11
views
0
recommends
+1 Recommend
0 collections
    0
    shares
      • Record: found
      • Abstract: found
      • Article: found
      Is Open Access

      Chamber volume development, metabolic rates, and selective extinction in cephalopods

      research-article

      Read this article at

      Bookmark
          There is no author summary for this article yet. Authors can add summaries to their articles on ScienceOpen to make them more accessible to a non-specialist audience.

          Abstract

          Reconstructing the physiology of extinct organisms is key to understanding mechanisms of selective extinction during biotic crises. Soft tissues of extinct organisms are rarely preserved and, therefore, a proxy for physiological aspects is needed. Here, we examine whether cephalopod conchs yield information about their physiology by assessing how the formation of chambers respond to external stimuli such as environmental changes. We measured chamber volume through ontogeny to detect differences in the pattern of chamber volume development in nautilids, coleoids, and ammonoids. Results reveal that the differences between ontogenetic trajectories of these cephalopods involve the presence or absence of abrupt decreases of chamber volume. Accepting the link between metabolic rate and growth, we assume that this difference is rooted in metabolic rates that differ between cephalopod clades. High metabolic rates combined with small hatching size in ammonoids as opposed to lower metabolic rates and much larger hatchlings in most nautilids may explain the selective extinction of ammonoids as a consequence of low food availability at the end of the Cretaceous.

          Related collections

          Most cited references52

          • Record: found
          • Abstract: found
          • Article: not found

          Cephalopod origin and evolution: A congruent picture emerging from fossils, development and molecules: Extant cephalopods are younger than previously realised and were under major selection to become agile, shell-less predators.

          Cephalopods are extraordinary molluscs equipped with vertebrate-like intelligence and a unique buoyancy system for locomotion. A growing body of evidence from the fossil record, embryology and Bayesian molecular divergence estimations provides a comprehensive picture of their origins and evolution. Cephalopods evolved during the Cambrian (∼530 Ma) from a monoplacophoran-like mollusc in which the conical, external shell was modified into a chambered buoyancy apparatus. During the mid-Palaeozoic (∼416 Ma) cephalopods diverged into nautiloids and the presently dominant coleoids. Coleoids (i.e. squids, cuttlefish and octopods) internalised their shells and, in the late Palaeozoic (∼276 Ma), diverged into Vampyropoda and the Decabrachia. This shell internalisation appears to be a unique evolutionary event. In contrast, the loss of a mineralised shell has occurred several times in distinct coleoid lineages. The general tendency of shell reduction reflects a trend towards active modes of life and much more complex behaviour. Copyright © 2011 WILEY Periodicals, Inc.
            Bookmark
            • Record: found
            • Abstract: found
            • Article: not found

            Good genes and good luck: ammonoid diversity and the end-Permian mass extinction.

            The end-Permian mass extinction removed more than 80% of marine genera. Ammonoid cephalopods were among the organisms most affected by this crisis. The analysis of a global diversity data set of ammonoid genera covering about 106 million years centered on the Permian-Triassic boundary (PTB) shows that Triassic ammonoids actually reached levels of diversity higher than in the Permian less than 2 million years after the PTB. The data favor a hierarchical rather than logistic model of diversification coupled with a niche incumbency hypothesis. This explosive and nondelayed diversification contrasts with the slow and delayed character of the Triassic biotic recovery as currently illustrated for other, mainly benthic groups such as bivalves and gastropods.
              Bookmark
              • Record: found
              • Abstract: found
              • Article: found

              On impact and volcanism across the Cretaceous-Paleogene boundary

              Around the time of the end-Cretaceous mass extinction that wiped out dinosaurs, there was both a bolide impact and a large amount of volcanism. Hull et al. ran several temperature simulations based on different volcanic outgassing scenarios and compared them with temperature records across the extinction event. The best model fits to the data required most outgassing to occur before the impact. When combined with other lines of evidence, these models support an impact-driven extinction. However, volcanic gases may have played a role in shaping the rise of different species after the extinction event. Science , this issue p. [Related article:] 266 The primary cause of the end-Cretaceous mass extinction was an impact, with volcanism playing a role in the aftermath. The cause of the end-Cretaceous mass extinction is vigorously debated, owing to the occurrence of a very large bolide impact and flood basalt volcanism near the boundary. Disentangling their relative importance is complicated by uncertainty regarding kill mechanisms and the relative timing of volcanogenic outgassing, impact, and extinction. We used carbon cycle modeling and paleotemperature records to constrain the timing of volcanogenic outgassing. We found support for major outgassing beginning and ending distinctly before the impact, with only the impact coinciding with mass extinction and biologically amplified carbon cycle change. Our models show that these extinction-related carbon cycle changes would have allowed the ocean to absorb massive amounts of carbon dioxide, thus limiting the global warming otherwise expected from postextinction volcanism.
                Bookmark

                Author and article information

                Contributors
                atajika@amnh.org
                Journal
                Sci Rep
                Sci Rep
                Scientific Reports
                Nature Publishing Group UK (London )
                2045-2322
                19 February 2020
                19 February 2020
                2020
                : 10
                : 2950
                Affiliations
                [1 ]ISNI 0000 0001 2152 1081, GRID grid.241963.b, Division of Paleontology (Invertebrates), , American Museum of Natural History, ; Central Part West 79th Street, New York, NY 10024 USA
                [2 ]ISNI 0000 0004 0490 981X, GRID grid.5570.7, Institut für Geologie, Mineralogie und Geophysik, , Ruhr-Universität Bochum, ; Bochum, 44801 Germany
                [3 ]ISNI 0000 0001 2111 7257, GRID grid.4488.0, BCUBE – Center for Molecular Bioengineering, , Technische Universität Dresden, ; Dresden, 01307 Germany
                [4 ]ISNI 0000 0004 0372 2033, GRID grid.258799.8, Laboratory of Physical Anthropology, Graduate School of Science, , Kyoto University, ; Kitashirakawa Oiwake-cho, Sakyo-ku, 606-8502 Kyoto Japan
                [5 ]ISNI 0000 0001 2190 4373, GRID grid.7700.0, Institut für Geowissenschaften, , Ruprecht-Karls-Universität Heidelberg, ; Im Neuenheimer Feld 234/Raum 217, D-69120 Heidelberg, Germany
                [6 ]ISNI 0000 0004 1937 0650, GRID grid.7400.3, Paläontologisches Institut und Museum, , Universität Zürich, ; Karl-Schmid-Strasse 4, Zürich, 8006 Switzerland
                Author information
                http://orcid.org/0000-0002-4099-7453
                Article
                59748
                10.1038/s41598-020-59748-z
                7031508
                32076034
                80958eb3-791e-421a-894a-ffa38e6d495e
                © The Author(s) 2020

                Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons license and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/.

                History
                : 31 October 2019
                : 3 February 2020
                Funding
                Funded by: FundRef https://doi.org/10.13039/501100001711, Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung (Swiss National Science Foundation);
                Award ID: 200020_169847
                Award ID: 200020_169847
                Award ID: 200021_149119
                Award Recipient :
                Funded by: Japan Society for the Promotion of Science
                Categories
                Article
                Custom metadata
                © The Author(s) 2020

                Uncategorized
                palaeontology,palaeoecology
                Uncategorized
                palaeontology, palaeoecology

                Comments

                Comment on this article