Truckee Formation

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Truckee Formation
Stratigraphic range: Late Miocene, 10.3  Ma
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Type Formation
Unit of Lahontan Basin
Lithology
Primary Diatomite
Location
Region Nevada
Country United States
Type section
Named for Truckee River

The Truckee Formation is a lacustrine geologic formation in Nevada, USA. It preserves fossils dating back to the late Miocene. Part of the Lahontan Basin, it was deposited in the prehistoric Lake Truckee, a predecessor to Lake Lahontan. [1]

Contents

Paleoecology

The formation is notable for its preservation of articulated vertebrate skeletons in diatomite, which is mined near Hazen, Nevada. The diatomite deposition, which would have occurred seasonally, provides a snapshot of the ecological dynamics that would have occurred in the lake ecosystem every year. [2] Despite the exquisite preservation, only a total of eleven vertebrate taxa are known from the diatomite beds. However, the two most abundant vertebrate taxa of the formation provide crucial data about eco-evolutionary dynamics within a prehistoric ecosystem. [1]

Among the most famous taxa from the formation is the stickleback Gasterosteus doryssus , which provides the majority of fossil fish specimens from the formation. Fossil specimens of this stickleback form a time series spanning many generations over thousands of years, in which they can be observed developing a number of adaptations to their lake environment and diverging into two distinct ecotypes, exemplifying the rapid evolution that their modern relative, the three-spined stickleback, is well known for. [1] [3] [4] The other most frequent taxon in the formation is the killifish Fundulus nevadensis ; despite its abundance, they are very rare up until the youngest sections, very few of its fossils co-occur with sticklebacks, and when the killifish do become abundant in the fossil record, the sticklebacks essentially disappear from the lake within a period of less than 50 years. This suggests that following their colonization of the lake, the killifish may have driven the sticklebacks to extinction on a rapid timescale comparable to modern biological invasions. [2]

Uniquely, the paleofauna of the formation shares many elements with the native freshwater fauna found in lowlands along the Pacific Coast. It is thought that the Sierra Nevada Mountains were lower when the formation was deposited, allowing for connectivity between the Pacific lowlands and the rivers draining out of Lake Truckee, and in turn allowing for fishes from these habitats to colonize the lake. The rise of the mountains would have eventually cut off this water source, drying out the rivers and driving the ancestors of these fish to extinction. The exception is the catfish Ameiurus hazenensis , which belongs to a lineage found in eastern North America; it is thought that Lake Truckee also had some connectivity with the Mississippi Basin, explaining the catfish's presence there. [1]

Vertebrate paleobiota

Based on Cerasconi et al., 2024: [1]

Ray-finned fish

GenusSpeciesMaterialNotesImages
Ameiurus A. hazenensis An articulated skeleton.A bullhead catfish. Ameiurus melas by Duane Raver.png
Fundulus F. nevadensis Numerous articulated skeletonsA killifish. One of the most common fish in the formation. Annual report of the Forest, Fish and Game Commission of the State of New York (1899) (14569003897).jpg
Gasterosteus G. doryssus Numerous articulated skeletonsA stickleback related to the three-spined stickleback. One of the most common fish in the formation. Gasterosteus aculeatus aculeatus.jpg
Oncorhynchus O. belli An articulated skeleton.A Pacific trout potentially related to the cutthroat trout. Oncorhynchus clarkii.jpg

Amphibians

GenusSpeciesMaterialNotesImages
Anura indet.An articulated skeleton.A large-sized frog, most likely a member of the genus Rana .

Reptiles

GenusSpeciesMaterialNotesImages
Colubridae indet.An articulated skeleton.A colubrid snake, initially identified as Coluber sp. Appears to have had piscivorous tendencies and may have died choking on a stickleback, so it may represent a garter snake instead.

Birds

GenusSpeciesMaterialNotesImages
Passeriformes indet.Two nearly complete skeletonsA perching bird.
Podicepidae indet.Podicepidae sp. AArticulated skeletonA grebe that appears to have fed on sticklebacks.
Podicepidae sp. BArticulated skeleton

Mammals

GenusSpeciesMaterialNotesImages
Sciurus S. olsoni Articulated skeletonA squirrel. The presence of this species fills in a major gap in the presence of fossil Sciurus on the North American continent. [1] The quadrupeds of North America (Plate CLIII) (7752432766).jpg

See also

References

  1. 1 2 3 4 5 6 Cerasoni, Jacopo Niccolò; Bell, Michael A.; Stuart, Yoel E. (2024). "Geology, microstratigraphy, and paleontology of the lacustrine Truckee Formation diatomite deposits near Hazen, Nevada, USA, with emphasis on fossil stickleback fish". PaleoBios. 41 (1). doi: 10.5070/P941161500 . ISSN   0031-0298.
  2. 1 2 "Fossil fishing for clues about a prehistoric invasion". ucmp.berkeley.edu. Retrieved 2024-12-08.
  3. Bell, M. A. (2009). "Implications of a fossil stickleback assemblage for Darwinian gradualism". Journal of Fish Biology. 75 (8): 1977–1999. Bibcode:2009JFBio..75.1977B. doi:10.1111/j.1095-8649.2009.02416.x. ISSN   1095-8649.
  4. Siddiqui, Raheyma; Swank, Samantha; Ozark, Allison; Joaquin, Franklin; Travis, Matthew P.; McMahan, Caleb D.; Bell, Michael A.; Stuart, Yoel E. (2024-04-17). "Inferring the evolution of reproductive isolation in a lineage of fossil threespine stickleback, Gasterosteus doryssus". Proceedings of the Royal Society B: Biological Sciences. 291 (2021): 20240337. doi:10.1098/rspb.2024.0337. PMC   11021931 . PMID   38628124.