(Table 1) Age determination of composite sediment record LO09-14 ...
A sediment core from Reykjanes Ridge has been studied at 10- to 50-year time resolution to document variability of Holocene surface water conditions in the western North Atlantic and to evaluate effects of Holocene ice-rafting episodes. Diatom assemblages are converted to quantitative sea surface te...
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ftdatacite:10.1594/pangaea.832194 2024-09-15T18:12:27+00:00 (Table 1) Age determination of composite sediment record LO09-14 ... Berner, K S Koç, Nalân Divine, Dmitry V Godtliebsen, Fred Moros, Matthias 2008 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.832194 https://doi.pangaea.de/10.1594/PANGAEA.832194 en eng PANGAEA https://dx.doi.org/10.1029/2006pa001339 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Event label DEPTH, sediment/rock Depth, composite Laboratory code/label Age, dated Age, dated standard deviation Calendar age Gravity corer Giant box corer Kasten corer Gravity corer Kiel type Intercore correlation Age, 14C AMS Age, 14C calibrated LO09 Professor Logachev dataset Supplementary Dataset Dataset 2008 ftdatacite https://doi.org/10.1594/pangaea.83219410.1029/2006pa001339 2024-08-01T10:51:31Z A sediment core from Reykjanes Ridge has been studied at 10- to 50-year time resolution to document variability of Holocene surface water conditions in the western North Atlantic and to evaluate effects of Holocene ice-rafting episodes. Diatom assemblages are converted to quantitative sea surface temperatures (SST) using three different transfer functions. Spectral and scale-space methods are also applied on the records to explore variability at different timescales. Diatom assemblage and SST records clearly show that decaying remnants of the Laurentide ice sheet strongly influenced early Holocene climate in the western North Atlantic. This overrode the predominance of Milankovitch forcing, which played a key role in the development of Holocene climate in the eastern North Atlantic and Nordic Seas. Superimposed on general Holocene climate change is high-frequency SST variability on the order of 1°-3°C. The record also documents climatic oscillations with 600- to 1000-, ~1500-, and 2500-year periodicities, ... : All measurements are made on the foraminifer species Globigerina bulloides. ... Dataset Ice Sheet Nordic Seas North Atlantic DataCite |
institution |
Open Polar |
collection |
DataCite |
op_collection_id |
ftdatacite |
language |
English |
topic |
Event label DEPTH, sediment/rock Depth, composite Laboratory code/label Age, dated Age, dated standard deviation Calendar age Gravity corer Giant box corer Kasten corer Gravity corer Kiel type Intercore correlation Age, 14C AMS Age, 14C calibrated LO09 Professor Logachev |
spellingShingle |
Event label DEPTH, sediment/rock Depth, composite Laboratory code/label Age, dated Age, dated standard deviation Calendar age Gravity corer Giant box corer Kasten corer Gravity corer Kiel type Intercore correlation Age, 14C AMS Age, 14C calibrated LO09 Professor Logachev Berner, K S Koç, Nalân Divine, Dmitry V Godtliebsen, Fred Moros, Matthias (Table 1) Age determination of composite sediment record LO09-14 ... |
topic_facet |
Event label DEPTH, sediment/rock Depth, composite Laboratory code/label Age, dated Age, dated standard deviation Calendar age Gravity corer Giant box corer Kasten corer Gravity corer Kiel type Intercore correlation Age, 14C AMS Age, 14C calibrated LO09 Professor Logachev |
description |
A sediment core from Reykjanes Ridge has been studied at 10- to 50-year time resolution to document variability of Holocene surface water conditions in the western North Atlantic and to evaluate effects of Holocene ice-rafting episodes. Diatom assemblages are converted to quantitative sea surface temperatures (SST) using three different transfer functions. Spectral and scale-space methods are also applied on the records to explore variability at different timescales. Diatom assemblage and SST records clearly show that decaying remnants of the Laurentide ice sheet strongly influenced early Holocene climate in the western North Atlantic. This overrode the predominance of Milankovitch forcing, which played a key role in the development of Holocene climate in the eastern North Atlantic and Nordic Seas. Superimposed on general Holocene climate change is high-frequency SST variability on the order of 1°-3°C. The record also documents climatic oscillations with 600- to 1000-, ~1500-, and 2500-year periodicities, ... : All measurements are made on the foraminifer species Globigerina bulloides. ... |
format |
Dataset |
author |
Berner, K S Koç, Nalân Divine, Dmitry V Godtliebsen, Fred Moros, Matthias |
author_facet |
Berner, K S Koç, Nalân Divine, Dmitry V Godtliebsen, Fred Moros, Matthias |
author_sort |
Berner, K S |
title |
(Table 1) Age determination of composite sediment record LO09-14 ... |
title_short |
(Table 1) Age determination of composite sediment record LO09-14 ... |
title_full |
(Table 1) Age determination of composite sediment record LO09-14 ... |
title_fullStr |
(Table 1) Age determination of composite sediment record LO09-14 ... |
title_full_unstemmed |
(Table 1) Age determination of composite sediment record LO09-14 ... |
title_sort |
(table 1) age determination of composite sediment record lo09-14 ... |
publisher |
PANGAEA |
publishDate |
2008 |
url |
https://dx.doi.org/10.1594/pangaea.832194 https://doi.pangaea.de/10.1594/PANGAEA.832194 |
genre |
Ice Sheet Nordic Seas North Atlantic |
genre_facet |
Ice Sheet Nordic Seas North Atlantic |
op_relation |
https://dx.doi.org/10.1029/2006pa001339 |
op_rights |
Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 |
op_doi |
https://doi.org/10.1594/pangaea.83219410.1029/2006pa001339 |
_version_ |
1810450033723572224 |