Occurrence of Inoceramus in the South Atlantic and oxygen isotopic paleotemperatures in DSDP Hole 75-530A

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Main Authors: Barron, E J, Saltzman, Eric S, Price, David A
Format: Dataset Open Access
Language:en
Published: PANGAEA 1984
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author Barron, E J
Saltzman, Eric S
Price, David A
author_facet Barron, E J
Saltzman, Eric S
Price, David A
collection Datos científicos de ciencias marinas y ambientales
contents Inoceramus occurs in every DSDP hole that penetrated Cretaceous sediments in the South Atlantic Ocean, and specimen occurrence has been mapped in detail for each core. Oxygen and carbon isotope measurements were completed on 18 Inoceramus specimens from Hole 530A. Textural evidence of diagenesis is accompanied by depletion in 18O. Paleotemperature results were obtained from 11 well-preserved specimens. Bottom water temperatures in the Angola Basin decreased from 23°C during the Coniacian to 13°C near the end of the Campanian.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_810137
institution PANGAEA
language en
publishDate 1984
publisher PANGAEA
record_format pangaea
spellingShingle Occurrence of Inoceramus in the South Atlantic and oxygen isotopic paleotemperatures in DSDP Hole 75-530A
Barron, E J
Saltzman, Eric S
Price, David A
3-21; 36-327A; 36-330; 39-355; 39-356; 39-357; 40-361; 40-363; 40-364; 75-530A; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Leg3; Leg36; Leg39; Leg40; Leg75; South Atlantic/BASIN; South Atlantic/CONT RISE; South Atlantic/PLATEAU; South Atlantic/RIDGE; South Atlantic/SYNCLINE; South Atlantic Ocean
Inoceramus occurs in every DSDP hole that penetrated Cretaceous sediments in the South Atlantic Ocean, and specimen occurrence has been mapped in detail for each core. Oxygen and carbon isotope measurements were completed on 18 Inoceramus specimens from Hole 530A. Textural evidence of diagenesis is accompanied by depletion in 18O. Paleotemperature results were obtained from 11 well-preserved specimens. Bottom water temperatures in the Angola Basin decreased from 23°C during the Coniacian to 13°C near the end of the Campanian.
title Occurrence of Inoceramus in the South Atlantic and oxygen isotopic paleotemperatures in DSDP Hole 75-530A
topic 3-21; 36-327A; 36-330; 39-355; 39-356; 39-357; 40-361; 40-363; 40-364; 75-530A; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Leg3; Leg36; Leg39; Leg40; Leg75; South Atlantic/BASIN; South Atlantic/CONT RISE; South Atlantic/PLATEAU; South Atlantic/RIDGE; South Atlantic/SYNCLINE; South Atlantic Ocean
url https://doi.org/10.1594/PANGAEA.810137