(Table 1) Thickness of the Holocene layer and sedimentation rates in the Atlantic Ocean
On the basis of planktonic foraminifera study, thickness of Holocene sediments has been ascertained in 60 sediment cores from various regions of the Atlantic Ocean. Ratios of species reflect warming of the upper water layer at the Pleistocene-Holocene boundary over the entire ocean. The Holocene bou...
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| Format: | Dataset |
| Language: | English |
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PANGAEA
1977
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| Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.754862 https://doi.org/10.1594/PANGAEA.754862 |
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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.754862 |
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openpolar |
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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.754862 2023-05-15T17:12:45+02:00 (Table 1) Thickness of the Holocene layer and sedimentation rates in the Atlantic Ocean Barash, Max S Lavrov, Vadim M MEDIAN LATITUDE: 29.919000 * MEDIAN LONGITUDE: -27.021583 * SOUTH-BOUND LATITUDE: -35.278333 * WEST-BOUND LONGITUDE: -78.310000 * NORTH-BOUND LATITUDE: 63.946667 * EAST-BOUND LONGITUDE: 7.896667 * MINIMUM ELEVATION: -5260.0 m * MAXIMUM ELEVATION: -670.0 m 1977-12-08 text/tab-separated-values, 120 data points https://doi.pangaea.de/10.1594/PANGAEA.754862 https://doi.org/10.1594/PANGAEA.754862 en eng PANGAEA https://doi.pangaea.de/10.1594/PANGAEA.754862 https://doi.org/10.1594/PANGAEA.754862 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess CC-BY P.P. Shirshov Institute of Oceanology, Russian Academy of Sciences, Moscow Supplement to: Barash, Max S; Lavrov, Vadim M (1977): On the thickness of the Holocene sediments within the bottom deposits of the Atlantic Ocean. Oceanology, 17(2), 172-176 AK10-K-838GC AK1-K-39GC AK3-K-121GC AK3-K-176GC AK3-K-178GC AK3-K-200GC AK3-K-212GC AK6-K-432GC AK6-K-434GC Akademik Kurchatov AKU1 AKU10 AKU3 AKU6 Archive of Ocean Data ARCOD Atlantic Ocean Calculated Counting foraminifera planktic DM1 DM1-M-2GC Dmitry Mendeleev E-156GC E-159GC E-170GC Elevation of event Event label GC Gravity corer Latitude of event Longitude of event Mikhail Lomonosov ML1 ML1_19GC ML1_26GC ML1_36GC ML1_61GC ML1_66GC ML10 ML10_827GC ML10_860GC ML10_878GC ML10_885GC ML10_909GC ML12 ML12_1033GC ML12_1045GC ML12_1056GC Dataset 1977 ftpangaea https://doi.org/10.1594/PANGAEA.754862 2023-01-20T08:51:46Z On the basis of planktonic foraminifera study, thickness of Holocene sediments has been ascertained in 60 sediment cores from various regions of the Atlantic Ocean. Ratios of species reflect warming of the upper water layer at the Pleistocene-Holocene boundary over the entire ocean. The Holocene boundary can be determined not only from microfaunal data, but also from lithologic ones including textural and structural features. Increase in CaCO3 contents in Holocene sediments as compared to Pleistocene is from 5-7% to 60-70% in different parts of the ocean. Dataset Mikhail Lomonosov Planktonic foraminifera PANGAEA - Data Publisher for Earth & Environmental Science ENVELOPE(-78.310000,7.896667,63.946667,-35.278333) |
| institution |
Open Polar |
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PANGAEA - Data Publisher for Earth & Environmental Science |
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ftpangaea |
| language |
English |
| topic |
AK10-K-838GC AK1-K-39GC AK3-K-121GC AK3-K-176GC AK3-K-178GC AK3-K-200GC AK3-K-212GC AK6-K-432GC AK6-K-434GC Akademik Kurchatov AKU1 AKU10 AKU3 AKU6 Archive of Ocean Data ARCOD Atlantic Ocean Calculated Counting foraminifera planktic DM1 DM1-M-2GC Dmitry Mendeleev E-156GC E-159GC E-170GC Elevation of event Event label GC Gravity corer Latitude of event Longitude of event Mikhail Lomonosov ML1 ML1_19GC ML1_26GC ML1_36GC ML1_61GC ML1_66GC ML10 ML10_827GC ML10_860GC ML10_878GC ML10_885GC ML10_909GC ML12 ML12_1033GC ML12_1045GC ML12_1056GC |
| spellingShingle |
AK10-K-838GC AK1-K-39GC AK3-K-121GC AK3-K-176GC AK3-K-178GC AK3-K-200GC AK3-K-212GC AK6-K-432GC AK6-K-434GC Akademik Kurchatov AKU1 AKU10 AKU3 AKU6 Archive of Ocean Data ARCOD Atlantic Ocean Calculated Counting foraminifera planktic DM1 DM1-M-2GC Dmitry Mendeleev E-156GC E-159GC E-170GC Elevation of event Event label GC Gravity corer Latitude of event Longitude of event Mikhail Lomonosov ML1 ML1_19GC ML1_26GC ML1_36GC ML1_61GC ML1_66GC ML10 ML10_827GC ML10_860GC ML10_878GC ML10_885GC ML10_909GC ML12 ML12_1033GC ML12_1045GC ML12_1056GC Barash, Max S Lavrov, Vadim M (Table 1) Thickness of the Holocene layer and sedimentation rates in the Atlantic Ocean |
| topic_facet |
AK10-K-838GC AK1-K-39GC AK3-K-121GC AK3-K-176GC AK3-K-178GC AK3-K-200GC AK3-K-212GC AK6-K-432GC AK6-K-434GC Akademik Kurchatov AKU1 AKU10 AKU3 AKU6 Archive of Ocean Data ARCOD Atlantic Ocean Calculated Counting foraminifera planktic DM1 DM1-M-2GC Dmitry Mendeleev E-156GC E-159GC E-170GC Elevation of event Event label GC Gravity corer Latitude of event Longitude of event Mikhail Lomonosov ML1 ML1_19GC ML1_26GC ML1_36GC ML1_61GC ML1_66GC ML10 ML10_827GC ML10_860GC ML10_878GC ML10_885GC ML10_909GC ML12 ML12_1033GC ML12_1045GC ML12_1056GC |
| description |
On the basis of planktonic foraminifera study, thickness of Holocene sediments has been ascertained in 60 sediment cores from various regions of the Atlantic Ocean. Ratios of species reflect warming of the upper water layer at the Pleistocene-Holocene boundary over the entire ocean. The Holocene boundary can be determined not only from microfaunal data, but also from lithologic ones including textural and structural features. Increase in CaCO3 contents in Holocene sediments as compared to Pleistocene is from 5-7% to 60-70% in different parts of the ocean. |
| format |
Dataset |
| author |
Barash, Max S Lavrov, Vadim M |
| author_facet |
Barash, Max S Lavrov, Vadim M |
| author_sort |
Barash, Max S |
| title |
(Table 1) Thickness of the Holocene layer and sedimentation rates in the Atlantic Ocean |
| title_short |
(Table 1) Thickness of the Holocene layer and sedimentation rates in the Atlantic Ocean |
| title_full |
(Table 1) Thickness of the Holocene layer and sedimentation rates in the Atlantic Ocean |
| title_fullStr |
(Table 1) Thickness of the Holocene layer and sedimentation rates in the Atlantic Ocean |
| title_full_unstemmed |
(Table 1) Thickness of the Holocene layer and sedimentation rates in the Atlantic Ocean |
| title_sort |
(table 1) thickness of the holocene layer and sedimentation rates in the atlantic ocean |
| publisher |
PANGAEA |
| publishDate |
1977 |
| url |
https://doi.pangaea.de/10.1594/PANGAEA.754862 https://doi.org/10.1594/PANGAEA.754862 |
| op_coverage |
MEDIAN LATITUDE: 29.919000 * MEDIAN LONGITUDE: -27.021583 * SOUTH-BOUND LATITUDE: -35.278333 * WEST-BOUND LONGITUDE: -78.310000 * NORTH-BOUND LATITUDE: 63.946667 * EAST-BOUND LONGITUDE: 7.896667 * MINIMUM ELEVATION: -5260.0 m * MAXIMUM ELEVATION: -670.0 m |
| long_lat |
ENVELOPE(-78.310000,7.896667,63.946667,-35.278333) |
| genre |
Mikhail Lomonosov Planktonic foraminifera |
| genre_facet |
Mikhail Lomonosov Planktonic foraminifera |
| op_source |
P.P. Shirshov Institute of Oceanology, Russian Academy of Sciences, Moscow Supplement to: Barash, Max S; Lavrov, Vadim M (1977): On the thickness of the Holocene sediments within the bottom deposits of the Atlantic Ocean. Oceanology, 17(2), 172-176 |
| op_relation |
https://doi.pangaea.de/10.1594/PANGAEA.754862 https://doi.org/10.1594/PANGAEA.754862 |
| 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.754862 |
| _version_ |
1766069598268948480 |