Stable carbon and oxygen isotope ratios of bulk sediment from the Weddell Sea

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Auteurs principaux: Shackleton, Nicholas J, Hall, Michael A
Format: Dataset Open Access
Langue:en
Publié: PANGAEA 1990
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author Shackleton, Nicholas J
Hall, Michael A
author_facet Shackleton, Nicholas J
Hall, Michael A
collection Datos científicos de ciencias marinas y ambientales
contents Carbon isotope measurements were made on bulk sediments from the well preserved calcareous sequences recovered at ODP Sites 689 and 690 on the Maud Rise, Weddell Sea, Antarctica. The very positive delta13C values that characterize the late Paleocene and the rapid trend toward lighter values in the early Eocene established in other sites are clearly recorded here and may be of value for long-distance stratigraphic correlation. However, values in the late Eocene are significantly more positive than have been reported from other areas. The general pattern of the records from Sites 689 and 690 is sufficiently unlike those previously reported from lower latitudes that we suggest that carbon isotope data should be used only with considerable caution for correlating sequences from such high latitudes with lower latitude records.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_726425
institution PANGAEA
language en
publishDate 1990
publisher PANGAEA
record_format pangaea
spellingShingle Stable carbon and oxygen isotope ratios of bulk sediment from the Weddell Sea
Shackleton, Nicholas J
Hall, Michael A
113-689B; 113-690B; 113-690C; DRILL; Drilling/drill rig; Joides Resolution; Leg113; Ocean Drilling Program; ODP; South Atlantic Ocean
Carbon isotope measurements were made on bulk sediments from the well preserved calcareous sequences recovered at ODP Sites 689 and 690 on the Maud Rise, Weddell Sea, Antarctica. The very positive delta13C values that characterize the late Paleocene and the rapid trend toward lighter values in the early Eocene established in other sites are clearly recorded here and may be of value for long-distance stratigraphic correlation. However, values in the late Eocene are significantly more positive than have been reported from other areas. The general pattern of the records from Sites 689 and 690 is sufficiently unlike those previously reported from lower latitudes that we suggest that carbon isotope data should be used only with considerable caution for correlating sequences from such high latitudes with lower latitude records.
title Stable carbon and oxygen isotope ratios of bulk sediment from the Weddell Sea
topic 113-689B; 113-690B; 113-690C; DRILL; Drilling/drill rig; Joides Resolution; Leg113; Ocean Drilling Program; ODP; South Atlantic Ocean
url https://doi.org/10.1594/PANGAEA.726425