Goler Formation
PeriodPaleogene
Prilithologyconglomerate, sandstone
Otherlithologysiltstone, mudstone
RegionCalifornia
CountryUnited States
UnderliesRicardo Group (unconformity)
OverliesGarlock Formation (unconformity)

The Goler Formation is a Paleogene geologic formation in California. It outcrops in the El Paso Mountains in the Mojave Desert near Ridgecrest. Fossils of mammals, reptiles, and cartilaginous fish are found in a few late Paleocene (Tiffanian age) sites from this formation, representing the best terrestrial Paleocene deposits in California.[1]

Geology

The Goler Formation is split into four members (subunits), labelled 1-4, with member 4 divided further into 4a-4d. The oldest members (1-2) lack fossils, and they probably represent alluvial fan environments eroding down into older canyons of granite and metamorphic rock. Fossils are found in members 3 and 4, which represent braided rivers and streams flowing down from the west in a warm monsoonal climate with strong wet and dry seasons. During the Paleocene, the Goler Formation was not far from the coast, but the predecessors of the Sierra Nevada further west created a rain shadow over the area. By the time of member 4d, the area was submerged by rising sea levels.[2]

Paleobiota

Nearly all fossils from the Goler Formation are concentrated into members 4a and 4b (the Goler Assemblage), with the exception of indeterminate turtles from member 3 and a Phenacodus tooth from member 4d.[1] Members 4a and 4b are probably Tiffanian (Ti3-Ti5) in age, around the start of the late Paleocene. Member 4d could be any time between Tiffanian 5 and Bridgerian (early-mid Eocene) in age.[1]

Mammals

The most abundant mammal fossils are Phenacodus cf. bisoneri and Nannodectes lynasi.[1]

Mammals of the Goler Formation
Genus / TaxonSpeciesStrataNotesImages
Arctocyonidae?indet.Member 4bAn indeterminate possible arctocyonid.
BessoecetorB. septentrionalisMember 4aA pantolestid.
DissacusD. sp.Member 4aA mesonychid.
GolerdelphysG. stockiMember 4bA herpetotheriid.
GoleroconusG. alfiMember 4a, 4bA periptychid.
IgnaciusI. frugivorusMember 4bA paromomyid.
LambertocyonL. cf. gingerichiMember 4aAn arctocyonid.
MimotricentesM. tedfordiMember 4aAn arctocyonid.
NannodectesN. lynasiMember 4a, 4bA plesiadapid.
ParomomysP. depressidensMember 4aA paromomyid.
PeradectesP. sp.Member 4a, 4bA peradectid.
PhenacodusP. cf. bisonensisMember 4a, 4bA phenacodontid.
P. cf. grangeriMember 4a
P. cf. matthewiMember 4a
P. cf. vortmaniMember 4d
PromioclaenusP. walshiMember 4aA hyopsodontid.
ProtictisP. cf. agastorMember 4aA viverravid.
P. paralus
ProtoseleneP. ashtoniMember 4aA hyopsodontid.
Stylinodontidaeindet.Member 4aAn indeterminate stylinodontid.
ThryptacodonT. sp.Member 4aAn oxyclaenid.

See also

References

  1. ^ Lofgren, Donald; Mckenna, Malcolm; Honey, James; Nydam, Randall; Wheaton, Christine; Yokote, Bryan; Henn, Lexington; Hanlon, Whitney; Manning, Stephen; Mcgee, Carter (2014-02-06). "New Records of Eutherian Mammals from the Goler Formation (Tiffanian, Paleocene) of California and Their Biostratigraphic and Paleobiogeographic Implications". American Museum Novitates. 3797 (3797): 1–57. doi:10.1206/3797.1. ISSN 0003-0082
  2. ^ Torres, M. A. & Gaines, R. R. (2013-07-29). "Paleoenvironmental and Paleoclimatic Interpretations of the Late Paleocene Goler Formation, Southern California, U.S.A., Based On Paleosol Geochemistry". Journal of Sedimentary Research. 83 (8): 591–605. doi:10.2110/jsr.2013.48. ISSN 1527-1404