Santiago Formation, California: Difference between revisions
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| type = [[Geological formation]] |
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| age = [[Late Eocene]]-[[Late Oligocene]] ([[Uintan]]-[[Duchesnean]]) |
| age = [[Late Eocene]]-[[Late Oligocene]] ([[Uintan]]-[[Duchesnean]]) |
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| period = Oligocene |
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The '''Santiago Formation''' is a [[Formation (geology)|geologic formation]] in [[Orange County, California|Orange]] and northwestern [[San Diego County, California|San Diego County]], [[California]]. The [[siltstone]]s, [[mudstone]]s and [[sandstone]]s of the formation preserve [[fossils]] of ''[[Walshina|Walshina esmaraldensis]]'' and ''[[Diegoaelurus|Diegoaelurus vanvalkenburghae]], dating back to the [[Late Eocene]] to [[Late Oligocene]] [[Period (geology)|periods]] ([[Uintan]] to [[Duchesnean]] in the [[North American land mammal age|NALMA classification]]).<ref>[http://www.fossilworks.org/cgi-bin/bridge.pl?a=collectionSearch&collection_no=196550 Kelly Ranch Core] at [[Fossilworks]].org</ref> |
The '''Santiago Formation''' is a [[Formation (geology)|geologic formation]] in [[Orange County, California|Orange]] and northwestern [[San Diego County, California|San Diego County]], [[California]]. The [[siltstone]]s, [[mudstone]]s and [[sandstone]]s of the formation preserve [[fossils]] of ''[[Walshina|Walshina esmaraldensis]]'' and ''[[Diegoaelurus|Diegoaelurus vanvalkenburghae]]'', dating back to the [[Late Eocene]] to [[Late Oligocene]] [[Period (geology)|periods]] ([[Uintan]] to [[Duchesnean]] in the [[North American land mammal age|NALMA classification]]).<ref>[http://www.fossilworks.org/cgi-bin/bridge.pl?a=collectionSearch&collection_no=196550 Kelly Ranch Core] at [[Fossilworks]].org</ref> |
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== Depositional environment == |
== Depositional environment == |
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The only paleoenvironmental interpretation based exclusively on specimens from the Santiago Formation is a study of land snails from SDSNH locality 3276 (Member C, [[Oceanside, San Diego County]]), which found the distribution of shell sizes and shapes to be consistent with interpretations of subtropical to tropical conditions and paleotemperatures in excess of {{convert|25|C|F}}.<ref name=Lopez2018_p5>López Torres et al., 2018, p.5</ref> |
The only paleoenvironmental interpretation based exclusively on specimens from the Santiago Formation is a study of land snails from SDSNH locality 3276 (Member C, [[Oceanside, San Diego County]]), which found the distribution of shell sizes and shapes to be consistent with interpretations of subtropical to tropical conditions and paleotemperatures in excess of {{convert|25|C|F}}.<ref name=Lopez2018_p5>López Torres et al., 2018, p.5</ref> |
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==Fossil content== |
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===Mammals=== |
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====Ferae==== |
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{| class="wikitable" align="center" |
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! colspan="6" align="center" | '''[[Ferae]] reported from the Santiago Formation''' |
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! Genus !! Species !! Presence |
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!'''Material'''!! Notes !! Images |
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|''[[Diegoaelurus]]'' |
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|''D. vanvalkenburghae'' |
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|"Member C".<ref name=":0">{{Cite journal |last=Zack |first=Shawn P. |last2=Poust |first2=Ashley W. |last3=Wagner |first3=Hugh |date=2022-03-15 |title=Diegoaelurus, a new machaeroidine (Oxyaenidae) from the Santiago Formation (late Uintan) of southern California and the relationships of Machaeroidinae, the oldest group of sabertooth mammals |url=https://peerj.com/articles/13032 |journal=PeerJ |language=en |volume=10 |pages=e13032 |doi=10.7717/peerj.13032 |issn=2167-8359}}</ref> |
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|A nearly complete [[dentary]].<ref name=":0" /> |
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|An [[Oxyaenidae|oxyaenid]]. |
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| ''[[Lycophocyon]]'' |
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|''L. hutchisoni'' |
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| Upper portions of "member C".<ref name=":1">{{Cite journal |last=Tomiya |first=Susumu |date=2011-09-14 |title=A New Basal Caniform (Mammalia: Carnivora) from the Middle Eocene of North America and Remarks on the Phylogeny of Early Carnivorans |url=https://journals.plos.org/plosone/article?id=10.1371/journal.pone.0024146 |journal=PLOS ONE |language=en |volume=6 |issue=9 |pages=e24146 |doi=10.1371/journal.pone.0024146 |issn=1932-6203 |pmc=PMC3173397 |pmid=21935380}}</ref> |
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|Multiple specimens.<ref name=":1" /> |
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| A basal [[Caniformia|caniform]]. |
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====Ungulates==== |
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{| class="wikitable" align="center" |
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! colspan="6" align="center" | '''[[Ungulate]]s reported from the Santiago Formation''' |
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! Genus !! Species !! Presence |
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!'''Material'''!! Notes !! Images |
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| ''[[Hesperaletes]]'' |
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|''H. borineyi'' |
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| Member C.<ref name=":2">{{Cite journal |last=Colbert |first=Matthew W. |date=2006-09-11 |title=Hesperaletes (Mammalia: Perissodactyla), a new tapiroid from the middle Eocene of southern California |url=https://www.researchgate.net/publication/232687764_Hesperaletes_Mammalia_Perissodactyla_a_new_tapiroid_from_the_middle_Eocene_of_southern_California |journal=Journal of Vertebrate Paleontology |language=en |volume=26 |issue=3 |pages=697–711 |doi=10.1671/0272-4634(2006)26[697:HMPANT]2.0.CO;2 |issn=0272-4634}}</ref> |
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|Numerous specimens.<ref name=":2" /> |
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| A [[Tapiroidea|tapiroid]]. |
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== See also == |
== See also == |
Revision as of 13:55, 7 December 2022
Santiago Formation | |
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Stratigraphic range: Late Eocene-Late Oligocene (Uintan-Duchesnean) | |
Type | Geological formation |
Lithology | |
Primary | Siltstone, mudstone |
Other | Sandstone |
Location | |
Coordinates | 33°06′N 117°18′W / 33.1°N 117.3°W |
Approximate paleocoordinates | 33°18′N 104°06′W / 33.3°N 104.1°W |
Region | Orange & NW San Diego County, California |
Country | United States |
The Santiago Formation is a geologic formation in Orange and northwestern San Diego County, California. The siltstones, mudstones and sandstones of the formation preserve fossils of Walshina esmaraldensis and Diegoaelurus vanvalkenburghae, dating back to the Late Eocene to Late Oligocene periods (Uintan to Duchesnean in the NALMA classification).[1]
Depositional environment
The only paleoenvironmental interpretation based exclusively on specimens from the Santiago Formation is a study of land snails from SDSNH locality 3276 (Member C, Oceanside, San Diego County), which found the distribution of shell sizes and shapes to be consistent with interpretations of subtropical to tropical conditions and paleotemperatures in excess of 25 °C (77 °F).[2]
Fossil content
Mammals
Ferae
Ferae reported from the Santiago Formation | |||||
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Genus | Species | Presence | Material | Notes | Images |
Diegoaelurus | D. vanvalkenburghae | "Member C".[3] | A nearly complete dentary.[3] | An oxyaenid. | |
Lycophocyon | L. hutchisoni | Upper portions of "member C".[4] | Multiple specimens.[4] | A basal caniform. |
Ungulates
Ungulates reported from the Santiago Formation | |||||
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Genus | Species | Presence | Material | Notes | Images |
Hesperaletes | H. borineyi | Member C.[5] | Numerous specimens.[5] | A tapiroid. |
See also
References
- ^ Kelly Ranch Core at Fossilworks.org
- ^ López Torres et al., 2018, p.5
- ^ a b Zack, Shawn P.; Poust, Ashley W.; Wagner, Hugh (15 March 2022). "Diegoaelurus, a new machaeroidine (Oxyaenidae) from the Santiago Formation (late Uintan) of southern California and the relationships of Machaeroidinae, the oldest group of sabertooth mammals". PeerJ. 10: e13032. doi:10.7717/peerj.13032. ISSN 2167-8359.
{{cite journal}}
: CS1 maint: unflagged free DOI (link) - ^ a b Tomiya, Susumu (14 September 2011). "A New Basal Caniform (Mammalia: Carnivora) from the Middle Eocene of North America and Remarks on the Phylogeny of Early Carnivorans". PLOS ONE. 6 (9): e24146. doi:10.1371/journal.pone.0024146. ISSN 1932-6203. PMC 3173397. PMID 21935380.
{{cite journal}}
: CS1 maint: PMC format (link) CS1 maint: unflagged free DOI (link) - ^ a b Colbert, Matthew W. (11 September 2006). "Hesperaletes (Mammalia: Perissodactyla), a new tapiroid from the middle Eocene of southern California". Journal of Vertebrate Paleontology. 26 (3): 697–711. doi:10.1671/0272-4634(2006)26[697:HMPANT]2.0.CO;2. ISSN 0272-4634.
Bibliography
- López Torres, S.; M.T. Silcox, and P.A. Holroyd. 2018. New omomyoids (Euprimates, Mammalia) from the late Uintan of southern California, USA, and the question of the extinction of the Paromomyidae (Plesiadapiformes, Primates). Palaeontologia Electronica 21. 1–28. Accessed 2020-03-15.
Further reading
- Prothero, D.R. 2001. Magnetic stratigraphy of the middle-upper Eocene Santiago Formation, Orange and San Diego Counties, California. Guidebook, Pacific Section, Society of Economic Paleontologists and Mineralogists, 91:107-118
Categories:
- Geologic formations of California
- Paleogene California
- Duchesnean
- Uintan
- Priabonian Stage
- Rupelian Stage
- Chattian Stage
- Siltstone formations
- Mudstone formations
- Sandstone formations
- Fluvial deposits
- Fossiliferous stratigraphic units of North America
- Paleontology in California
- Orange County, California
- San Diego County, California