Latitudinal variation in the planktic foraminifer Contusotruncana contusa in the terminal Cretaceous ocean ...
The morphological variability (coiling properties, size and shape) of the planktic foraminifer Contusortuncana contusa (Cushman) in the terminal Cretaceous ocean was examined at eight deep-sea sites and two continental sections from low (16°) to middle (42°) paleolatitudes in both hemispheres. The m...
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Online Access: | https://dx.doi.org/10.1594/pangaea.681878 https://doi.pangaea.de/10.1594/PANGAEA.681878 |
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ftdatacite:10.1594/pangaea.681878 2024-09-30T14:39:39+00:00 Latitudinal variation in the planktic foraminifer Contusotruncana contusa in the terminal Cretaceous ocean ... Kucera, Michal Malmgren, Bjorn 1996 application/zip https://dx.doi.org/10.1594/pangaea.681878 https://doi.pangaea.de/10.1594/PANGAEA.681878 en eng PANGAEA https://dx.doi.org/10.1016/0377-8398(95)00078-x Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Drilling/drill rig Outcrop sample Leg39 Leg43 Leg62 Leg74 Leg80 Leg122 Glomar Challenger Joides Resolution Deep Sea Drilling Project DSDP Ocean Drilling Program ODP Collection Supplementary Publication Series of Datasets article 1996 ftdatacite https://doi.org/10.1594/pangaea.68187810.1016/0377-8398(95)00078-x 2024-09-02T08:35:09Z The morphological variability (coiling properties, size and shape) of the planktic foraminifer Contusortuncana contusa (Cushman) in the terminal Cretaceous ocean was examined at eight deep-sea sites and two continental sections from low (16°) to middle (42°) paleolatitudes in both hemispheres. The material used in this study includes samples from the South Atlantic (DSDP Sites 356, 527 and 525A), North Atlantic (Sites 384 and 548A), Indian and Pacific Oceans (DSDP Site 465A and ODP Sites 761C and 762C) and Tethyan Ocean (outcrop sections from El-Kef and Caravaca). On average 45 specimens from two samples per location were analysed, from an interval corresponding approximately to the last 60 kyr of the Cretaceous.No differences in coiling direction (dextral proportions were > 90% in all samples), percentage of kummerform specimens (usually > 50%) and number of chambers in the last whorl (4-5) were observed between the sites. Both test size (expressed as spiral outline area and test volume) and total ... : Supplement to: Kucera, Michal; Malmgren, Bjorn (1996): Latitudinal variation in the planktic foraminifer Contusotruncana contusa in the terminal Cretaceous ocean. Marine Micropaleontology, 28(1), 31-52 ... Article in Journal/Newspaper North Atlantic DataCite Indian Malmgren ENVELOPE(-66.117,-66.117,-65.750,-65.750) Pacific |
institution |
Open Polar |
collection |
DataCite |
op_collection_id |
ftdatacite |
language |
English |
topic |
Drilling/drill rig Outcrop sample Leg39 Leg43 Leg62 Leg74 Leg80 Leg122 Glomar Challenger Joides Resolution Deep Sea Drilling Project DSDP Ocean Drilling Program ODP |
spellingShingle |
Drilling/drill rig Outcrop sample Leg39 Leg43 Leg62 Leg74 Leg80 Leg122 Glomar Challenger Joides Resolution Deep Sea Drilling Project DSDP Ocean Drilling Program ODP Kucera, Michal Malmgren, Bjorn Latitudinal variation in the planktic foraminifer Contusotruncana contusa in the terminal Cretaceous ocean ... |
topic_facet |
Drilling/drill rig Outcrop sample Leg39 Leg43 Leg62 Leg74 Leg80 Leg122 Glomar Challenger Joides Resolution Deep Sea Drilling Project DSDP Ocean Drilling Program ODP |
description |
The morphological variability (coiling properties, size and shape) of the planktic foraminifer Contusortuncana contusa (Cushman) in the terminal Cretaceous ocean was examined at eight deep-sea sites and two continental sections from low (16°) to middle (42°) paleolatitudes in both hemispheres. The material used in this study includes samples from the South Atlantic (DSDP Sites 356, 527 and 525A), North Atlantic (Sites 384 and 548A), Indian and Pacific Oceans (DSDP Site 465A and ODP Sites 761C and 762C) and Tethyan Ocean (outcrop sections from El-Kef and Caravaca). On average 45 specimens from two samples per location were analysed, from an interval corresponding approximately to the last 60 kyr of the Cretaceous.No differences in coiling direction (dextral proportions were > 90% in all samples), percentage of kummerform specimens (usually > 50%) and number of chambers in the last whorl (4-5) were observed between the sites. Both test size (expressed as spiral outline area and test volume) and total ... : Supplement to: Kucera, Michal; Malmgren, Bjorn (1996): Latitudinal variation in the planktic foraminifer Contusotruncana contusa in the terminal Cretaceous ocean. Marine Micropaleontology, 28(1), 31-52 ... |
format |
Article in Journal/Newspaper |
author |
Kucera, Michal Malmgren, Bjorn |
author_facet |
Kucera, Michal Malmgren, Bjorn |
author_sort |
Kucera, Michal |
title |
Latitudinal variation in the planktic foraminifer Contusotruncana contusa in the terminal Cretaceous ocean ... |
title_short |
Latitudinal variation in the planktic foraminifer Contusotruncana contusa in the terminal Cretaceous ocean ... |
title_full |
Latitudinal variation in the planktic foraminifer Contusotruncana contusa in the terminal Cretaceous ocean ... |
title_fullStr |
Latitudinal variation in the planktic foraminifer Contusotruncana contusa in the terminal Cretaceous ocean ... |
title_full_unstemmed |
Latitudinal variation in the planktic foraminifer Contusotruncana contusa in the terminal Cretaceous ocean ... |
title_sort |
latitudinal variation in the planktic foraminifer contusotruncana contusa in the terminal cretaceous ocean ... |
publisher |
PANGAEA |
publishDate |
1996 |
url |
https://dx.doi.org/10.1594/pangaea.681878 https://doi.pangaea.de/10.1594/PANGAEA.681878 |
long_lat |
ENVELOPE(-66.117,-66.117,-65.750,-65.750) |
geographic |
Indian Malmgren Pacific |
geographic_facet |
Indian Malmgren Pacific |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_relation |
https://dx.doi.org/10.1016/0377-8398(95)00078-x |
op_rights |
Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 |
op_doi |
https://doi.org/10.1594/pangaea.68187810.1016/0377-8398(95)00078-x |
_version_ |
1811642259273154560 |