Trochammina as opportunist foraminifera in the Lower Jurassic from north Siberia

References

• Bailey T.R., Resenthal Y., McArthur J.M., van de Schootbrugge B., Thirlwall M.F. Paleoceanographic changes of the Late Pliensbachian–Early Toarcian interval: a possible link to the genesis of an oceanic anoxic event. Earth and Planetary Science Letters. 2003; 212: 307–320.
   Web of Science ®Google Scholar
• Bak K. Biostratigraphy of deep-water agglutinated foraminifera in Scaglia Rossa-type deposits of the Pienniny Klippen Belt, Carpathians, Poland. Grzybowski Foundation Special Publication. 2000; 7: 15–41.
   Google Scholar
• Bartolini A., Nocchi M., Baldanza A., Parisi G. Takayanagi Y., Saito T. Benthic life during the Early Toarcian Anoxic Event in the south western Tethyan Umbria-Marche Basin, central Italy. Studies in benthic foraminifera. Proceedings of the Fourth International Symposium on Benthic Foraminifera, Sendai, Japan, 1990. 1992; Sendai: Tokai University Press. 323–338.
   Google Scholar
• Boutakiout M., Elmi S. Tectonic and eustatic controls during the Lower and Middle Jurassic of the South Rif Ridge (Morocco) and their importance for the foraminifera-communities. Georesearch Forum. 1996; 1–2: 237–247.
   Google Scholar
• Butler J.N. Carbon dioxide equilibria and their applications. 1982; Reading, MA: Addison-Wesley.
   Google Scholar
• Clémence M.E., Gardin S., Bartolini A., Paris G., Beaumont V., Guex J. Bentho-planktonic evidence from the Austrian Alps for a decline in sea-surface carbonate production at the end of the Triassic. Swiss Journal of Geosciences. 2010; 103: 293–315.
   Web of Science ®Google Scholar
• Coccioni R., Luciani V. Planktonic foraminifera and environmental changes across the Bonarelli Event (OAE2, Latest Cenomanian) in its type area: a high-resolution study from the Tethyan reference Bottaccione section (Gubbio, Central Italy). Journal of Foraminiferal Research. 2004; 34: 109–129.
   Web of Science ®Google Scholar
• Corliss B.H. Morphology and microhabitat preferences of benthic foraminifera from the northwest Atlantic Ocean. Marine Micropaleontology. 1991; 17: 195–236.
   Web of Science ®Google Scholar
• Corliss B.H., Chen C. Morphotype patterns of Norwegian deep sea benthic foraminifera and ecological implications. Geology. 1988; 16: 716–719.
   Web of Science ®Google Scholar
• Dera G., Brigaud B., Monna F., Laffont R., Pucéat E., Deconinck J.F., Pellenard P., Joachimski M.M., Durlet C. Climatic ups and downs in disturbed Jurassic world. Geology. 2011; 39: 215–218.
   Web of Science ®Google Scholar
• Ernst S., Van der Zwaan B. Effects of experimentally induced raised levels of organic flux and oxygen depletion on a continental slope benthic foraminiferal community. Deep-Sea Research Part I. 2004; 51: 1709–1739.
   Google Scholar
• Fisher R.A., Corbet A.S., Williams C.B. The relations between the number of species and the number of individuals in a random sample of an animal population. Journal of Animal Ecology. 1943; 12: 42–58.
   Web of Science ®Google Scholar
• Ford D., Golonka J. Phanerozoic paleogeography, paleoenvironment and lithofacies maps of the circum-Atlantic margins. Marine and Petroleum Geology. 2003; 20: 249–285.
   Web of Science ®Google Scholar
• Friedrich O., Erbacher J., Wilson P.A., Moriya K., Mutterlose J. Paleoenvironmental changes across the Mid Cenomanian Event in the tropical Atlantic Ocean (Demerara Rise ODP Leg 207) inferred from benthic foraminiferal assemblages. Marine Micropaleontology. 2009; 71: 28–40.
   Web of Science ®Google Scholar
• Friedrich O., Reichelt K., Herrle J.O., Lehmann J., Pross J., Hemleben C. Formation of the Late Aptian Niveau Fallot black shales in the Vocontian Basin (SE France): evidence from foraminifera, palynomorphs, and stable isotopes. Marine Micropaleontology. 2003; 49: 65–85.
   Web of Science ®Google Scholar
• Gebhardt H., Kuhnt W., Holbourn A. Foraminiferal response to sea level change, organic flux and oxygen deficiency in the Cenomanian of the Tarfaya Basin, southern Morocco. Marine Micropaleontology. 2004; 53: 133–157.
   Web of Science ®Google Scholar
• Golebiowski R. Facial and faunistic changes from Triassic to Jurassic in the northern Calcareous Alps. Cahiers de l'Université de Lyon. 1990; 3: 175–184.
   Google Scholar
• Golonka J. Late Triassic and Early Jurassic paleogeography of the world. Palaeogeography, Palaeoclimatology, Palaeoecology. 2007; 244: 297–307.
   Web of Science ®Google Scholar
• Golonka J. Spencer A.M. Phanerozoic palaeoenvironment and palaeolithofacies maps of the Arctic region. Arctic petroleum geology. 2011; London: Geological Society. 79–129.
   Google Scholar
• Golonka J., Bocharova N.Y., Ford D., Edrich M.E., Bednarczyk J., Wildharber J. Paleogeographic reconstructions and basins development of the Arctic. Marine and Petroleum Geology. 2003; 20: 211–248.
   Web of Science ®Google Scholar
• Golonka J., Scotese C.R. Simakov K.V., Thurston D.K. Phanerozoic paleogeographic maps of Arctic margins. Proceedings of International Conference on Arctic Margins. Magadan, Russia, September 1994. 1995; Magadan: Russian Academy of Sciences, Far Eastern Branch. 1–16.
   Google Scholar
• Gómez J.J., Goy A. Warming-driven mass extinction in the Early Toarcian (Early Jurassic) of northern and central Spain. Correlation with other time-equivalent European sections. Palaeogeography, Palaeoclimatology, Palaeoecology. 2011; 306: 176–195.
   Web of Science ®Google Scholar
• Gómez J.J., Goy A., Canales M.L. Seawater temperature and carbon isotope variations in belemnites linked to mass extinction during the Toarcian (Early Jurassic) in central and northern Spain. Comparison with other European sections. Palaeogeography, Palaeoclimatology, Palaeoecology. 2008; 258: 28–58.
   Web of Science ®Google Scholar
• Hallam A. Estimates of the amount and rate of sea-level change across the Rhaetian-Hettangian and Pliensbachian-Toarcian boundaries (latest Triassic to early Jurassic). Journal of the Geological Society, London. 1997; 154: 773–779.
   Web of Science ®Google Scholar
• Hallam A. A review of the broad pattern of Jurassic sea-level changes and their possible causes in the light of current knowledge. Palaeogeography, Palaeoclimatology, Palaeoecology. 2001; 167: 23–37.
   Web of Science ®Google Scholar
• Hallock P. Why are larger foraminifera large?. Paleobiology. 1985; 11: 195–208.
   Web of Science ®Google Scholar
• Hallock P., Premoli Silva I., Boersma A. Similarities between planktonic and larger foraminiferal evolutionary trends through Paleogene evolutionary trend. Palaeogeography, Palaeoclimatology, Palaeoecology. 1991; 84: 49–64.
   Web of Science ®Google Scholar
• Haq B.U., Hardenbol J., Vail P.R. Chronology of fluctuating sea level since the Triassic. Science. 1987; 235: 1156–1167.
   PubMed Web of Science ®Google Scholar
• Hermoso M., Le Callonnec L., Minoletti F., Renard M., Hesselbo S.P. Expression of the Early Toarcian negative carbon-isotope excursion in separated carbonate microfractions (Jurassic, Paris Basin). Earth and Planetary Science Letters. 2009; 277: 194–203.
   Web of Science ®Google Scholar
• Hesselbo S.P., Jenkyns H.C., Duarte L.V., Oliveira L.C.V. Carbon isotope record of the Early Jurassic (Toarcian) Oceanic Anoxic Event from fossil wood and marine carbonate (Lusitanian Basin, Portugal). Earth and Planetary Science Letters. 2007; 253: 455–470.
   Web of Science ®Google Scholar
• Hylton M.D., Hart M.B. Benthic foraminiferal response to Pliensbachian-Toarcian (Lower Jurassic) sea-level change and oceanic anoxia in NW Europe. Georesearch Forum. 2000; 6: 455–462.
   Google Scholar
• Jenkins C.D. The ecological significance of foraminifera in the Kimmeridgian of Southern England. Grzybowski Foundation Special Publication. 2000; 7: 167–178.
   Google Scholar
• Jenkyns H.C., Clayton C.K. Lower Jurassic epicontinental carbonates and mudstones from England and Wales: chemostratigraphic signals and the early Toarcian anoxic event. Sedimentology. 1997; 44: 687–706.
   Web of Science ®Google Scholar
• Jones R.W., Charnock M.A. “Morphogroups” of agglutinating foraminifera. Their life position and feeding habits and potential applicability in (paleo)ecological studies. Revue de Paléobiologie. 1985; 4: 311–320.
   Google Scholar
• Jorissen F.J., De Stigter H.C., Widmark J.G.V. A conceptual model explaining benthic foraminiferal habitats. Marine Micropaleontology. 1995; 26: 3–15.
   Web of Science ®Google Scholar
• Kaplan M.E. Litologija morskih mezozojskih otlo(enij severa vostocnoj Sibiri. (Lithology of marine Mesozoic deposits in the northern part of Eastern Siberia.). 1976; Leningrad: Nedra Leningrad.
   Google Scholar
• Kitazato H., Matsushita S. Laboratory observations of sexual and asexual reproduction of Trochammina hadai Uchio. Transactions and Proceedings of the Palaeontological Society of Japan, New Series. 1996; 182: 454–466.
   Google Scholar
• Koho K.A., Langezaal A.M., van Lith Y.A., Duijnstee I.A.P., van der Zwaan G.J. The influence of a simulated diatom bloom on deep-sea benthic foraminifera and the activity of bacteria: a mesocosm study. Deep-Sea Research Part I. 2008; 55: 696–719.
   Google Scholar
• Korte C., Hesselbo S.P. Shallow marine carbon and oxygen isotope and elemental records indicate icehouse–greenhouse cycles during the Early Jurassic. Paleoceanography. 2011; 26: PA4219.
   Google Scholar
• Koutsoukos E.A.M., Hart M.B. Cretaceous foraminiferal morphogroup distribution patterns, paleocommunities and trophic structures—a case-study from the Serpige Basin, Brazil. Transactions of the Royal Society of Edinburgh-Earth Sciences. 1990; 81: 221–246.
   Google Scholar
• Kuerschner W.M., Bonis N.R., Krystyn L. Carbon isotope stratigraphy and palynostratigraphy of the Triassic-Jurassic transition in the Tiefengraben section—Northern Calcareous Alps (Austria). Palaeogeography, Palaeoclimatology, Palaeoecology. 2007; 244: 257–280.
   Web of Science ®Google Scholar
• Loubere P. The surface ocean productivity and bottom water oxygen signals in deep water benthic foraminiferal assemblages. Marine Micropaleontology. 1996; 28: 247–261.
   Web of Science ®Google Scholar
• MacArthur R.H., Wilson E.O. The theory of island biogeography. 1967; Princeton, NJ: Princeton University Press.
   Google Scholar
• Mailliot S., Mattioli E., Bartolini A., Baudin F., Pittet B., Guex J. Late Pliensbachian–Early Toarcian (Early Jurassic) environmental changes in an epicontinental basin of NW Europe (Causses area, central France): a micropaleontological and geochemical approach. Palaeogeography, Palaeoclimatology, Palaeoecology. 2009; 273: 346–364.
   Web of Science ®Google Scholar
• McArthur J.M., Donovan D.T., Thirvall M.F., Fouke B.W., Mattey D. Strontium isotope of the Early Toarcian (Jurassic) oceanic anoxic event, the duration of ammonite biozones and belemnite palaeotemperatures. Earth and Planetary Science Letters. 2000; 179: 269–285.
   Web of Science ®Google Scholar
• McGann M., Sloan D. Benthic foraminifers in the regional monitoring program's San Francisco estuary samples: Richmond, San Francisco Estuary Institute. In: San Francisco Estuary Regional Monitoring Program for Trace Substances. 1997 annual report. 1999; Richmond, CA: San Francisco Estuary Institute. 249–258.
   Google Scholar
• Morten S.D., Twitchett R.J. Fluctuations in the body size of marine invertebrates through the Pliensbachian–Toarcian extinction event. Palaeogeography, Palaeoclimatology, Palaeoecology. 2009; 284: 29–38.
   Web of Science ®Google Scholar
• Murray J.W., Alve E., Jones B.W. A new look at modern agglutinated benthic foraminiferal morphogroups: their value in palaeoecological interpretation. Palaeogeography, Palaeoclimatology, Palaeoecology. 2011; 309: 229–241.
   Web of Science ®Google Scholar
• Nagy J. Environmental significance of foraminiferal morphogroups in Jurassic North Sea deltas. Palaeogeography, Palaeoclimatology, Palaeoecology. 1992; 95: 111–134.
   Web of Science ®Google Scholar
• Nagy J., Berge S.H. Micropalaeontological evidence of brackish water conditions during deposition of the Knorringfjellet Formation, Late Triassic–Early Jurassic, Spitsbergen. Polar Research. 2008; 27: 413–427.
   Web of Science ®Google Scholar
• Nagy J., Hess S., Alve E. Environmental significance of foraminiferal assemblages dominated by small-sized Ammodiscus and Trochammina in Triassic and Jurassic delta-influenced deposits. Earth-Science Reviews. 2010; 99: 31–49.
   Web of Science ®Google Scholar
• Nagy J., Johansen H.O. Delta-influenced foraminiferal assemblages from the Jurassic (Toarcian–Bajocian) of the northern North Sea. Micropaleontology. 1991; 37: 1–7.
   Web of Science ®Google Scholar
• Nagy J., Reolid M., Rodríguez-Tovar F.J. Foraminiferal morphogroups in dysoxic shelf deposits from the Jurassic of Spitsbergen. Polar Research. 2009; 28: 214–221.
   Web of Science ®Google Scholar
• Nikitenko B.L. The Early Jurassic to Aalenian paleobiogeography of the Arctic Realm: implications of microbenthos (foraminifers and ostracodes): stratigraphy. Geological Correlation. 2008; 16: 59–80.
   Web of Science ®Google Scholar
• Nikitenko B.L. Jurassic stratigraphy, palaeobiogeography and biofacies of Siberia on microfauna (foraminifers and ostracodes). 2009; Novosibirsk: Parallel.
   Google Scholar
• Nikitenko B.L., Mickey M.B. Foraminifera and ostracodes across the Pliensbachian–Toarcian boundary in the Arctic Realm (stratigraphy, paleobiogeography and biofaces). Journal Geological Society Special Publication. 2004; 230: 137–174.
   Google Scholar
• Nikitenko B.L., Reolid M., Glinskikh L. Ecostratigraphy of benthic foraminifera for interpreting Arctic record of Early Toarcian biotic crisis (northern Siberia, Russia). Palaeogeography, Palaeoclimatology, Palaeoecology. 2013; 376: 200–212.
   Web of Science ®Google Scholar
• Nocchi M., Bartolini A. Investigations on Late Domerian–Early Toarcian Lagenina and Glomospirella assemblages in the Umbria Marche Basin (central Italy). Geobios M.S. 1994; 17: 689–699.
   Google Scholar
• Nyong E.E., Ramanathan R. A record of oxygen-deficient paleoenvironments in the Cretaceous of the Calabar Flank, SE Nigeria. Journal of African Earth Sciences. 1985; 3: 455–460.
   Web of Science ®Google Scholar
• Price G.D. The evidence and implication of polar ice during the Mesozoic. Earth-Science Reviews. 1999; 48: 183–210.
   Web of Science ®Google Scholar
• Reolid M., Chakiri S., Bejjaji Z. Adaptative strategies of the Toarcian benthic foraminiferal assemblages from the Middle Atlas (Morocco): palaeoecological implications. Journal of African Earth Sciences. 2013; 84: 1–12.
   Web of Science ®Google Scholar
• Reolid M., Nagy J. Jurassic transgressive–regressive cycles in carbonate and siliciclastic shelf facies: different response of foraminiferal assemblage trends to sea-level changes. Grzybowski Foundation Special Publication. 2008; 13: 199–213.
   Google Scholar
• Reolid M., Nagy J., Rodríguez-Tovar F.J. Ecostratigraphic trends of Jurassic agglutinated foraminiferal assemblages as a response to sea-level changes in shelf deposits of Svalbard (Norway). Palaeogeography, Palaeoclimatology, Palaeoecology. 2010; 293: 184–196.
   Web of Science ®Google Scholar
• Reolid M., Nagy J., Rodríguez-Tovar F.J., Olóriz F. Foraminiferal assemblages as palaeoenvironmental bioindicators in Late Jurassic epicontinental platforms: relation with trophic conditions. Acta Palaeontologica Polonica. 2008; 53: 706–722.
   Web of Science ®Google Scholar
• Reolid M., Rodríguez-Tovar F.J., Marok A., Sebane A. The Toarcian Oceanic Anoxic Event in the Western Saharan Atlas, Algeria (North African Paleomargin): role of anoxia and productivity. Geological Society of America Bulletin. 2012; 124: 1646–1664.
   Web of Science ®Google Scholar
• Reolid M., Rodríguez-Tovar F.J., Nagy J. Ecological replacement of Valanginian agglutinated foraminifera during a maximum flooding event in the Boreal realm (Spitsbergen). Cretaceous Research. 2012; 33: 196–204.
   Web of Science ®Google Scholar
• Reolid M., Rodríguez-Tovar F.J., Nagy J., Olóriz F. Benthic foraminiferal morphogroups of mid to outer shelf environments of the Late Jurassic (Prebetic Zone, southern Spain): characterisation of biofacies and environmental significance. Palaeogeography, Palaeoclimatology, Palaeoecology. 2008; 261: 280–299.
   Web of Science ®Google Scholar
• Reolid M., Sebane A., Rodríguez-Tovar F.J., Marok A. Foraminiferal morphogroups as a tool to approach the Toarcian Anoxic Event in the Western Saharan Atlas (Algeria). Palaeogeography, Palaeoclimatology, Palaeoecology. 2012; 323–325: 87–99.
   Web of Science ®Google Scholar
• Rey J., Bonnet L., Cubaynes R., Qajoun A., Ruget C. Sequence stratigraphy and biological signals: statistical studies of benthic foraminifera from Liassic series. Palaeogeography, Palaeoclimatology, Palaeoecology. 1994; 111: 149–171.
   Web of Science ®Google Scholar
• Röhl H.J., Schmid-Röhl A., Oschmann W., Frimmel A., Schwark L. The Posidonian Shale (Lower Toarcian) of SW-Germany: an oxygen-depleted ecosystem controlled by sea level and paleoclimate. Palaeogeography, Palaeoclimatology, Palaeoecology. 2001; 165: 27–52.
   Web of Science ®Google Scholar
• Rosales I., Quesada S., Robles S. Paleotemperature variations of Early Jurassic seawater recorded in geochemical trends of belemnites from the Basque–Cantabrian basin, northern Spain. Palaeogeography, Palaeoclimatology, Palaeoecology. 2004; 203: 253–275.
   Web of Science ®Google Scholar
• Scotese C.R. Paleogeographic reconstructions of the circum-Arctic region since the Late Jurassic. Search and Discovery. 2011. article no. 30193.
   Google Scholar
• Setoyama E., Radmacher W., Kaminski M.A., Tyszka J. Foraminiferal and palynological biostratigraphy and biofacies from a Santonian–Campanian submarine dan system in the Vøring Basin (offshore Norway). Marine and Petroleum Geology. 2013; 43: 396–408.
   Web of Science ®Google Scholar
• Sjoerdsma P.G., Van der Zwaan G.J. Simulating the effect of changing organic flux and oxygen content on the distribution of benthic foraminifera. Marine Micropaleontology. 1992; 19: 163–180.
   Web of Science ®Google Scholar
• Song H., Tong J., Chen Z.Q. Evolutionary dynamics of the Permian–Triassic foraminifer size: evidence for Lilliput effect in the end-Permian mass extinction and its aftermath. Palaeogeography, Palaeoclimatology, Palaeoecology. 2011; 308: 98–110.
   Web of Science ®Google Scholar
• Soua M., Zaghbin-Turki D., Ben Jemia H., Smaoui J., Boukadi A. Geochemical record of the Cenomanian–Turonian Anoxic Event in Tunisia: is it correlative and isochronous to the biotic signal?. Acta Geologica Sinica-English Edition. 2011; 85: 1310–1335.
   Web of Science ®Google Scholar
• Suan G., Mattioli E., Pittet B., Lécuyer C., Suchéras-Marx B., Duarte L.V., Philippe M., Reggiani M.L., Martineau F. Secular environmental precursors of Early Toarcian (Jurassic) extreme climate changes. Earth and Planetary Science Letters. 2010; 290: 448–458.
   Web of Science ®Google Scholar
• Suan G., Nikitenko B.L., Rogov M.A., Baudin F., Spangenberg J.E., Knyazev V.G., Glinskikh L.A., Goryacheva A.A., Adatte T., Riding J.B., Föllmi K.B., Pittet B., Mattioli E., Lécuyer C. Polar record of Early Jurassic massive carbon injection. Earth and Planetary Science Letters. 2011; 312: 102–113.
   Web of Science ®Google Scholar
• Svensen H., Planke S., Chevallier L., Malthe-Sorenssen A., Corfu F., Jamtveit B. Hydrothermal venting of greenhouse gases triggering Early Jurassic global warming. Earth and Planetary Science Letters. 2007; 290: 448–458.
   Google Scholar
• Thurman H.V., Trujillo A.P. Introductory oceanography. 2004; Upper Saddle River, NJ: Prentice Hall.
   Google Scholar
• Torsvik T.H., Van der Voo R., Preeden U., MacNiocaill C., Steinberger B., Doubrovine P.V., van Hinsbergen D.J.J., Domeier M., Gaina C., Tohver E., Meert J.G., McCausland P.J.A., Cocks L.R.M. Phanerozoic polar wander, palaeogeography and dynamics. Earth-Science Reviews. 2012; 114: 325–368.
   Web of Science ®Google Scholar
• Tsujimoto A., Nomura R., Yasuhara M., Yamazaki H., Yoshikawa S. Impact of eutrophication on shallow marine benthic foraminifers over the last 150 years in Osaka Bay, Japan. Marine Micropaleontology. 2006; 60: 258–268.
   Web of Science ®Google Scholar
• Twitchett R.J. The Lilliput effect in the aftermath of the end-Permian extinction event. Palaeogeography, Palaeoclimatology, Palaeoecology. 2007; 252: 132–144.
   Web of Science ®Google Scholar
• Tyszka J. Response of Middle Jurassic benthic foraminiferal morphogroups to dysoxic/anoxic conditions in the Pieniny Klippen Basin, Polish Carpathians. Palaeogeography, Palaeoclimatology, Palaeoecology. 1994; 110: 55–81.
   Web of Science ®Google Scholar
• Tyszka J. Foraminiferal response to seasonality modulated by orbital cycles in the Cretaceous mid-latitudes: the Albian record from the Lower Saxony Basin. Palaeogeography, Palaeoclimatology, Palaeoecology. 2009; 276: 148–159.
   Web of Science ®Google Scholar
• Tyszka J. Seasonal opportunists: in fossilio experiment on Albian foraminifera. Taxonomic challenges and innovations. In: The Micropalaeontological Society's Foraminifera and Nannofossil Groups’ Joint Spring Meeting. 28 June, The Natural History Museum, London. 2010; London: Micropalaeontological Society. 9–10.
   Google Scholar
• Valentine J.W. Evolutionary ecology of the marine biosphere. 1973; Englewood Cliffs, NJ: Prentice Hall.
   Google Scholar
• Van de Schootbrugge B., McArthur J.M., Bailey T.R., Rosenthal Y., Wright J.D., Miller K.G. Toarcian oceanic anoxic event: an assessment of global causes using belemnite C isotope records. Paleoecanography. 2005; 20 PA3008.
   Google Scholar
• Van der Zwaan G.J., Duijnstee I.A.P., Den Dulk M., Ernst S.R., Jannink N.T., Kouwenhoven T.J. Benthic foraminifers: proxies or problem? A review of paleoecological concepts. Earth-Science Reviews. 1999; 46: 213–236.
   Web of Science ®Google Scholar
• Wignall P.B., Newton R.J., Little C.T.S. The timing of paleoenvironmental change and cause-and-effect relationships during the Early Jurassic mass extinction in Europe. American Journal of Sciences. 2005; 305: 1014–1032.
   Web of Science ®Google Scholar