural Dinosaur Museum 6:
57–61. - Yukimitsu Tomida & Toshikazu Ohta - 2007.
- Habitat preferences of the enigmatic Miocene tethythere Desmostylus
and Paleoparadoxia (Desmostylia; Mammalia) inferred from the
depositional depth of fossil occurrences in the Northwestern Pacific
realm. - Palaeogeography, Palaeoclimatology, Palaeoecology. 471:
254–265 - 2017.