Fossil Hill Member
{{Short description|Triassic geologic unit}}
{{Distinguish|Fossil Hill Formation}}
{{Infobox rockunit|name=Fossil Hill Member|image=|caption=|type=Geological member|age={{Geological range|Anisian}}|prilithology=Calcareous Shale|otherlithology=Limestone|namedfor=|namedby=Kathryn Nichols and Norman Silberling|region=Nevada|country=United States|coordinates=|unitof=Prida Formation, Favret Formation|subunits=|underlies=|overlies=|thickness=|extent=|area=|map=|map_caption=|period=Triassic}}
The Fossil Hill Member is a Middle Triassic-aged rock unit. The Fossil Hill unit occurs as a member of both the Prida and Favret formations. It outcrops in multiple locations across Northwestern Nevada including the western Humboldt Range, Tobin Range, Augusta Mountains, and China Mountain. Calcareous shale, mudstone, and black limestones are the most common lithologies present within the unit.{{Citation |last1=Nichols |first1=K. M. |title=Stratigraphy and Depositional History of the Star Peak Group (Triassic), Northwestern Nevada |date=1977 |work=Geological Society of America Special Papers |volume=178 |pages=1–74 |url=https://pubs.geoscienceworld.org/books/book/301/chapter/3795487/ |access-date=2024-07-09 |publisher=Geological Society of America |language=en |doi=10.1130/spe178-p1 |isbn=978-0-8137-2178-1 |last2=Silberling |first2=N. J.|url-access=subscription }} The member was named for Fossil Hill, Nevada, a locality within the Humboldt Mountains where large quantities of Anisian-aged marine fossils were discovered in the early 20th century. Fossils are common throughout the Fossil Hill, and the unit is well known for preserving the remains of some of the earliest marine reptiles, including several genera of ichthyosaurs and a pistosaur.{{Cite journal |last1=Sander |first1=P. Martin |last2=Griebeler |first2=Eva Maria |last3=Klein |first3=Nicole |last4=Juarbe |first4=Jorge Velez |last5=Wintrich |first5=Tanja |last6=Revell |first6=Liam J. |last7=Schmitz |first7=Lars |date=2021-12-24 |title=Early giant reveals faster evolution of large body size in ichthyosaurs than in cetaceans |url=https://www.science.org/doi/10.1126/science.abf5787 |journal=Science |language=en |volume=374 |issue=6575 |doi=10.1126/science.abf5787 |issn=0036-8075|url-access=subscription }} Other fossils include bony fish, hybodont sharks, and invertebrates with ceratitid ammonoids being especially abundant.{{Cite web |last=((Various Contributors to the Paleobiology Database)) |title=Fossilworks: Gateway to the Paleobiology Database |url=https://www.fossilworks.org}}
History
The Fossil Hill Member was first recognized for its paleontological resources at the end of the 19th century. John Campbell Merriam and Eustace Furlong from the University of California Berkeley led the Saurian Expedition of 1905 to Fossil Hill in the Humboldt Mountains with the intention to search for Ichthyosaur fossils. The expedition was joined by the venerable heiress Annie Alexander who financed the expedition and provided most of the written documentation through journal entries and photographs.{{Cite web |title=1905 Saurian Expedition |url=https://ucmp.berkeley.edu/about-ucmp/history-of-ucmp/saurian-expedition-1905/ |access-date=2024-10-10 |website=ucmp.berkeley.edu}} The expedition excavated the remains of 25 Triassic Ichthyosaurs, many of which were collected and shipped back to Berkeley. These skeletons, along with those collected from subsequent expeditions by UC Berkeley in the early 20th century, were the most complete Ichthyosaur specimens from North America at the time, and Merriam's study of these fossils provided some of the earliest knowledge on early ichthyosaur evolution. {{multiple image
| total_width = 330
| align = right
| direction = vertical
| image1 = Cymbospondylus_petrinus_skull.jpg
| image2 = The Osteology of the Reptiles-275 kijhv jh ghj.png
| alt1 = Drawing of a gray ichthyosaur skull on a white background
| alt2 = Drawing of an ichthyosaur skeleton on white background
| footer = Sketches representing the skull and fossil skeleton of UCMP 9950, one of the specimens of C. petrinus having been discovered during expeditions led by the University of California at the beginning of the 20th century
}}In the latter half of the 20th century, the section of Fossil Hill Member outcropping in the Augusta Mountains was identified for its ammonoid record to be used in biostratigraphic definition and correlation of Triassic rocks.{{Cite journal |last=Silberling |first=Norman J. |last2=Nichols |first2=K.M. |date=1982 |title=Middle Triassic molluscan fossils of biostratigraphic significance from the Humboldt Range, northwestern Nevada |url=http://dx.doi.org/10.3133/pp1207 |journal=Professional Paper |doi=10.3133/pp1207 |issn=2330-7102}} Field observations of vertebrate fossils in the Augusta Mountains drew the attention of paleontologist Martin Sander who has led numerous teams to collect marine reptile fossils including specimens representing 7 new species. Paleontological fieldwork and research in the Augusta Mountains is ongoing.
Geology
= Stratigraphy =
The Favret Formation and the Prida Formation, constitute two of the recognized geological formations within the Star Peak Group, of Northwestern Nevada. The Fossil Hill member links these two formations.
Tectonic fragmentation of the region has broken apart most stratigraphic units of the Star Peak Group. Because of this outcrop discontinuity, the Fossil Hill Member is part of different formations in different parts of the outcrop area. In the Prida Formation, this member outcrops west of the Humboldt Range, and in the Favret Formation, it outcrops in the Augusta Mountains and southern extent of the Tobin Range. Although differing in precise age, the strata assigned to this member form a laterally uniform unit of offshore calcareous rocks. The various occurrences of the Fossil Hill member are also united by a distinct pelagic Anisian paleofauna preserved in the rocks.
The Fossil Hill varies in thickness throughout its outcrops. In the China Mountain and Tobin Range sections, erosion and dolomitization from overlying units have rendered the Fossil Hill usually thin or locally absent. The unit within the Prida Formation varies from 60 to 120 meters thick while the section in the Augusta Mountains exceeds 250 meters.
Silty shale is the prevailing lithology throughout the Fossil Hill Member outcropping in the Augusta Mountains with alternating facies of fissile shaley limestone and massive black limestones common throughout the entire section. Specific bioclastic beds dominated by Daonella fossils occur at multiple intervals within the shaley limestones. Compressed ammonoid fossils are also common. Three dimensionally preserved ammonoids occur less commonly but are still present in multiple areas. These three dimensional ammonoids are less prone to weathering and are useful for biostratigraphy.
Paleobiota
= Ichthyosaurs =
| class="wikitable"
|+ !Genus !Species !Material !Notes !Images |
| rowspan="4" |Cymbospondylus
|C. petrinus{{Cite book |last=Campbell |first=John C. |url=https://www.biodiversitylibrary.org/item/60829#page/9/mode/1up |title=Triassic Ichthyosauria, with special reference to the American forms |publisher=The University Press |year=1908 |series=Memoirs of the University of California |volume=1 |location=Berkeley, California |pages=1–196}} |Multiple specimens of excellent quality from both the Favret and Prida Formations including UCMP 9950, a near-complete specimen from Fossil Hill. |A large cymbospondylid ichthyosaur varying in size from {{convert|8-12|m|ft}}. |
| C. nichollsi{{Cite journal |last1=FRÖBISCH |first1=NADIA B. |last2=SANDER |first2=P. MARTIN |last3=RIEPPEL |first3=OLIVIER |date=2006 |title=A new species of Cymbospondylus (Diapsida, Ichthyosauria) from the Middle Triassic of Nevada and a re-evaluation of the skull osteology of the genus |url=http://dx.doi.org/10.1111/j.1096-3642.2006.00225.x |journal=Zoological Journal of the Linnean Society |volume=147 |issue=4 |pages=515–538 |doi=10.1111/j.1096-3642.2006.00225.x |issn=1096-3642}}
| FMNH PR2251, from the Favret Formation, consists of the back half of a skull, the first 28 vertebrae, several ribs, and part of the shoulder girdle | Mid-sized species of Cymbospondylus, estimated to be about {{convert|7.6|m|ft}} long |
| C. duelfiri{{Cite journal |last1=Klein |first1=Nicole |last2=Schmitz |first2=Lars |last3=Wintrich |first3=Tanja |last4=Sander |first4=P. Martin |date=2020-04-20 |title=A new cymbospondylid ichthyosaur (Ichthyosauria) from the Middle Triassic (Anisian) of the Augusta Mountains, Nevada, USA |url=http://dx.doi.org/10.1080/14772019.2020.1748132 |journal=Journal of Systematic Palaeontology |volume=18 |issue=14 |pages=1167–1191 |doi=10.1080/14772019.2020.1748132 |bibcode=2020JSPal..18.1167K |issn=1477-2019|url-access=subscription }}
|LACM DI 158109 consists of a nearly complete skull with articulated and disarticulated post cranial material. Diminutive strings of articulated fetal vertebrae in the trunk. |The smallest species of the genus at {{convert|4.3|m|ft}} long, holotype is among the earliest examples of viviparity |
| C. youngorum
|LACM DI 157871, consists of a large complete skull, some cervical vertebrae, the right humerus as well as fragments of the shoulder girdle. |A giant, {{convert|17|m|ft}} long ichthyosaur; among the largest animals known up to this point in time |
| Omphalosaurus
|Multiple specimens from both the Fossil Hill locality and the Favret formation. |A medium-sized—{{convert|5|m|ft}}—basal ichthyosaur with dental batteries of button shaped teeth and a presumed durophage |
| rowspan="2" |Phalarodon
|Multiple specimens from the Fossil Hill and Augusta Mountain localities |A small, {{convert|1|m|ft}} long mixosaur |
| P. callowayi
| | Holotype found in the same beds as Augustasaurus |File:PhalarodonDB15.jpg of Phalarodon]] |
| Thalattoarchon
|FMNH PR 3032, consists of a major part of the skull and the axial skeleton, including parts of the pelvic girdle and rear flippers |A large ichthyosaur with large, laterally compressed teeth, interpreted as a macropredator |File:Thalattoarchon_saurophagis.jpg and size comparison of a T. saurophagis with a human]] |
= Sauropterygians =
A partial femur attributed to a nothosaurid (possibly Corosaurus) and an interclavicle putatively attributed to a thalattosaur have been uncovered from outcroppings of the Fossil Hill Member in the Favret Formation.
| class="wikitable"
|+ !Genus !Species !Material !Notes !Images |
| Augustasaurus
|Single specimen. FMNH PR 1974 is a partial articulated skeleton containing the posterior neck, trunk, shoulder girdle, and both forelimbs and a disassociated skull, |A pistosauroid from the Favret Formation |
= Pseudosuchians =
| class="wikitable"
|+ !Genus !Species !Material !Notes !Images |
| Benggwigwishingasuchus
|A single, mostly complete skeleton (LACM-DI 158616) |A poposauroid pseudosuchian from the Favret Formation, specimen was probably a terrestrial animal washed out to sea |
=Actinopterygians=
Various bones including opercular remains, jaw fragments, and scales have been found that are not attributable to any specific taxon.
| class="wikitable"
|+ !Genus !Species !Material !Notes !Images |
| Saurichthys
|FMNH PR 1800, parts of a relatively large upper and lower jaw; FMNH PR 1801, a mostly complete skull roof and an operculum |
=Chondrichthyans=
| class="wikitable"
|+ !Genus !Species !Material !Notes !Images |
| rowspan="4"|Acrodus
| A. cuneocostatus | A complete tooth (the holotype, FMNH PF 14857) with 27 teeth of varying completenessG. Cuny, O. Rieppel, and P. M. Sander. 2001. The shark fauna from the Middle Triassic (Anisian) of north-western Nevada. Zoological Journal of the Linnean Society 133:285-301 | An acrodontid hybodontiform | |
| A. cf. oreodontus
| Referred to A. oreodontus, but not confidently | |
| A. spitzbergensis
| | |
| A. cf. vermicularis
| Distinct from A. spitzbergensis, but possibly indeterminate | |
| Hybodus
| H. sp. | Not referrable to any of the named species of Hybodus | File:Hybodus hauffianus.png known in hybodonts]] |
| Mucrovenator
| M. minimus | 22 teeth, including the holotype (FMNH PF 15020) | A synechodontiform euselachian | |
| rowspan="2"| Palaeobates
| P. cf. shastaensis | Previously assigned to the genus Strophodus | |
| P. sp.
| A polyacrodontid hybodontiform, too incomplete to assign to any of the named species of Palaeobates | |
| Palaeospinax
| P. sp. | A synechodontiform shark with teeth superficially similar to Hybodus | | |
| rowspan="2"| Polyacrodus
| P. bucheri | One incomplete tooth (the holotype, FMNH PF 14969) and 14 other teeth of varying completness | | |
| P. tregoi
| 31 teeth, none of them fully complete | | |
=Molluscs=
;Ammonites
{{columns-list|colwidth=15em|
- Acrochordiceras hatschekii
- A. carolinae
- A. hatschekii
- A. hyattiH. Bucher. 1988. A new Middle Anisian (Middle Triassic) ammonoid zone from northwestern Nevada. Eclogae Geologicae Helvetiae 81(3):723-762
- Alanites
- A. mulleri
- A. obesus
- Anagymnotoceras spivaki
- Aplococeras
- A. parvus
- A. smithi
- A. vogdesi
- Atractites
- A. clavatulus
- A. solidus
- A. "sp. A"
- A. "sp. B"
- A. "sp. C"
- Augustaceras
- A. escheri
- A. staffordi
- Brackites vogdesi
- Calliconites nevadensis
- Caucasites nicholsi
- Constrigymnites robertsi
- Discoptychites sp.
- Eogymnotoceras thompsoni
- Epigymnites alexandrae
- Eutomoceras
- E. dalli
- E. dunni
- E. lahontanum
- E. laubei
- Frechites
- F. nevadanus
- F. occidentalis
- Grambergia sp.
- Groenlandites
- G. merriami
- G. pridaense
- Gymnites
- G. billingsi
- G. perplanus
- Gymnotoceras
- G. blakei
- G. rotelliformis
- Hollandites congressensis
- Humboldtites septentrionalis
- Intornites
- I. mctaggarti
- I. nevadanus
- Isculites tozeri
- Japonites
- J. surgriva
- J. welteriH. Bucher. 1989. Lower Anisian ammonoids from the northern Humboldt Range (northwestern Nevada, USA) and their bearing upon the Lower-Middle Triassic boundary. Eclogae Geologicae Helvetiae 82:945-1002
- Kocaelia sp.
- Leiophyllites sp.
- Longobardites
- L. parvus
- L. zsigmondyi
- Metadagnoceras youngi
- Metadinarites desertorus
- Nevadisculites
- N. smithi
- N. taylori
- Nevadites
- N. humboldtensis
- N. hyatti
- Nicholsites tozeri
- Paracrochordiceras
- P. americanum
- P. mclearni
- P. plicatus
- P. silberlingsi
- P. sp.
- Paradanubites crassicostatus
- Parafrechites meeki
- Paranevadites
- P. furlongi
- P. gabbi
- Platycuccoceras
- P. bonaevistae
- P. favretense
- Proarcestes
- P. balfouri
- P. gabbi
- Pseudodanubites nicholsi
- Pseudokeyserlingites guexi
- Ptychites sp.
- Sageceras walteri
- Silberlingites
- S. cricki
- S. mulleri
- S. tregoi
- Silberlingitoides
- S. clarkei
- S. cricki
- Stenopopanoceras sp.
- Sturia japonica
- Thanamites contractus
- Tozerites
- T. gemmellaroi
- T. humboldtensis
- T. polygyratus
- Trematoceras elegans
- Tropigastrites
- T. lahontanus
- T. louderbacki
- Tropigymnites planorbis
- Ussurites
- U. arthaberi
- U. detwilleri
- U. sp.
}}
;Bivalves
- Daonella
- D. americana
- D. dubia
- D. moussoni
- D. sturi
;Nautiloids
See also
References
{{reflist}}
{{Chronostratigraphy of Nevada}}
Category:Triassic geology of Nevada
Category:Geologic formations of the United States
Category:Natural history of Nevada
Category:Stratigraphy of Nevada
Category:Triassic System of North America
Category:Shale formations of the United States
Category:Fossiliferous stratigraphic units of North America