The 2600 feet thick Hsanda Gol formation is covered in various places by Miocene-age variegated clays, sands, and gravels. It rests on top of the Early CretaceousHühteeg Svita formation. The lower portions of the formation are composed of yellow conglomerate, with the higher areas being dominated by red clays, silts and sands, as well as lava and basalt flows.[citation needed]
Hsanda Gol was traditionally assigned to the Middle Oligocene,[2][3] but after the reassignation of the preceding Ergilian age to the Late Eocene it has now been rendered early Oligocene. It is followed after a faunal hiatus by the overlaying Loh Formation which extends from the Late Oligocene into the Miocene and also contains fossil mammals. Paleomagnetism in underlying and overlaying lava flows establish the beginning of the formation at the end of the magnetic Chron C13n 33.4 million years ago, and its end at the Chron C12n, 31 million years ago.[1]
The Hsanda Gol levels rest directly over, and are continuous with the earlier Houldjin Gravels which are sometimes counted as part of the formation, but were rather deposited during the latest Eocene under wetter and more energetic conditions. In general, the Houldjin Gravels and the Hsanda Gol formation show a transition from more humid, forested conditions to an arid climate with presence of dunes and ephemeral rivers. Some taxa lived through this change including hyaenodonts and indricotheres, but others, such as brontotheres, amynodonts, rhinocerotids and entelodonts went extinct and are as a result absent from Hsanda Gol proper. The following Loh Formation, on the other hand, represents a return to more benign conditions as indicated by the reappearance of rhinocerotids and the entry of the first chalicotheres.[1]
Hsanda Gol's paleobiota resembles current desert mammal faunas, including the one found in the same area today. It is composed largely of rodents and lagomorphs with high-crowned teeth adapted to chew hard vegetation; several of these species are fossorial and none arboreal, indicating that there were no areas with high tree density. The only large browsingungulate, Paraceratherium, was probably transient and there were no medium-large herbivores. Predators were diverse but generally small, with the largest (Hyaenodon) being wolf-sized, and were adapted to hunt by ambush. Landscape would appear as a sparse plain with few tall trees near rivers or where groundwater could be found otherwise. Pallinology studies in contemporary sites of China and Mongolia are consistent with an arid-adapted woody scrubland dominated by Mormon tea and salt-tolerant nitre bush. The few trees were broad-leaved and deciduous, related to modern elm, birch, and oak.[3][1]
D. berkeyi is the only species present west of Tatal Gol, and D. colgatei is the only present at Field 538. They appear together in the others. Though not believed to have modern descendants or ecological equivalents, they present an enlargement of the mastoid region convergent with kangaroo rats and sengis found in semi-arid areas.
SW Loh East Loh NE Kholobolchi Nor Loh Tatal Gol Field 538
Pikas. "D." robustus may belong to a different genus. SW Loh only contains D. gobiensis; NE Kholobolchi Nor only "D." robustus. D. gobiensis may be ecologically similar to Pallas's pika and "D." robustus to the desert hare.
A small nimravid or "false sabertooth". There are at least two different species represented, both unnamed: a smaller one similar to a wildcat and a larger one resembling a Eurasian lynx.
An early felid better known from Europe and North America. Some authors have instead assigned this material to the nimravid Eofelis or the more advanced felid Pseudaelurus, based on dental features.[4]
A giant browsing rhinoceros of the family Hyracodontidae, originally described as Indricotherium grangeri, and one of the largest land mammals of all time. Despite its massive size (up to 6 meters tall), it could have occupied a niche similar to the Bactrian camel at Hsanda Gol.
West Tatal Gol SW Loh NE Kholobolchi Nor Loh Tatal Gol Field 538
The largest carnivore in the formation, a predatory creodont similar to a grey wolf that lived in many different Holarctic environments. H. pervagus is the only species found outside of Tatal Gol.
Restoration of H. gigas, the largest species of Hyaenodon
↑ Mellett, James Silvan (1966). Fossil mammals from the Oligocene Hsanda Gol formation, Mongolia. Part I: Insectivora, Rodentia and Deltatheridia, with notes on the paleobiology of Cricetops dormitor (Thesis). OCLC40155505.[pageneeded]
1 2 Mellett, James S (28 March 1968). "The Oligocene Hsanda Gol Formation, Mongolia: a revised faunal list". American Museum Novitates (2318). hdl:2246/2528.
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