Английская Википедия:Agardhfjellet Formation
Шаблон:Short description Шаблон:Infobox rockunit
The Agardhfjellet Formation is a geologic formation in Svalbard, Norway. It preserves fossils dating back to the Oxfordian to Berriasian stages, spanning the Late Jurassic-Early Cretaceous boundary.[1] The formation contains the Slottsmøya Member, a highly fossiliferous unit (Lagerstätte) where many ichthyosaur and plesiosaur fossils have been found, as well as abundant and well preserved fossils of invertebrates.[2][3]
Description
The formation overlies the Knorringfjellet Formation and is overlain by the Rurikfjellet Formation. The formation comprises the lower Oppdalsåta and upper Slottsmøya Members. The Slottsmøya Member, which averages Шаблон:Convert in thickness in the study area, consists of dark-grey to black silty mudstone, often weathering to paper shale, and discontinuous silty beds with local occurrences of red to yellowish sideritic concretions as well as siderite and dolomite interbeds.[3] It consists of a mix of shales and siltstones which were deposited in a shallow marine environment, near a patch of deeper marine sediment.[4] The seafloor, which was located about Шаблон:Convert below the surface, seems to have been relatively dysoxic, or oxygen-poor, although the diversity of the benthic fauna suggest that these environments were likely not truly anoxic and that oxygen-depletion may have been a seasonal phenomenon.[5][6] Although direct evidence from Slottsmøya is currently lacking, the high latitude of this site and relatively cool global climate of the Tithonian suggest that some sea ice may have been present at least in the winter. [7][8]
These sites represent shallow-water methane seeps which were spread over a relatively large geographic area, and like modern day seeps, they supported high biodiversity. Near the top of the member, various assemblages of invertebrates have been discovered; these include ammonites, bivalves, lingulate brachiopods, rhynchonellate brachiopods, tubeworms, belemnoids, tusk shells, sponges, crinoids, sea urchins, brittle stars, starfish, crustaceans, and gastropods, numbering 54 taxa in total. The most common and abundant of these taxa were bivalves and brachiopods, each of which make up 27.8% of the known seep fauna. Several chemosymbiotic species are known, such as the bivalve Nucinella.[5] Outside of the cold seeps, several non-seep-restricted invertebrates were also present in abundance.[6] In addition to the invertebrates, the Slottsmøya Member has also revealed a diverse assemblage of marine reptiles, including several taxa of ichthyosaurs and plesiosaurs. Many of these specimens are relatively complete and in articulation, which is rare among Jurassic marine fossil sites.[6] It thus provides a unique and detailed glimpse into the boreal seas of the Late Jurassic. As it spans the Jurassic-Cretaceous boundary, it is also important to understanding how marine ecosystems changed going into the Cretaceous.
Paleobiota
Шаблон:Paleobiota-key-compact The formation, especially the Slottsmøya Member, has provided an abundance of marine fossils dating to the Late Jurassic-Early Cretaceous.[3]
The timeline below follows stratigraphic data provided in Delsett et al. 2018 and Roberts et al. 2020. [9][10] <timeline> ImageSize = width:1000px height:auto barincrement:15px PlotArea = left:10px bottom:50px top:10px right:10px
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Colors =
#legends id:CAR value:blue id:ANK value:rgb(0.4,0.3,0.196) id:HER value:green id:HAD value:blue id:black value:black id:white value:white id:tithonian value:rgb(0.675,0.675,0.35) id:berriasian value:rgb(0.753,0.753,0.486)
BarData=
bar:eratop bar:space bar:periodtop bar:space bar:NAM1 bar:NAM2 bar:NAM3 bar:NAM4 bar:NAM5 bar:NAM6 bar:NAM7 bar:NAM8 bar:NAM9 bar:NAM10 bar:NAM11
bar:space bar:period bar:space bar:era
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align:center textcolor:black fontsize:M mark:(line,black) width:25 shift:(7,-4)
bar:periodtop from: -145 till: -141 color:berriasian text:Berriasian from: -152.1 till: -145 color:tithonian text:Tithonian
bar:eratop from: -152.1 till: -141 color:CAR text:Vertebrate Biostratigraphy of the Slottsmøya Member
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align:left fontsize:M mark:(line,white) width:5 anchor:till align:left
color:HAD bar:NAM1 from:-148.5 till:-147.5 text:Colymbosaurus svalbardensis color:HAD bar:NAM2 from:-149.3 till:-148.3 text:Djupedalia engeri color:HAD bar:NAM3 from:-148 till:-147 text:Spitrasaurus larseni color:HAD bar:NAM4 from:-146.4 till:-145.8 text:Spitrasaurus wensaasi color:HAD bar:NAM5 from:-145.3 till:-144.7 text:Ophthalmothule cryostea color:HAD bar:NAM6 from:-148.5 till:-146.3 text:Pliosaurus funkei color:HER bar:NAM7 from:-147.3 till:-146.3 text:Undorosaurus gorodischensis color:HER bar:NAM8 from:-151.5 till:-150.5 text:Arthropterygius lundi color:HER bar:NAM9 from:-148.5 till:-147.5 text:Arthropterygius hoybergeti color:HER bar:NAM10 from:-148 till:-144.5 text:Arthropterygius chrisorum color:HER bar:NAM11 from:-145.2 till:-144.5 text:Nannopterygius borealis
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align:center textcolor:black fontsize:M mark:(line,black) width:25
bar:era from: -152.1 till: -141 color:CAR text:Vertebrate Biostratigraphy of the Slottsmøya Member
</timeline>
Vertebrates
Bony fish
Bony fish from the Agardhfjellet Formation | ||||||
---|---|---|---|---|---|---|
Genus | Species | Location | Member | Material | Notes | Images |
Leptolepis[11] | L. nathorsti | Oppdalssåta & Lardyfjellet Members |
Plesiosaurs
Plesiosaurs from the Agardhfjellet Formation | ||||||
---|---|---|---|---|---|---|
Genus | Species | Location | Member | Material | Notes | Images |
T. svalbardensis |
Slottsmøya Member |
Reassigned to the genus Colymbosaurus after further analysis[12] | ||||
Colymbosaurus | C. svalbardensis | Slottsmøya Member | A colymbosaurine cryptoclidid, also known from the Kimmeridge Clay | |||
Djupedalia | D. engeri | Slottsmøya Member | A cryptoclidid plesiosaur | |||
Ophthalmothule | O. cryostea | Slottsmøya Member | Extensive skeletal material including a complete cranium | A cryptoclidid plesisosaur which has unusually large orbits.[10] | ||
Spitrasaurus | S. wensaasi | Slottsmøya Member | A cryptoclidid plesiosaur related to Ophthalmothule | |||
S. larseni | ||||||
Pliosaurus | P. funkei | Slottsmøya Member | Known from two partial skeletons | A large thalassophonean pliosaurid which was informally known as "Predator X" prior to being named. This species is notable for having unusually large paddles in comparison to its body size. |
Ichthyosaurs
Ichthyosaurs from the Agardhfjellet Formation | ||||||
---|---|---|---|---|---|---|
Genus | Species | Location | Member | Material | Notes | Images |
Cryopterygius | C. kristiansenae | Slottsmøya Member | Junior synonym of Undorosaurus gorodischensis | |||
Undorosaurus | U. gorodischensis | Slottsmøya Member | A single, largely complete specimen | A large platypterygiine ichthyosaur, also known from the Russian Volga.[13] | ||
Janusaurus | J. lundi | Slottsmøya Member | Junior synonym of Arthropterygius lundi | |||
Palvennia | P. hoybergeti | Slottsmøya Member | Junior synonym of A. hoybergeti | |||
Keilhauia | K. nui | Slottsmøya Member | A nomen dubium referred to A. sp. cf. chrisorum | |||
Arthropterygius | A. lundi | Slottsmøya Member | Several specimens of varying ages, previously referred to several other genera | A widespread genus of ophthalmosaurid ichthyosaur, also known from Canada, Russia, and Argentina. Is present both before and directly after the Jurassic-Cretaceous Boundary. [14] | ||
A. hoybergeti | ||||||
A. chrisorum | ||||||
Nannopterygius | N. borealis | Slottsmøya Member | An ophthalmosaurid ichthyosaur present in early Cretaceous strata. This genus is also known from the Kimmeridge Clay and from fossil sites in the Volga.[15] | |||
Brachypterygius | B. sp. | Slottsmøya Member | Partial skull | Referred to Brachypterygius by Angst et al. (2010)[16] |
Invertebrates
An unnamed galatheid squat lobster is known from a single, poorly preserved fragment.[5]
Cephalopods
Large belemnoid arm hooks are known.[17]
Cephalopods from the Agardhfjellet Formation | ||||||
---|---|---|---|---|---|---|
Genus | Species | Location | Member | Material | Notes | Images |
Craspedites[18] | C. okensis | Slottsmøya Member | ||||
C. originalis | ||||||
Borealites | B. rossicus | Slottsmøya Member | ||||
B. sp. | ||||||
Hectoroceras | H. kochi | Slottsmøya Member | ||||
H. sp. | ||||||
Kachpurites | K. sp. | Slottsmøya Member | ||||
Surites | S. spasskensis | Slottsmøya Member | ||||
S. spasskensoides | ||||||
S. tzikwinianus | ||||||
S. mesezhnikovi | ||||||
Tollia | T. tolli | Slottsmøya Member |
Echinoderms
Echinoderms from the Agardhfjellet Formation | ||||||
---|---|---|---|---|---|---|
Genus | Species | Location | Member | Material | Notes | Images |
Chariocrinus | C. sp. | Slottsmøya Member | A form of isocrinid crinoid | |||
Hemipedina | H. sp. | Slottsmøya Member | A species of pedinoid sea urchins related to the extant Caenopedina | |||
Polarasterias | P. janusensis | Slottsmøya Member | Nearly complete specimen | A forcipulatid sea star | ||
Savignaster | S. septemtrionalis | Slottsmøya Member | A pterasterid sea star | |||
Ophiogaleus | O. sp. | Slottsmøya Member | A ophiacanthid brittle star | |||
Ophioculina | O. hoybergia | Slottsmøya Member | An ophiurine brittle star |
Bivalves
Remains of possible anomiid clams have been found which are as yet undescribed.
Bivalves from the Agardhfjellet Formation | ||||||
---|---|---|---|---|---|---|
Genus | Species | Location | Member | Material | Notes | Images |
Pseudotrapezium | P. aff. groelandicum | Slottsmøya Member | An arcticid clam which constitutes nearly half of the fauna recovered from the seep assemblages. | |||
Mesosaccella | M. rogovi | Slottsmøya Member | ||||
M. toddi | ||||||
Nucinella | N. svalbardensis | Slottsmøya Member | The most abundant chemosymbiotic species in the Spitsbergen seeps. | |||
Buchia | B. sp | Slottsmøya Member | ||||
Solemya | S. cf. woodwardiana | Slottsmøya Member | A burrowing chemosymbiotic bivalve which is very abundant in the seep sites | |||
Tehamatea | T. rasmusseni | Slottsmøya Member | A lucinid clam | |||
Cretaxinus | C. hurumi | Slottsmøya Member | A thyacirid clam | |||
Camptonectes | C. spp | Slottsmøya Member | A pectinid clam represented by at least two species | |||
Oxytoma | O. octavia | Slottsmøya Member | ||||
Pseudolimea | P. arctica | Slottsmøya Member | ||||
Dacromya | D. chetaensis | Slottsmøya Member | Rare | |||
Goniomya | G. literata | Slottsmøya Member | Rare |
Serpulids
Serpulids from the Agardhfjellet Formation | ||||||
---|---|---|---|---|---|---|
Genus | Species | Location | Member | Material | Notes | Images |
Propomatoceros | P. sp. | Slottsmøya Member | A serpulid tube worm | |||
aff. Pyrgopolon | aff. P. nodulosum | Slottsmøya Member | A serpulid tube worm which forms mass accumulations in the Echinoderm Bed | |||
Nogrobs | N. sp. | Slottsmøya Member |
Brachiopods
Brachiopods from the Agardhfjellet Formation | ||||||
---|---|---|---|---|---|---|
Genus | Species | Location | Member | Material | Notes | Images |
Lingularia | L. similis | Slottsmøya Member | The most abundant species of brachiopod that is present in Slottsmøya | |||
Ptilorhynchia | P. mclachlani | Slottsmøya Member | A rhynchonellide brachiopod |
Gastropods
Gastropods from the Agardhfjellet Formation | ||||||
---|---|---|---|---|---|---|
Genus | Species | Location | Member | Material | Notes | Images |
Ambercyclus | A. sp. | Slottsmøya Member | The most abundant species of gastropod that is known from the Slottsmøya seep deposits | |||
Hudlestoniella | H. sp. | Slottsmøya Member | A rissoid gastropod | |||
Cantrainea | C. sp. | Slottsmøya Member | A turbinid gastropod; it is rare and only known from one of the seep sites |
See also
References
Bibliography
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- ↑ Шаблон:Cite thesis
- ↑ Delsett et al., 2019, p.741
- ↑ 3,0 3,1 3,2 Agardhfjellet Formation at Fossilworks.org
- ↑ Шаблон:Cite journal
- ↑ 5,0 5,1 5,2 Шаблон:Cite journal
- ↑ 6,0 6,1 6,2 Шаблон:Cite bookШаблон:Dead link
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- ↑ 10,0 10,1 Шаблон:Cite journal
- ↑ Шаблон:Cite journal
- ↑ E. M. Knutsen, P. S. Druckenmiller, and J. Hurum. 2012. Redescription and taxonomic clarification of ‘Tricleidus’ svalbardensis based on new material from the Agardhfjellet Formation (Middle Volgian). Norwegian Journal of Geology 92:175-186
- ↑ Шаблон:Cite journal
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