NOAA/WDS Paleoclimatology - De Rif, South Africa Holocene Hyrax Midden Stable Isotope Data
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title: NOAA/WDS Paleoclimatology - De Rif, South Africa Holocene Hyrax Midden Stable Isotope Data
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date: 2019-08-19
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Anchor: DOI doi:10.25921/emnw-ch67
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individualName: Chase, B.M.
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abstract: 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 Other Collections. The data include parameters of others with a geographic location of South Africa, Southern Africa. The time period coverage is from 11385 to 42 in calendar years before present (BP). See metadata information for parameter and study location details. Please cite this study when using the data.
purpose: Data of past climate and environment derived from unusual proxy evidence. Parameter keywords describe what was measured in this data set. Additional summary information can be found in the abstracts of papers listed in the data set citations.
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keyword: Earth Science > Climate Indicators > Paleoclimate Indicators > Paleoclimate Reconstructions
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keyword: Continent > Africa > Southern Africa > South Africa > De Rif > LATITUDE -32.446 > LONGITUDE 19.221
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otherConstraints: Cite as: Chase, B.M.; Boom, A.; Carr, A.S.; Reimer, P.J. (2019-08-19): NOAA/WDS Paleoclimatology - De Rif, South Africa Holocene Hyrax Midden Stable Isotope Data. [indicate subset used]. NOAA National Centers for Environmental Information. https://doi.org/10.25921/emnw-ch67. Accessed [date].
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otherConstraints: Distribution liability: NOAA and NCEI make no warranty, expressed or implied, regarding these data, nor does the fact of distribution constitute such a warranty. NOAA and NCEI cannot assume liability for any damages caused by any errors or omissions in these data. If appropriate, NCEI can only certify that the data it distributes are an authentic copy of the records that were accepted for inclusion in the NCEI archives.
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otherConstraints: Please cite original publication, online resource, dataset and publication DOIs (where available), and date accessed when using downloaded data. If there is no publication information, please cite investigator, title, online resource, and date accessed. The appearance of external links associated with a dataset does not constitute endorsement by the Department of Commerce/National Oceanic and Atmospheric Administration of external Web sites or the information, products or services contained therein. For other than authorized activities, the Department of Commerce/NOAA does not exercise any editorial control over the information you may find at these locations. These links are provided consistent with the stated purpose of this Department of Commerce/NOAA Web site.
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title: Evolving Southern Hemisphere response to abrupt deglacial North Atlantic climate change events
date: (CI_Date)
date: 2015
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individualName: Brian M. Chase, Arnoud Boom, Andrew S. Carr, Matthieu Carré, Manuel Chevalier, Michael E. Meadows, Joel B. Pedro, J. Curt Stager, Paula J. Reimer
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description: Brian M. Chase, Arnoud Boom, Andrew S. Carr, Matthieu Carré, Manuel Chevalier, Michael E. Meadows, Joel B. Pedro, J. Curt Stager, Paula J. Reimer, 2015: Evolving Southern Hemisphere response to abrupt deglacial North Atlantic climate change events. Quaternary Science Reviews, 121, 132-136, 10.1016/j.quascirev.2015.05.023
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description: Date Range: 11385 cal yr BP to 42 cal yr BP;
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westBoundLongitude: 19.221
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southBoundLatitude: -32.446
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supplementalInformation: STUDY NOTES: Please contact principle investigator Brian Chase to obtain these data. Stable nitrogen (d15N) and carbon (d13C) isotope data obtained from the De Rif rock hyrax (Procavia capensis) midden in the Cederberg Mountains of South Africa's Western Cape. d15N is interpreted as a proxy for aridity, with higher values reflecting an enrichment of 15N in soils under drier conditions ABSTRACT SUPPLIED BY ORIGINATOR: Climate change during the last deglaciation was strongly influenced by the 'bipolar seesaw', producing antiphase climate responses between the North and South Atlantic. However, mounting evidence demands refinements of this model, with the occurrence of abrupt events in southern low to mid latitudes occurring in-phase with North Atlantic climate. Improved constraints on the north-south phasing and spatial extent of these events are therefore critical to understanding the mechanisms that propagate abrupt events within the climate system. We present a 19,400 year multi-proxy record of climate change obtained from a rock hyrax midden in southernmost Africa. Arid anomalies in phase with the Younger Dryas and 8.2 ka events are apparent, indicating a clear shift in the influence of the bipolar seesaw, which diminished as the Earth warmed, and was succeeded after ~14.6 ka by the emergence of a dominant interhemispheric atmospheric teleconnection.
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