NOAA/WDS Paleoclimatology - Atlantic Ocean Pliocene Planktonic and Benthic d18O and Mg/Ca Data
This archived Paleoclimatology Study is available from the NOAA National Centers for Environmental Information (NCEI), under the World Data Service (WDS) for Paleoclimatology. The associated NCEI study type is Paleoceanography. The data include parameters of paleoceanography with a geographic location of North Atlantic Ocean. The time period coverage is from 6002000 to 2786000 in calendar years before present (BP). See metadata information for parameter and study location details. Please cite this study when using the data.
- Cite as: Karas, C.; Nürnberg, D.; Bahr, A.; Groeneveld, J.; Herrle, J.O.; Tiedemann, R.; deMenocal, P.B. (2017-01-04): NOAA/WDS Paleoclimatology - Atlantic Ocean Pliocene Planktonic and Benthic d18O and Mg/Ca Data. [indicate subset used]. NOAA National Centers for Environmental Information. https://doi.org/10.25921/95ba-jz28. Accessed [date].
- Please refer to Credit tab for full citation information.
- doi:10.25921/95ba-jz28
- noaa-ocean-21150
- NCEI DSI 1200_02
- NCEI DSI 1200_01
noaa-ocean-21150
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Distributor | NOAA National Centers for Environmental Information
ncei.info@noaa.gov |
Dataset Point of Contact | NOAA National Centers for Environmental Information
ncei.info@noaa.gov |
Dataset Point of Contact | Data Center Contact
NOAA World Data Service for Paleoclimatology 828-271-4800 paleo@noaa.gov |
Coverage Description | Date Range: 6002000 cal yr BP to 2786000 cal yr BP; |
Time Period | -6000050 to -2784050 |
Spatial Bounding Box Coordinates |
N: 56.042667
S: -30.2833
E: -23.231333
W: -35.2833
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Spatial Coverage Map |
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Data Presentation Form | Digital table - digital representation of facts or figures systematically displayed, especially in columns
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Dataset Progress Status | Complete - production of the data has been completed |
Data Update Frequency | Data update frequency not available |
Supplemental Information |
STUDY NOTES: Combined planktonic foraminiferal Mg/Ca and d18O data, benthic d18O data and foraminiferal test weights from Deep Sea Drilling Project (DSDP) sites 516A and 552A (South and North Atlantic Oceans).
ABSTRACT SUPPLIED BY ORIGINATOR: Tectonically induced changes in oceanic seaways had profound effects on global and regional climate during the Late Neogene. The constriction of the Central American Seaway reached a critical threshold during the early Pliocene ~4.8-4 million years (Ma) ago. Model simulations indicate the strengthening of the Atlantic Meridional Overturning Circulation (AMOC) with a signature warming response in the Northern Hemisphere and cooling in the Southern Hemisphere. Subsequently, between ~4-3 Ma, the constriction of the Indonesian Seaway impacted regional climate and might have accelerated the Northern Hemisphere Glaciation. We here present Pliocene Atlantic interhemispheric sea surface temperature and salinity gradients (deduced from foraminiferal Mg/Ca and stable oxygen isotopes, d18O) in combination with a recently published benthic stable carbon isotope (d13C) record from the southernmost extent of North Atlantic Deep Water to reconstruct gateway-related changes in the AMOC mode. After an early reduction of the AMOC at ~5.3 Ma, we show in agreement with model simulations of the impacts of Central American Seaway closure a strengthened AMOC with a global climate signature. During ~3.8-3 Ma, we suggest a weakening of the AMOC in line with the global cooling trend, with possible contributions from the constriction of the Indonesian Seaway. |
Purpose | Records of past climate and ocean circulation derived from marine sediments. Parameter keywords describe what was measured in this dataset. Additional summary information can be found in the abstracts of papers listed in the dataset citations. |
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Theme keywords | Global Change Master Directory (GCMD) Science Keywords
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Data Center keywords | Global Change Master Directory (GCMD) Data Center Keywords
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Last Modified: 2024-04-27
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