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Stable isotopic indication for the cyst formation depth of Campanian/Maastrichtian calcareous dinoflagellates
δ18O and δ13C values for the calcareous dinoflagellate species Orthopithonella? globosa ($F\ddot utterer$1984) Lentin and Williams 1985 and Pirumella krasheninnikovii (Bolli 1974) Lentin and Williams 1993 from latest Campanian and earliest Maastrichtian of ODP Hole 690C (Weddell Sea, Antarctic Ocean...
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Published in: | Micropaleontology 2003-12, Vol.49 (4), p.375-380 |
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description | δ18O and δ13C values for the calcareous dinoflagellate species Orthopithonella? globosa ($F\ddot utterer$1984) Lentin and Williams 1985 and Pirumella krasheninnikovii (Bolli 1974) Lentin and Williams 1993 from latest Campanian and earliest Maastrichtian of ODP Hole 690C (Weddell Sea, Antarctic Ocean) have been studied in order to evaluate the species' depth habitat in the water column and their applicability in paleoceanographic studies. The calcareous dinoflagellates show isotopic values comparable to probably shallow-dwelling planktic foraminifera from the same samples in δ18O, but have an offset of about$-5\textperthousand$to$-7\textperthousand$in δ13C. This suggests that calcareous dinoflagellate oxygen isotopes may provide information for paleoceanographic reconstructions of sea-surface water temperatures, whereas their extremely light carbon isotope values are probably due to photosynthetic processes. |
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This suggests that calcareous dinoflagellate oxygen isotopes may provide information for paleoceanographic reconstructions of sea-surface water temperatures, whereas their extremely light carbon isotope values are probably due to photosynthetic processes.</description><identifier>ISSN: 0026-2803</identifier><identifier>EISSN: 1937-2795</identifier><identifier>DOI: 10.2113/49.4.375</identifier><language>eng</language><publisher>American Museum of Natural History</publisher><subject>C-13/C-12 ; Campanian ; carbon ; Carbon isotopes ; Cretaceous ; Cysts ; depth ; Dinoflagellata ; Drilling ; Foraminifera ; geochemical indicators ; geochemistry ; isotope ratios ; Isotopes ; Leg 113 ; lower Maestrichtian ; Maestrichtian ; Mesozoic ; microfossils ; Micropaleontology ; morphology ; O-18/O-16 ; Ocean Drilling Program ; Oceans ; ODP Site 690 ; Orthopithonella ; Oxygen ; Oxygen isotopes ; paleo-oceanography ; paleoecology ; palynomorphs ; photochemistry ; photosynthesis ; Seas ; Senonian ; Southern Ocean ; stable isotopes ; Stratigraphy ; Taxa ; upper Campanian ; Upper Cretaceous ; Weddell Sea</subject><ispartof>Micropaleontology, 2003-12, Vol.49 (4), p.375-380</ispartof><rights>GeoRef, Copyright 2020, American Geosciences Institute.</rights><rights>Copyright 2003 The Micropaleontology Project, Inc.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a336t-48718d7286102939da15b86f338c2e387390f6a7bfdf1f27df96430d9697a5c53</citedby></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.jstor.org/stable/pdf/3648454$$EPDF$$P50$$Gjstor$$H</linktopdf><linktohtml>$$Uhttps://www.jstor.org/stable/3648454$$EHTML$$P50$$Gjstor$$H</linktohtml><link.rule.ids>314,776,780,27903,27904,58216,58449</link.rule.ids></links><search><creatorcontrib>Friedrich, Oliver</creatorcontrib><creatorcontrib>Meier, K. J. Sebastian</creatorcontrib><title>Stable isotopic indication for the cyst formation depth of Campanian/Maastrichtian calcareous dinoflagellates</title><title>Micropaleontology</title><description>δ18O and δ13C values for the calcareous dinoflagellate species Orthopithonella? globosa ($F\ddot utterer$1984) Lentin and Williams 1985 and Pirumella krasheninnikovii (Bolli 1974) Lentin and Williams 1993 from latest Campanian and earliest Maastrichtian of ODP Hole 690C (Weddell Sea, Antarctic Ocean) have been studied in order to evaluate the species' depth habitat in the water column and their applicability in paleoceanographic studies. The calcareous dinoflagellates show isotopic values comparable to probably shallow-dwelling planktic foraminifera from the same samples in δ18O, but have an offset of about$-5\textperthousand$to$-7\textperthousand$in δ13C. This suggests that calcareous dinoflagellate oxygen isotopes may provide information for paleoceanographic reconstructions of sea-surface water temperatures, whereas their extremely light carbon isotope values are probably due to photosynthetic processes.</description><subject>C-13/C-12</subject><subject>Campanian</subject><subject>carbon</subject><subject>Carbon isotopes</subject><subject>Cretaceous</subject><subject>Cysts</subject><subject>depth</subject><subject>Dinoflagellata</subject><subject>Drilling</subject><subject>Foraminifera</subject><subject>geochemical indicators</subject><subject>geochemistry</subject><subject>isotope ratios</subject><subject>Isotopes</subject><subject>Leg 113</subject><subject>lower Maestrichtian</subject><subject>Maestrichtian</subject><subject>Mesozoic</subject><subject>microfossils</subject><subject>Micropaleontology</subject><subject>morphology</subject><subject>O-18/O-16</subject><subject>Ocean Drilling Program</subject><subject>Oceans</subject><subject>ODP Site 690</subject><subject>Orthopithonella</subject><subject>Oxygen</subject><subject>Oxygen isotopes</subject><subject>paleo-oceanography</subject><subject>paleoecology</subject><subject>palynomorphs</subject><subject>photochemistry</subject><subject>photosynthesis</subject><subject>Seas</subject><subject>Senonian</subject><subject>Southern Ocean</subject><subject>stable isotopes</subject><subject>Stratigraphy</subject><subject>Taxa</subject><subject>upper Campanian</subject><subject>Upper Cretaceous</subject><subject>Weddell Sea</subject><issn>0026-2803</issn><issn>1937-2795</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2003</creationdate><recordtype>article</recordtype><recordid>eNo9kEtrHDEQhEVIIBsnkB-Qg04mEGat1-hxDEsSG9b4kOQsevXwapkZjSUtwf8-s4zxqamuj6a6EPpMyZZRym-E2YotV_0btKGGq44p079FG0KY7Jgm_D36UOuJEKKl6jdo_N3gMAScam55Tg6nyScHLeUJx1xwOwbsnmu7iHFd-zC3I84R72CcYUow3dwD1FaSO7ZFYQeDgxLyuWKfphwHeAzDAC3Uj-hdhKGGTy_zCv39-ePP7rbbP_y6233fd8C5bJ3QimqvmJaUMMONB9oftIyca8cC14obEiWoQ_SRRqZ8NFJw4o00CnrX8yt0vd6dS346h9rsmKq7hJgusSw1mnJN6AJ-XUFXcq0lRDuXNEJ5tpTYS59WGCvs0ueCflnRU225vHJcCi16sdjfVvsx5OpSmFz4l8vg7Smfy7Q8axkhwhLFdc_4fy6UgR0</recordid><startdate>20031201</startdate><enddate>20031201</enddate><creator>Friedrich, Oliver</creator><creator>Meier, K. J. Sebastian</creator><general>American Museum of Natural History</general><general>Dept. of Micropaleontology, American Museum of Natural History</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7TN</scope><scope>F1W</scope><scope>H95</scope><scope>H96</scope><scope>L.G</scope><scope>M7N</scope></search><sort><creationdate>20031201</creationdate><title>Stable isotopic indication for the cyst formation depth of Campanian/Maastrichtian calcareous dinoflagellates</title><author>Friedrich, Oliver ; Meier, K. J. Sebastian</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a336t-48718d7286102939da15b86f338c2e387390f6a7bfdf1f27df96430d9697a5c53</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2003</creationdate><topic>C-13/C-12</topic><topic>Campanian</topic><topic>carbon</topic><topic>Carbon isotopes</topic><topic>Cretaceous</topic><topic>Cysts</topic><topic>depth</topic><topic>Dinoflagellata</topic><topic>Drilling</topic><topic>Foraminifera</topic><topic>geochemical indicators</topic><topic>geochemistry</topic><topic>isotope ratios</topic><topic>Isotopes</topic><topic>Leg 113</topic><topic>lower Maestrichtian</topic><topic>Maestrichtian</topic><topic>Mesozoic</topic><topic>microfossils</topic><topic>Micropaleontology</topic><topic>morphology</topic><topic>O-18/O-16</topic><topic>Ocean Drilling Program</topic><topic>Oceans</topic><topic>ODP Site 690</topic><topic>Orthopithonella</topic><topic>Oxygen</topic><topic>Oxygen isotopes</topic><topic>paleo-oceanography</topic><topic>paleoecology</topic><topic>palynomorphs</topic><topic>photochemistry</topic><topic>photosynthesis</topic><topic>Seas</topic><topic>Senonian</topic><topic>Southern Ocean</topic><topic>stable isotopes</topic><topic>Stratigraphy</topic><topic>Taxa</topic><topic>upper Campanian</topic><topic>Upper Cretaceous</topic><topic>Weddell Sea</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Friedrich, Oliver</creatorcontrib><creatorcontrib>Meier, K. J. Sebastian</creatorcontrib><collection>CrossRef</collection><collection>Oceanic Abstracts</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 1: Biological Sciences & Living Resources</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Algology Mycology and Protozoology Abstracts (Microbiology C)</collection><jtitle>Micropaleontology</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Friedrich, Oliver</au><au>Meier, K. J. Sebastian</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Stable isotopic indication for the cyst formation depth of Campanian/Maastrichtian calcareous dinoflagellates</atitle><jtitle>Micropaleontology</jtitle><date>2003-12-01</date><risdate>2003</risdate><volume>49</volume><issue>4</issue><spage>375</spage><epage>380</epage><pages>375-380</pages><issn>0026-2803</issn><eissn>1937-2795</eissn><abstract>δ18O and δ13C values for the calcareous dinoflagellate species Orthopithonella? globosa ($F\ddot utterer$1984) Lentin and Williams 1985 and Pirumella krasheninnikovii (Bolli 1974) Lentin and Williams 1993 from latest Campanian and earliest Maastrichtian of ODP Hole 690C (Weddell Sea, Antarctic Ocean) have been studied in order to evaluate the species' depth habitat in the water column and their applicability in paleoceanographic studies. The calcareous dinoflagellates show isotopic values comparable to probably shallow-dwelling planktic foraminifera from the same samples in δ18O, but have an offset of about$-5\textperthousand$to$-7\textperthousand$in δ13C. This suggests that calcareous dinoflagellate oxygen isotopes may provide information for paleoceanographic reconstructions of sea-surface water temperatures, whereas their extremely light carbon isotope values are probably due to photosynthetic processes.</abstract><pub>American Museum of Natural History</pub><doi>10.2113/49.4.375</doi><tpages>6</tpages></addata></record> |
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subjects | C-13/C-12 Campanian carbon Carbon isotopes Cretaceous Cysts depth Dinoflagellata Drilling Foraminifera geochemical indicators geochemistry isotope ratios Isotopes Leg 113 lower Maestrichtian Maestrichtian Mesozoic microfossils Micropaleontology morphology O-18/O-16 Ocean Drilling Program Oceans ODP Site 690 Orthopithonella Oxygen Oxygen isotopes paleo-oceanography paleoecology palynomorphs photochemistry photosynthesis Seas Senonian Southern Ocean stable isotopes Stratigraphy Taxa upper Campanian Upper Cretaceous Weddell Sea |
title | Stable isotopic indication for the cyst formation depth of Campanian/Maastrichtian calcareous dinoflagellates |
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