Paris biota | |
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Stratigraphic range: earliest Spathian, ~ | |
Type | Geological formation |
Lithology | |
Primary | Shale, limestone, siltstone |
Location | |
Region | Idaho and Nevada, United States |
Country | USA |
The Paris biota is an exceptionally diverse Early Triassic (approximately 249 million years ago) [1] fossil assemblage described in 2017 from the Lower Shale Member of the Thaynes Group. It was first discovered in Paris Canyon, west of the town of Paris in Bear Lake County, southeastern Idaho, United States. [2] This biota was later also found in coeval and slightly younger beds in northeastern Nevada (Elko County) and Bear Lake and Caribou counties, southeastern Idaho. [3]
The Paris biota was found in layers dating back to the earliest Spathian, a substage of the Olenekian stage of the Early Triassic epoch. The biostratigraphy is constrained by the presence of the ammonoids Tirolites and Bajarunia , and conodonts. [2] [3] The Tirolites/ Columbites beds are dated with 248.853±0.086 Ma. [1] The Paris biota was later also discovered in slightly younger beds in Immigrant Canyon, northeastern Nevada, associated with the ammonoid index fossils Prohungarites sp. and Neopopanoceras haugi , which point to a middle–late Spathian age. [3]
The organisms of the Paris biota lived in a shallow marine epicontinental sea (western USA basin) on the western coast of Pangea. The sites were located in a near-equatorial position during the Early Triassic epoch. [2] [3]
The Spathian aged Paris biota is one of the earliest diverse fossil assemblages from the post-extinction interval, about 3 million years ago [1] [4] after the Permian-Triassic mass extinction, and the first one in the wake of the Smithian-Spathian boundary extinction.
The Paris biota comprises fossils belonging to 20 orders or seven phyla: (1) Retaria (foraminifers) [2] (2) sponges, (3) brachiopods (4) mollusks, (5) arthropods, (6) echinoderms and (7) chordates (vertebrates). The assemblage also contains fossil algae and coprolites (trace fossils). Ammonoids and bivalves dominate the fauna. [2] It combines Palaeozoic survivors with members of the Modern evolutionary fauna (i.e., groups that are typical for the Mesozoic and Cenozoic). The Paris biota therefore provides a glimpse at the faunal turnover associated with the largest mass extinction in Earth's history. For example, the biota includes leptomitid protomonaxonid sponges, a group that is otherwise known from the early Paleozoic era (e.g. from the Cambrian Burgess Shale of western Canada). Among the modern clades, it contains a gladius-bearing coleoid cephalopod ( Idahoteuthis ).
The preservation of Paris biota organisms is considered taxon-dependent, but is not fully understood. [5] The study of some fossils could be improved using synchrotron μXRF imaging. [6]
Most organisms of the Paris biota were described in a thematic issue of the journal Geobios in 2019, [7] but new taxa were also subsequently described.
In 2023, another diverse post-extinction biota was presented from South China, the Dienerian aged Guiyang biota, [8] which includes fossils belonging to twelve classes and 19 orders. The Early Triassic is generally considered as an environmentally unstable and diversity-poor interval, [2] highlighting the importance of the discovery of such diverse lagerstätten.
The following taxa (animals sorted by phylum) were either reported or described from the Paris biota (not listed are the foraminifera and conodonts, which have not yet been described):
Color key
| Notes Uncertain or tentative taxa are in small text; |
Porifera of the Paris biota | ||
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Taxon / Genus | Species | Notes |
Pseudoleptomitus | P. advenus | A leptomitid protomonaxonid sponge similar to Leptomitus . This group was previously only known from the Cambrian and Ordovician periods [9] |
Color key
| Notes Uncertain or tentative taxa are in small text; |
Brachiopoda of the Paris biota | ||
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Taxon / Genus | Species | Notes |
Brachiopoda | Gen. et sp. indet. | An epizoan species closely associated with the sponges [3] |
Lingularia | L. borealis | A lingulid [3] |
Rhynchonellata | Gen. et sp. indet. | A brachiopod [3] |
Color key
| Notes Uncertain or tentative taxa are in small text; |
Mollusca of the Paris biota | ||
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Taxon / Genus | Species | Notes |
Albanites | A. americanus | An ammonoid cephalopod [10] |
Avichlamys ? | A.? csopakensis? | A pectinid bivalve [3] |
Bajarunia | B. cf. pilata | An ammonoid cephalopod typical of the earliest Spathian substage [10] |
Belemnoidea | Gen. et sp. indet. | Arm hooks of a belemnoid [2] |
Caribouceras | C. slugense | An endemic ammonoid cephalopod [10] |
Columbites | C. parisianus | An ammonoid cephalopod [10] |
Coscaites | C. crassus | An ammonoid cephalopod [10] |
Critendenia | C. kummeli | A bivalve [3] |
Crittendenia sp. | A claraiid bivalve [3] | |
Eumorphotis | E. cf. ericius | A heteropectinid bivalve [3] |
E. multiformis? | A heteropectinid bivalve [3] | |
Eumorphotis sp. | A heteropectinid bivalve [3] | |
Hedenstroemiidae | Gen. et sp. indet. | An ammonoid cephalopod [10] |
Idahoteuthis | I. parisiana | A gladius-bearing coleoid cephalopod [11] |
Leptochondria | L. curtocardinalis | A hunanopectinid bivalve [3] |
L. nuetzeli? | A hunanopectinid bivalve [3] | |
L. occidanea | A hunanopectinid bivalve [3] | |
L. virgalensis? | A hunanopectinid bivalve [3] | |
Leptochondria sp. | A hunanopectinid bivalve [3] | |
Phaedrysmocheilus | P. idahoensis | A nautiloid cephalopod [10] |
Pleuronectites | P. meeki | A pectinid bivalve [3] |
Scythentolium | Scythentolium sp. | A entoliid bivalve [3] |
Tirolites | T. harti | An ammonoid cephalopod typical of the earliest Spathian substage [10] |
T. aff. cassianus | An ammonoid cephalopod typical for the earliest Spathian substage [10] | |
Trematoceras | Trematoceras sp. | An orthoconic nautiloid cephalopod [10] |
Color key
| Notes Uncertain or tentative taxa are in small text; |
Arthropoda of the Paris biota | ||
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Taxon / Genus | Species | Notes |
Aeger | Aeger sp. | An aegerid prawn [12] |
Anisaeger | A. longirostrus | An aegerid prawn [12] |
Ankitokazocaris | A. triassica | A thylacocephalan [13] |
Caridea | Gen. et sp. indet. | A shrimp [2] [3] |
Hoplocarida | Gen. et sp. indet. | A malacostracan crustacean [3] |
Ligulacaris | L. parisiana | A thylacocephalan [13] |
Limulidae? | Gen. et sp. indet. | A xiphosuran chelicerate [3] |
Litogaster | L. turnbullensis? | A glypheid pleocyemate crustacean [3] [12] |
Litogaster sp. | A glypheid pleocyemate crustacean [3] | |
Penaeoidea | Gen. et sp. indet. | A prawn [2] [3] |
Pemphix | P. krumenackeri | A glypheid pleocyemate crustacean [12] |
Thylacocephala | Gen. et sp. indet. | A thylacocephalan [3] |
Triassosculda | T. ahyongi | A mantis shrimp [14] |
Color key
| Notes Uncertain or tentative taxa are in small text; |
Echinodermata of the Paris biota | ||
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Taxon / Genus | Species | Notes |
Holocrinus | Holocrinus nov. sp. | A sea lily [15] |
Shoshonura | S. brayardi | An ophiacanthid brittle star [16] |
Color key
| Notes Uncertain or tentative taxa are in small text; |
Chordata of the Paris biota | ||
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Taxon / Genus | Species | Notes |
Actinistia | Gen. et sp. indet. | Coelacanth remains [3] |
Bobasatrania | Bobasatrania sp. | A bobasatraniiform ray-finned fish. Complete specimens [3] |
Hybodontiformes | Gen. et sp. indet. A | A slab with several hybodontiform chondrichthyan teeth showing a heterodont durophagous dentition [17] |
Gen. et sp. indet. B | A single hybodontiform tooth [17] | |
Osteichthyes | Gen. et sp. indet. | Tooth plate [2] |
Vertebrata | indet. | coprolites referrable to large vertebrate producers [2] |
Color key
| Notes Uncertain or tentative taxa are in small text; |
Algae of the Paris biota | ||
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Taxon / Genus | Species | Notes |
Algae | Gen. et ap. indet. | Filamental algae and other algae [3] |
Dasycladales | Gen. et ap. indet. | An unicellular green algae [3] |
Rhodophyta | Gen. et ap. indet. | A red algae [3] |
Approximately 251.9 million years ago, the Permian–Triassicextinction event forms the boundary between the Permian and Triassic geologic periods, and with them the Paleozoic and Mesozoic eras. It is the Earth's most severe known extinction event, with the extinction of 57% of biological families, 83% of genera, 81% of marine species and 70% of terrestrial vertebrate species. It is also the largest known mass extinction of insects. It is the largest of the "Big Five" mass extinctions of the Phanerozoic. There is evidence for one to three distinct pulses, or phases, of extinction.
The Triassic is a geologic period and system which spans 50.5 million years from the end of the Permian Period 251.902 million years ago (Mya), to the beginning of the Jurassic Period 201.4 Mya. The Triassic is the first and shortest period of the Mesozoic Era. Both the start and end of the period are marked by major extinction events. The Triassic Period is subdivided into three epochs: Early Triassic, Middle Triassic and Late Triassic.
A Lagerstätte is a sedimentary deposit that exhibits extraordinary fossils with exceptional preservation—sometimes including preserved soft tissues. These formations may have resulted from carcass burial in an anoxic environment with minimal bacteria, thus delaying the decomposition of both gross and fine biological features until long after a durable impression was created in the surrounding matrix. Lagerstätten span geological time from the Neoproterozoic era to the present. Worldwide, some of the best examples of near-perfect fossilization are the Cambrian Maotianshan shales and Burgess Shale, the Ordovician Soom Shale, the Silurian Waukesha Biota, the Devonian Hunsrück Slates and Gogo Formation, the Carboniferous Mazon Creek, the Triassic Madygen Formation, the Jurassic Posidonia Shale and Solnhofen Limestone, the Cretaceous Yixian, Santana, and Agua Nueva formations, the Eocene Green River Formation, the Miocene Foulden Maar and Ashfall Fossil Beds, the Pliocene Gray Fossil Site, the Pleistocene Naracoorte Caves, the La Brea Tar Pits, and the Tanis Fossil Site.
Aeger is a genus of fossil prawns. They first occur in the Early Triassic, and died out at the end of the Late Cretaceous. A total of 21 species are known.
The Early Triassic is the first of three epochs of the Triassic Period of the geologic timescale. It spans the time between 251.9 Ma and 247.2 Ma. Rocks from this epoch are collectively known as the Lower Triassic Series, which is a unit in chronostratigraphy.
In the geologic timescale, the Olenekian is an age in the Early Triassic epoch; in chronostratigraphy, it is a stage in the Lower Triassic series. It spans the time between 251.2 Ma and 247.2 Ma. The Olenekian is sometimes divided into the Smithian and the Spathian subages or substages. The Olenekian follows the Induan and is followed by the Anisian.
The Induan is the first age of the Early Triassic epoch in the geologic timescale, or the lowest stage of the Lower Triassic series in chronostratigraphy. It spans the time between 251.9 Ma and 251.2 Ma. The Induan is sometimes divided into the Griesbachian and the Dienerian subages or substages. The Induan is preceded by the Changhsingian and is followed by the Olenekian.
Anasibirites is an extinct genus of ammonoid cephalopod from the lower upper Smithian Wasatchites distractus Zone.
Acrodus is an extinct genus of hybodont spanning from the Early Triassic to the Late Jurassic. It was durophagous, with blunt, broad teeth designed for crushing and grinding. Some Middle Triassic species have been suggested to have grown to lengths of 1.8–2.5 metres (5.9–8.2 ft). Species are known from both marine and freshwater environments, with all Middle and Late Jurassic species only known from freshwater.
Boreosomus is an extinct genus of Triassic ray-finned fish. It was first described from the Arctic island of Spitsbergen, but was later also discovered in other parts of the world. The type species is Boreosomus arcticus.
Aegeridae is a family of fossil prawns, one of the earliest Mesozoic shrimp families. It contains the genera Aeger, Acanthochirana, Anisaeger and Distaeger. The main diagnostic character of Aegeridae is the presence of numerous spines or thin setae on the third maxilliped.
The Thaynes Group, Thaynes Formation in older literature, is a geologic group in eastern Idaho, western Wyoming, Utah and eastern Nevada. It includes the Sinbad Formation, Virgin Formation and Shnabkaib Formation. The Thaynes Group is of marine origin. Its formations are interbedded with layers of the non-marine Moenkopi Group.
Protomonaxonida is an extinct order of sea sponges. It is a paraphyletic group gathering the most ancient species from the Burgess Shale to modern sponges.
Tirolites is an extinct genus of ammonoid cephalopod. Its first appearance defines the Smithian-Spathian boundary in the Olenekian stage of the Early Triassic epoch. It is prominent in the Paris biota.
The Guiyang biota is an exceptionally preserved Early Triassic fossil assemblage from the Daye Formation near Guiyang (China), discovered between 2015 and 2019 and first reported in 2023. It is the oldest known Mesozoic lagerstätte, and it provides evidence of the existence of a complex marine ecosystem shortly after the Permian–Triassic extinction event.
Anisaeger is a genus of fossil prawns first described from the Luoping biota of the middle Triassic of China but also known from the Guiyang biota and Paris biota of the early Triassic. It includes three species, A. brevirostrus, A. longirostrus and A. spiniferus.
Triassosculda is an extinct genus of mantis shrimp from the Early Triassic aged Paris biota of Idaho. Its discovery bridged a 100-million-year gap in mantis shrimp evolution from the late Carboniferous to the Jurassic. Its only species is T. ahyongi.
Tyrannosculda is an extinct genus of mantis shrimp which lived during the Late Jurassic in southern Germany. It was named in 2021, with T. laurae as the type and only species. Several fossil specimens are known, representing various growth stages.
Sculdidae is a family of fossil mantis shrimps which lived from the late Jurassic to late Cretaceous periods. It was erected in 1886 to contain the type genus Sculda, and other genera have since been assigned to it. Fossils of sculdids have been found in Germany, Lebanon and the United States. The family may be polyphyletic.
Chabardella is an extinct genus of mantis shrimp which lived during the Late Carboniferous in France. It was named in 2009, with C. spinosa as the type and only species.