Beiträge in Fachzeitschriften

• Abdelhady A., Seuß B., El-Dawy M., Obaidalla N., Hussien S., Mahfouzd K.:
  The Unitary Association method in biochronology and its potential stratigraphic power between benthic and planktic organisms: A case study on foraminifers from Paleocene–Eocene strata of southern Egypt
  In: Geobios 51 (2018), S. 259-268
  ISSN: 0016-6995
  DOI: 10.1016/j.geobios.2018.06.005
• Niko S., Seuß B., Mapes RH.:
  Desmoinesian (Middle Pennsylvanian) orthocerid cephalopods from the Buckhorn Asphalt Lagerstätte in Oklahoma, Midcontinent North America
  In: Paleontological Research 22 (2018), S. 20-36
  ISSN: 1342-8144
  DOI: 10.2517/2017PR008
• Ivanov A., Seuß B., Nützel A.:
  The fish assemblage from the Pennsylvanian Buckhorn Asphalt Quarry Lagerstätte (Oklahoma, USA)
  In: Palaeontologische Zeitschrift 91 (2017), S. 565–576
  ISSN: 0031-0220
  DOI: 10.1007/s12542-017-0361-9
• Seuß B., Wisshak M., Mapes RH., Hembree DI., Landman N., Lignier V.:
  Microbial bioerosion of erratic sub-fossil Nautilus shells in a karstic cenote (Lifou, Loyalty Islands, New Caledonia)
  In: Ichnos-An International Journal For Plant and Animal Traces 23 (2016), S. 108-115
  ISSN: 1042-0940
  DOI: 10.1080/10420940.2015.1030074
• Ernst A., Seuß B., Taylor P., Nützel A.:
  Bryozoan fauna of the Boggy Formation (Deese Group, Pennsylvanian) of the Buckhorn Asphalt Quarry, Oklahoma, USA
  In: Palaeobiodiversity and Palaeoenvironments 96 (2016), S. 517-540
  ISSN: 1867-1594
  DOI: 10.1007/s12549-016-0231-6
• Seuß B., Hembree DI., Wisshak M., Mapes RH., Landman N.:
  Taphonomy of backshore versus deep-marine collected nautilus macromphalus conchs (New Caledonia)
  In: Palaios 30 (2015), S. 503-513
  ISSN: 0883-1351
  DOI: 10.2110/palo.2014.057
  URL: https://www.scopus.com/inward/record.uri?partnerID=HzOxMe3b&scp=84939493054&origin=inward
• Seuß B., Wisshak M., Mapes RH., Landman N.:
  Syn-vivo bioerosion of Nautilus by endo- and epilithic foraminiferans (New Caledonia and Vanuatu)
  In: PLoS ONE 10 (2015), S. e0125558
  ISSN: 1932-6203
  DOI: 10.1371/journal.pone.0125558
• Seuß B., Senowbari-Daryan B., Nützel A., Dittrich S., Neubauer J., Neubauer J.:
  A chaetetid sponge assemblage from the Desmoinesian (Upper Moscovian) Buckhorn Asphalt Quarry lagerstätte in Oklahoma, USA
  In: Rivista Italiana Di Paleontologia E Stratigrafia 120 (2014), S. 3-26
  ISSN: 0035-6883
• Seuß B., Nützel A., Scholz H., Frýda J.:
  The Paleozoic evolution of the gastropod larval shell: larval armor and tight coiling as results of predation-driven heterochronic character displacement
  In: Evolution & Development 14 (2012), S. 212-222
  ISSN: 1520-541X
  DOI: 10.1111/j.1525-142X.2012.00536.x
• Seuß B., Titschack J., Seifert S., Neubauer J., Nützel A.:
  Oxygen and stable carbon isotopes from a nautiloid from the middle Pennsylvanian (Late Carboniferous) impregnation Lagerstätte "Buckhorn Asphalt Quarry" - Primary paleo-environmental signals versus diagenesis
  In: Palaeogeography, Palaeoclimatology, Palaeoecology 319/320 (2012), S. 1-15
  ISSN: 0031-0182
• Seuß B., Mapes RH., Klug C., Nützel A.:
  Exceptional cameral deposits in a sublethally injured Carboniferous orthoconic nautiloid from the Buckhorn Asphalt Lagerstätte in Oklahoma, USA
  In: Acta Palaeontologica Polonica 57 (2012), S. 375-390
  ISSN: 0567-7920
  DOI: 10.4202/app.2011.0008
• Arp G., Schulbert C., Seuß B., Aiglstorfer M., Havlik P., Krause T., Waltschew A., Strobl C.:
  Neuaufschluss des berühmten Schwarzjura-Profils am historischen Ludwig-Donau-Main-Kanal bei Dörlbach/Mittelfranken
  In: GMIT - Geowissenschaftliche Mitteilungen 45 (2011), S. 21-23
  ISSN: 1616-3931
• Seuß B., Nützel A., Mapes RH., Yancey TE.:
  Facies and fauna of the Pennsylvanian Buckhorn Asphalt Quarry deposit: a review and new data on an important Palaeozoic fossil Lagerstätte with aragonite preservation
  In: Facies 55 (2009), S. 609-645
  ISSN: 0172-9179
  DOI: 10.1007/s10347-009-0181-9
• Seuß B., Höfling R., Nützel A.:
  Triassic-Jurassic carbonates from the Hochfelln Mountain (Northern Calcareous Alps) - Its facies, silicified fauna and implications for the end-Triassic biotic crisis
  In: Facies 51 (2005), S. 405-418
  ISSN: 0172-9179
  DOI: 10.1007/s10347-005-0048-7

Beiträge in Sammelbänden

• Seuß B.:
  Pennsylvanian of Southern Oklahoma (Upper Carboniferous, USA) - The Buckhorn Asphalt Quarry
  In: IGCP 596 Climate Change and Biodiversity Patterns in the Mid-Palaeozoic, 2016, S. 42
  DOI: 10.1016/j.palaeo.2011.12.008
• Seuß B., Mapes RH.:
  Pennsylvanian in North Central Texas, USA - The Finis Shale
  In: IGCP 596 Climate Change and Biodiversity Patterns in the Mid-Palaeozoic, 2016, S. 44
• Seuß B., Nützel A.:
  Gastropoda
  In: IGCP 596 Climate Change and Biodiversity Patterns in the Mid-Palaeozoic, 2016, S. 44
• Seuß B., Mapes RH.:
  Cephalopoda
  In: IGCP 596 Climate Change and Biodiversity Patterns in the Mid-Palaeozoic, 2016, S. 34
• Wisshak M., Seuß B., Nützel A.:
  Evolutionary implications of an exceptionally preserved Carboniferous microboring assemblage in the Buckhorn Asphalt Lagerstätte (Oklahoma, USA)
  In: Current Developments in Bioerosion, Berlin, Heidelberg: Springer, 2008, S. 21-54
  ISBN: 9783540775973
  DOI: 10.1007/978-3-540-77598-0-2

• Paläobiodiversität und Faunenstruktur in Lagerstätten während der permo-karbonen Vereisung und die Reaktion des marinen wirbellosen Benthos auf globale Abkühlung
  (Drittmittelfinanzierte Einzelförderung)
  Laufzeit: 01.07.2014 - 01.07.2017
  Mittelgeber: DFG-Einzelförderung / Sachbeihilfe (EIN-SBH)
  Abstract

  Paleo-biodiversity studies have become of increasing interest and numerous manuscripts have been published dealing with global diversity trends throughout the Phanerozoic. However, data used in these studies mostly derive from databases that may contain various biases and therefore distort statistical analysis. Moreover, Fossil Lagerstätten are commonly excluded although the quality of preservation and information is much better than in other deposits - fossil assemblages from Lagerstätten reflect the composition of former living communities to a much higher degree.The Phanerozoic is marked by two long-term cooling events. One of these is the Late Paleozoic Ice Age (LPIA) with its major onset in the middle to late Mississippian (Lower Carboniferous) and ending in the mid-Sakmarian (Permian). This project focuses on the paleo-biodiversity during the Upper Carboniferous (Pennsylvanian), i.e. during a large part of the LPIA. Instead of purely using information from databases three fossil Lagerstätten (here Lagerstätten is used in terms of exceptionally preserved fauna; e.g. original shell material, color patterns, delicate ornamentation, minute larval shells) are sampled. These localities were influenced by the glacio-eustatic regime during the LPIA and are, from the American Midcontinent, the Finis Shale (Virgilian) and the Buckhorn Asphalt Quarry (Desmoinesian) and, from the Appalachian Basin, the Kendrick Shale (Morrowan).One objective of this project is to study true biodiversities and ecological structures within deposits of exceptionally preserved fossils based on the fact that such deposits depict a more complete image of the original fossil assemblage than other localities. Stanley & Powell (2003) found that during the Pennsylvanian the rates of origination and extinction were depressed and that the global biodiversity remained relatively stable, whereas Alroy et al. (2008) found a general decrease in this period. Therefore, as the second objective, it will be tested if these previous results are visible in Lagerstätten from the Pennsylvanian as well: Do we also see depressed origination and extinction rates or decreasing biodiversity or are the results presented by Stanley & Powell (2003) and Alroy et al. (2008) caused by biases in their data, as for example by faunas of less quality of preservation? Furthermore, diversity dynamics will be studied by analyzing the Carboniferous-Permian faunal turnover. Which taxa control the diversities? The local marine paleo-temperatures within each profile will be investigated. Isotope-analyses will be carried out for the Finis Shale, the Buckhorn Asphalt Quarry, and the Kendrick Shale. Temperature and diversity will be cross correlated to shed light on the relation of temperature and biodiversity during the LPIA to answer the question 'How does the living environment react to global cooling?'.
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