Comparative Ichnology of Shelf-Sea and Deep-Sea Chalk
All chalk is a fine-grained pelagic sediment derived from calcareous microplankton and nannoplankton. However, "shelf-sea" chalk (deposited in hundreds of meters of water) differs from "deep-sea" chalk (deposited in thousands of meters of water) in several paleontologic and sedim...
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Veröffentlicht in: | Journal of paleontology 1984-03, Vol.58 (2), p.322-332 |
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description | All chalk is a fine-grained pelagic sediment derived from calcareous microplankton and nannoplankton. However, "shelf-sea" chalk (deposited in hundreds of meters of water) differs from "deep-sea" chalk (deposited in thousands of meters of water) in several paleontologic and sedimentologic respects. Unlike deep-sea chalk, shelf-sea chalk characteristically contains abundant megafossils, flints, omission surfaces, hardgrounds, borings and early diagenetic mineralization (pyrite, glauconite and phosphate) of trace fossils and clasts. Trace fossil associations are dominated by Thalassinoides and other crustacean burrows in most shelf-sea chalk sections; trace fossil associations in deep-sea chalk cores are dominated by Chrondrites, Planolites and Zoophycos. |
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G.</creatorcontrib><description>All chalk is a fine-grained pelagic sediment derived from calcareous microplankton and nannoplankton. However, "shelf-sea" chalk (deposited in hundreds of meters of water) differs from "deep-sea" chalk (deposited in thousands of meters of water) in several paleontologic and sedimentologic respects. Unlike deep-sea chalk, shelf-sea chalk characteristically contains abundant megafossils, flints, omission surfaces, hardgrounds, borings and early diagenetic mineralization (pyrite, glauconite and phosphate) of trace fossils and clasts. Trace fossil associations are dominated by Thalassinoides and other crustacean burrows in most shelf-sea chalk sections; trace fossil associations in deep-sea chalk cores are dominated by Chrondrites, Planolites and Zoophycos.</description><identifier>ISSN: 0022-3360</identifier><identifier>EISSN: 1937-2337</identifier><language>eng</language><publisher>Society of Economic Paleontologists and Mineralogists and the Paleontological Society</publisher><subject>Chalk ; Chondrites ; Crustaceans ; Drilling ; Flint ; Geology ; Limestones ; Seas ; Sediments ; Trace fossils</subject><ispartof>Journal of paleontology, 1984-03, Vol.58 (2), p.322-332</ispartof><rights>Copyright 1984 The Society of Economic Paleontologists and Mineralogists and The Paleontological Society</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.jstor.org/stable/pdf/1304787$$EPDF$$P50$$Gjstor$$H</linktopdf><linktohtml>$$Uhttps://www.jstor.org/stable/1304787$$EHTML$$P50$$Gjstor$$H</linktohtml><link.rule.ids>314,776,780,799,57992,58225</link.rule.ids></links><search><creatorcontrib>Ekdale, A. A.</creatorcontrib><creatorcontrib>Bromley, R. G.</creatorcontrib><title>Comparative Ichnology of Shelf-Sea and Deep-Sea Chalk</title><title>Journal of paleontology</title><description>All chalk is a fine-grained pelagic sediment derived from calcareous microplankton and nannoplankton. However, "shelf-sea" chalk (deposited in hundreds of meters of water) differs from "deep-sea" chalk (deposited in thousands of meters of water) in several paleontologic and sedimentologic respects. Unlike deep-sea chalk, shelf-sea chalk characteristically contains abundant megafossils, flints, omission surfaces, hardgrounds, borings and early diagenetic mineralization (pyrite, glauconite and phosphate) of trace fossils and clasts. Trace fossil associations are dominated by Thalassinoides and other crustacean burrows in most shelf-sea chalk sections; trace fossil associations in deep-sea chalk cores are dominated by Chrondrites, Planolites and Zoophycos.</description><subject>Chalk</subject><subject>Chondrites</subject><subject>Crustaceans</subject><subject>Drilling</subject><subject>Flint</subject><subject>Geology</subject><subject>Limestones</subject><subject>Seas</subject><subject>Sediments</subject><subject>Trace fossils</subject><issn>0022-3360</issn><issn>1937-2337</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1984</creationdate><recordtype>article</recordtype><sourceid/><recordid>eNotjMtKAzEUQINYcGz9Axf5gUCSm0luljK-CoUuqutyM0mc1mkzzAxC_15ROYvD2ZwrVikPTmgAd80qKbUWAFbesNtpOkqptFWqYnVTTgONNB--El-33bn05ePCS-a7LvVZ7BJxOkf-mNLwG01H_eeKLTL1U7r795K9Pz-9Na9is31ZNw8bQcq7WUQvg7ExkLdt8GQDWjTB_SDrEJKJmAGy87WFnDC2XrfksA4YDSIFD0t2__c9TnMZ98N4ONF42SuQxqGDbxNMP10</recordid><startdate>19840301</startdate><enddate>19840301</enddate><creator>Ekdale, A. A.</creator><creator>Bromley, R. G.</creator><general>Society of Economic Paleontologists and Mineralogists and the Paleontological Society</general><scope/></search><sort><creationdate>19840301</creationdate><title>Comparative Ichnology of Shelf-Sea and Deep-Sea Chalk</title><author>Ekdale, A. A. ; Bromley, R. G.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a197t-d90b46dba96cb9a6b8684b7b7b05bbe4d8f33f79563fe8dc92ca785b8d488ab93</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>1984</creationdate><topic>Chalk</topic><topic>Chondrites</topic><topic>Crustaceans</topic><topic>Drilling</topic><topic>Flint</topic><topic>Geology</topic><topic>Limestones</topic><topic>Seas</topic><topic>Sediments</topic><topic>Trace fossils</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Ekdale, A. A.</creatorcontrib><creatorcontrib>Bromley, R. G.</creatorcontrib><jtitle>Journal of paleontology</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Ekdale, A. A.</au><au>Bromley, R. G.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Comparative Ichnology of Shelf-Sea and Deep-Sea Chalk</atitle><jtitle>Journal of paleontology</jtitle><date>1984-03-01</date><risdate>1984</risdate><volume>58</volume><issue>2</issue><spage>322</spage><epage>332</epage><pages>322-332</pages><issn>0022-3360</issn><eissn>1937-2337</eissn><abstract>All chalk is a fine-grained pelagic sediment derived from calcareous microplankton and nannoplankton. However, "shelf-sea" chalk (deposited in hundreds of meters of water) differs from "deep-sea" chalk (deposited in thousands of meters of water) in several paleontologic and sedimentologic respects. Unlike deep-sea chalk, shelf-sea chalk characteristically contains abundant megafossils, flints, omission surfaces, hardgrounds, borings and early diagenetic mineralization (pyrite, glauconite and phosphate) of trace fossils and clasts. Trace fossil associations are dominated by Thalassinoides and other crustacean burrows in most shelf-sea chalk sections; trace fossil associations in deep-sea chalk cores are dominated by Chrondrites, Planolites and Zoophycos.</abstract><pub>Society of Economic Paleontologists and Mineralogists and the Paleontological Society</pub><tpages>11</tpages></addata></record> |
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source | Jstor Complete Legacy |
subjects | Chalk Chondrites Crustaceans Drilling Flint Geology Limestones Seas Sediments Trace fossils |
title | Comparative Ichnology of Shelf-Sea and Deep-Sea Chalk |
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