Other| June 01, 2000 Environmental Distribution of Spinose Brachiopods from the Devonian of New York: Test of the Soft-substrate Hypothesis LINDSEY R. LEIGHTON LINDSEY R. LEIGHTON 1Museum of Paleontology, Department of Geological Sciences, University of Michigan, Ann Arbor, MI 48109 *Current address: Department of Geological Sciences, Indiana University, Bloomington, IN 47405 Search for other works by this author on: GSW Google Scholar Author and Article Information LINDSEY R. LEIGHTON *Current address: Department of Geological Sciences, Indiana University, Bloomington, IN 47405 1Museum of Paleontology, Department of Geological Sciences, University of Michigan, Ann Arbor, MI 48109 Publisher: SEPM Society for Sedimentary Geology Accepted: 11 Feb 2000 First Online: 03 Mar 2017 Online ISSN: 1938-5323 Print ISSN: 0883-1351 Society for Sedimentary Geology PALAIOS (2000) 15 (3): 184–193. https://doi.org/10.1669/0883-1351(2000)015<0184:EDOSBF>2.0.CO;2 Article history Accepted: 11 Feb 2000 First Online: 03 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation LINDSEY R. LEIGHTON; Environmental Distribution of Spinose Brachiopods from the Devonian of New York: Test of the Soft-substrate Hypothesis. PALAIOS 2000;; 15 (3): 184–193. doi: https://doi.org/10.1669/0883-1351(2000)015<0184:EDOSBF>2.0.CO;2 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyPALAIOS Search Advanced Search Abstract Brachiopod spines have been interpreted as a mechanism that enables the organism to rest on soft substrates by distributing shell mass over a greater area. This hypothesis is based on an arrangement in which spines are long, strongly curved, few in number, and generally restricted to the pedicle valve. However, other spine geometries also are prevalent, and the assumption that all arrangements functioned similarly may be unwarranted. Spinatrypa and Praewaagenoconcha, an atrypide and a productide, respectively, are genera of spinose brachiopods from the Upper Devonian Java Formation of New York. Although these genera belong to different subclasses, they have a similar spine geometry consisting of hundreds of thin, short, sub-perpendicular (to shell surface) spines, arranged concentrically on both valves.Population densities of articulate brachiopods were obtained from six localities of the Java Formation along an offshore-onshore gradient. Individuals were counted relative to surface area of the bedding planes. There are moderate, but highly significant, correlations between grain size and abundance of each spinose taxon, and the greatest mean densities of both Praewaagenoconcha and Spinatrypa occur in coarse sandstones. Although both genera have broad environmental ranges, peak mean abundances of Praewaagenoconcha and Spinatrypa are in platform margin and outer platform facies. All of these distributions are statistically distinguishable (χ 2 test, p < 0.0001) from the distribution of non-spinose taxa within the Java Formation.These results are inconsistent with the hypothesis that all spine geometries served as soft substrate supports. Alternative functional hypotheses for this spine geometry include (1) anchorage in high energy habitats, and/or (2) protection from predation. You do not have access to this content, please speak to your institutional administrator if you feel you should have access.
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