_version_ 1867169119837618176
author Wang, Xiangli
Reinhard, Christopher T
Planavsky, Noah J
Owens, Jeremy D
Lyons, Timothy W
Johnson, Thomas M
author_facet Wang, Xiangli
Reinhard, Christopher T
Planavsky, Noah J
Owens, Jeremy D
Lyons, Timothy W
Johnson, Thomas M
collection Datos científicos de ciencias marinas y ambientales
contents In order to advance our understanding of the emerging chromium (Cr) isotope system as a paleoredox proxy, we measured the 53Cr/52Cr of black shales deposited before, during, and after Cretaceous Oceanic Anoxic Event 2 (OAE2). We observed a > 1 per mil coherent negative 53Cr/52Cr excursion and significant drawdown in Cr enrichments during OAE2 coincident with a large positive carbon isotope excursion. Our observed negative 53Cr/52Cr excursion during OAE2 is most easily linked to an increase in the ratio of euxinic to reducing conditions. Additional work on other OAE sections is needed to determine the spatial significance of this Cr isotope trend.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_873605
institution PANGAEA
language en
publishDate 2017
publisher PANGAEA
record_format pangaea
spellingShingle Geochemical results for black shale samples from different Holes of ODP Site 1258
Wang, Xiangli
Reinhard, Christopher T
Planavsky, Noah J
Owens, Jeremy D
Lyons, Timothy W
Johnson, Thomas M
207-1258A; 207-1258B; 207-1258C; AGE; Carbon, organic, total; Chromium; Depth, composite; DRILL; Drilling/drill rig; Event label; Fraction; Inductively coupled plasma-mass spectroscopy (ICP-MS), Agilent, 7500-ce; Joides Resolution; Leg207; Molybdenum; North Atlantic Ocean; Ocean Drilling Program; ODP; Sample code/label; Titanium; δ53Cr
In order to advance our understanding of the emerging chromium (Cr) isotope system as a paleoredox proxy, we measured the 53Cr/52Cr of black shales deposited before, during, and after Cretaceous Oceanic Anoxic Event 2 (OAE2). We observed a > 1 per mil coherent negative 53Cr/52Cr excursion and significant drawdown in Cr enrichments during OAE2 coincident with a large positive carbon isotope excursion. Our observed negative 53Cr/52Cr excursion during OAE2 is most easily linked to an increase in the ratio of euxinic to reducing conditions. Additional work on other OAE sections is needed to determine the spatial significance of this Cr isotope trend.
title Geochemical results for black shale samples from different Holes of ODP Site 1258
topic 207-1258A; 207-1258B; 207-1258C; AGE; Carbon, organic, total; Chromium; Depth, composite; DRILL; Drilling/drill rig; Event label; Fraction; Inductively coupled plasma-mass spectroscopy (ICP-MS), Agilent, 7500-ce; Joides Resolution; Leg207; Molybdenum; North Atlantic Ocean; Ocean Drilling Program; ODP; Sample code/label; Titanium; δ53Cr
url https://doi.org/10.1594/PANGAEA.873605