Contusotruncana contusa abundances and morphotypes in the cretaceous mid-latitude South Atlantic

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Main Authors: Kucera, Michal, Malmgren, Bjorn
Format: Dataset Open Access
Language:en
Published: PANGAEA 1998
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author Kucera, Michal
Malmgren, Bjorn
author_facet Kucera, Michal
Malmgren, Bjorn
collection Datos científicos de ciencias marinas y ambientales
contents Spatial and temporal patterns in test size and shape (test conicity and spiral roundness) and absolute abundance (accumulation rate) of the planktonic foraminifer Contusotruncana contusa were studied in the South Atlantic Ocean (DSDP sites 356, 516, 525 and 527) during an interval corresponding to the last 800 kyr of the Cretaceous. The variation in absolute abundance of C. contusa was characterised by alternating periods of high and low abundance; some of these periods were traceable across the entire mid-latitude South Atlantic Ocean. While the mean spiral roundness did not show any interpretable patterns, a sudden increase of the mean test size and mean test conicity occurred between 65.3 and 65.2 Ma (based on linear interpolation within the Cretaceous part of Subchron C29R) at all sites studied, indicating a poleward migration followed by rapid withdrawal of the low-latitude C. contusa morphotypes from the mid-latitude South Atlantic Ocean. We suggest that this event was caused by a short period of surface-water warming in the southern mid-latitudes corresponding to the brief high-latitude warming event and associated faunal migrations in the Boreal and Austral realms.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_704985
institution PANGAEA
language en
publishDate 1998
publisher PANGAEA
record_format pangaea
spellingShingle Contusotruncana contusa abundances and morphotypes in the cretaceous mid-latitude South Atlantic
Kucera, Michal
Malmgren, Bjorn
39-356; 43-384; 72-516F; 74-525A; 74-527; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Leg39; Leg43; Leg72; Leg74; North Atlantic/RIDGE; South Atlantic/CONT RISE; South Atlantic/CREST; South Atlantic/PLATEAU; South Atlantic Ocean
Spatial and temporal patterns in test size and shape (test conicity and spiral roundness) and absolute abundance (accumulation rate) of the planktonic foraminifer Contusotruncana contusa were studied in the South Atlantic Ocean (DSDP sites 356, 516, 525 and 527) during an interval corresponding to the last 800 kyr of the Cretaceous. The variation in absolute abundance of C. contusa was characterised by alternating periods of high and low abundance; some of these periods were traceable across the entire mid-latitude South Atlantic Ocean. While the mean spiral roundness did not show any interpretable patterns, a sudden increase of the mean test size and mean test conicity occurred between 65.3 and 65.2 Ma (based on linear interpolation within the Cretaceous part of Subchron C29R) at all sites studied, indicating a poleward migration followed by rapid withdrawal of the low-latitude C. contusa morphotypes from the mid-latitude South Atlantic Ocean. We suggest that this event was caused by a short period of surface-water warming in the southern mid-latitudes corresponding to the brief high-latitude warming event and associated faunal migrations in the Boreal and Austral realms.
title Contusotruncana contusa abundances and morphotypes in the cretaceous mid-latitude South Atlantic
topic 39-356; 43-384; 72-516F; 74-525A; 74-527; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Leg39; Leg43; Leg72; Leg74; North Atlantic/RIDGE; South Atlantic/CONT RISE; South Atlantic/CREST; South Atlantic/PLATEAU; South Atlantic Ocean
url https://doi.org/10.1594/PANGAEA.704985