Stable oxygen and carbon isotope ratios of Globigerina bulloides in sediment core MD95-2042 of the Iberian Margin, North Atlantic
A quantitative analysis of planktonic foraminifera in a core from the Iberian Margin allows a reconstruction of the evolution of oceanographic parameters during the last glacial cycle with a resolution of ~1000 years. A principal component analysis performed on 19 species allows the identification o...
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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.60829 2023-05-15T17:34:38+02:00 Stable oxygen and carbon isotope ratios of Globigerina bulloides in sediment core MD95-2042 of the Iberian Margin, North Atlantic Cayre, Olivia Vincent, Edith Lancelot, Yves Hall, Michael A LATITUDE: 37.799833 * LONGITUDE: -10.166500 * DATE/TIME START: 1995-07-09T00:00:00 * DATE/TIME END: 1995-07-09T00:00:00 * MINIMUM DEPTH, sediment/rock: 0.0 m * MAXIMUM DEPTH, sediment/rock: 29.8 m 1999-07-07 text/tab-separated-values, 368 data points https://doi.pangaea.de/10.1594/PANGAEA.60829 https://doi.org/10.1594/PANGAEA.60829 en eng PANGAEA https://doi.pangaea.de/10.1594/PANGAEA.60829 https://doi.org/10.1594/PANGAEA.60829 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess CC-BY Supplement to: Cayre, Olivia; Lancelot, Yves; Vincent, Edith; Hall, Melinda (1999): Paleoceanographic reconstructions from planctonic foraminifera off the Iberian Margin: temperature, salinity and Heinrich Events. Paleoceanography, 14(3), 384-396, https://doi.org/10.1029/1998PA900027 CALYPSO Calypso Corer DEPTH sediment/rock Globigerina bulloides δ13C δ18O IMAGES IMAGES I International Marine Global Change Study Marge Ibérique Marion Dufresne (1995) Mass spectrometer VG SIRA MD101 MD952042 MD95-2042 Dataset 1999 ftpangaea https://doi.org/10.1594/PANGAEA.60829 https://doi.org/10.1029/1998PA900027 2023-01-20T07:36:36Z A quantitative analysis of planktonic foraminifera in a core from the Iberian Margin allows a reconstruction of the evolution of oceanographic parameters during the last glacial cycle with a resolution of ~1000 years. A principal component analysis performed on 19 species allows the identification of 11 intervals characterized by increased abundances of the subpolar species. The youngest six of these intervals are correlated with the last 6 Heinrich events (HEs). The five cold events older than stage 4 are dated at 81, 90, 110, 129, and 140 ka, respectively. Paleotemperatures reconstructed using the modern analog technique indicate 4°C decreases during all even-numbered isotopic stages and stage 3. During the HEs, temperature decreases reach ~10°C and seawater delta18O anomalies reach ~1 per mil. Temperature and salinity reconstructions indicate that the environment of the Iberian Margin has been under the combined influence of global factors such as the migration of the polar front and iceberg discharge and of regional factors such as the precipitation/evaporation regime on both oceanic and continental area. Dataset North Atlantic Planktonic foraminifera PANGAEA - Data Publisher for Earth & Environmental Science Sira ENVELOPE(8.107,8.107,62.667,62.667) ENVELOPE(-10.166500,-10.166500,37.799833,37.799833) |
institution |
Open Polar |
collection |
PANGAEA - Data Publisher for Earth & Environmental Science |
op_collection_id |
ftpangaea |
language |
English |
topic |
CALYPSO Calypso Corer DEPTH sediment/rock Globigerina bulloides δ13C δ18O IMAGES IMAGES I International Marine Global Change Study Marge Ibérique Marion Dufresne (1995) Mass spectrometer VG SIRA MD101 MD952042 MD95-2042 |
spellingShingle |
CALYPSO Calypso Corer DEPTH sediment/rock Globigerina bulloides δ13C δ18O IMAGES IMAGES I International Marine Global Change Study Marge Ibérique Marion Dufresne (1995) Mass spectrometer VG SIRA MD101 MD952042 MD95-2042 Cayre, Olivia Vincent, Edith Lancelot, Yves Hall, Michael A Stable oxygen and carbon isotope ratios of Globigerina bulloides in sediment core MD95-2042 of the Iberian Margin, North Atlantic |
topic_facet |
CALYPSO Calypso Corer DEPTH sediment/rock Globigerina bulloides δ13C δ18O IMAGES IMAGES I International Marine Global Change Study Marge Ibérique Marion Dufresne (1995) Mass spectrometer VG SIRA MD101 MD952042 MD95-2042 |
description |
A quantitative analysis of planktonic foraminifera in a core from the Iberian Margin allows a reconstruction of the evolution of oceanographic parameters during the last glacial cycle with a resolution of ~1000 years. A principal component analysis performed on 19 species allows the identification of 11 intervals characterized by increased abundances of the subpolar species. The youngest six of these intervals are correlated with the last 6 Heinrich events (HEs). The five cold events older than stage 4 are dated at 81, 90, 110, 129, and 140 ka, respectively. Paleotemperatures reconstructed using the modern analog technique indicate 4°C decreases during all even-numbered isotopic stages and stage 3. During the HEs, temperature decreases reach ~10°C and seawater delta18O anomalies reach ~1 per mil. Temperature and salinity reconstructions indicate that the environment of the Iberian Margin has been under the combined influence of global factors such as the migration of the polar front and iceberg discharge and of regional factors such as the precipitation/evaporation regime on both oceanic and continental area. |
format |
Dataset |
author |
Cayre, Olivia Vincent, Edith Lancelot, Yves Hall, Michael A |
author_facet |
Cayre, Olivia Vincent, Edith Lancelot, Yves Hall, Michael A |
author_sort |
Cayre, Olivia |
title |
Stable oxygen and carbon isotope ratios of Globigerina bulloides in sediment core MD95-2042 of the Iberian Margin, North Atlantic |
title_short |
Stable oxygen and carbon isotope ratios of Globigerina bulloides in sediment core MD95-2042 of the Iberian Margin, North Atlantic |
title_full |
Stable oxygen and carbon isotope ratios of Globigerina bulloides in sediment core MD95-2042 of the Iberian Margin, North Atlantic |
title_fullStr |
Stable oxygen and carbon isotope ratios of Globigerina bulloides in sediment core MD95-2042 of the Iberian Margin, North Atlantic |
title_full_unstemmed |
Stable oxygen and carbon isotope ratios of Globigerina bulloides in sediment core MD95-2042 of the Iberian Margin, North Atlantic |
title_sort |
stable oxygen and carbon isotope ratios of globigerina bulloides in sediment core md95-2042 of the iberian margin, north atlantic |
publisher |
PANGAEA |
publishDate |
1999 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.60829 https://doi.org/10.1594/PANGAEA.60829 |
op_coverage |
LATITUDE: 37.799833 * LONGITUDE: -10.166500 * DATE/TIME START: 1995-07-09T00:00:00 * DATE/TIME END: 1995-07-09T00:00:00 * MINIMUM DEPTH, sediment/rock: 0.0 m * MAXIMUM DEPTH, sediment/rock: 29.8 m |
long_lat |
ENVELOPE(8.107,8.107,62.667,62.667) ENVELOPE(-10.166500,-10.166500,37.799833,37.799833) |
geographic |
Sira |
geographic_facet |
Sira |
genre |
North Atlantic Planktonic foraminifera |
genre_facet |
North Atlantic Planktonic foraminifera |
op_source |
Supplement to: Cayre, Olivia; Lancelot, Yves; Vincent, Edith; Hall, Melinda (1999): Paleoceanographic reconstructions from planctonic foraminifera off the Iberian Margin: temperature, salinity and Heinrich Events. Paleoceanography, 14(3), 384-396, https://doi.org/10.1029/1998PA900027 |
op_relation |
https://doi.pangaea.de/10.1594/PANGAEA.60829 https://doi.org/10.1594/PANGAEA.60829 |
op_rights |
CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1594/PANGAEA.60829 https://doi.org/10.1029/1998PA900027 |
_version_ |
1766133537161871360 |