NOAA/WDS Paleoclimatology - Norwegian Sea Foraminiferal Amino Acid Racemisation 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 Other Collections. The data include parameters of others with a geographic location of Norwegian Sea, North Atlantic Ocean. The time period coverage is from 160000 to 0 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: Wheeler, L.J.; Penkman, K.E.H.; Sejrup, H.P. (2020-11-19): NOAA/WDS Paleoclimatology - Norwegian Sea Foraminiferal Amino Acid Racemisation Data. [indicate subset used]. NOAA National Centers for Environmental Information. https://doi.org/10.25921/ge27-6959. Accessed [date].
- Please refer to Credit tab for full citation information.
- doi:10.25921/ge27-6959
- noaa-other-31836
- NCEI DSI 1200_02
- NCEI DSI 1200_01
noaa-other-31836
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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: 160000 cal yr BP to 0 cal yr BP; |
Time Period | -158050 to 1950 |
Spatial Bounding Box Coordinates |
N: 64.65
S: 64.65
E: 4.2
W: 4.2
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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: Amino acid racemization (AAR) data on Neogloboquadrina pachyderma (sinistral) from Norwegian Sea IMAGES core MD99-2288/2289
ABSTRACT SUPPLIED BY ORIGINATOR: While amino acid (AA) geochronology has been widely applied to foraminiferal biomineral proteins, there has been limited assessment of the potential of isolating an 'intra-crystalline' fraction of proteins to improve the reliability of AA geochronology for foraminifera. In this study, bleaching experiments were carried out on the foraminifer Neogloboquadrina pachyderma (sinistral) from an independently dated core from the south eastern Norwegian Sea spanning the last 120 ka. Results show that this species contains a bleach-resistant fraction of biomineral proteins, and that this intra-crystalline fraction may behave as a closed system. Racemisation in both the intra-crystalline and whole-protein fractions was found to systematically increase with time. Isoleucine epimerisation showed reliable trends with depth when analysed by ion exchange chromatography (IEC); analysis by reverse-phase liquid chromatography (RP-HPLC) resulted in reliable age-D/L relationships for aspartic acid, glutamic acid and alanine. Isolating the intra-crystalline fraction with a 48 h bleach treatment reduced the influence of contamination in younger material. Therefore, this paper recommends that the intra-crystalline approach is used when analysing Neogloboquadrina pachyderma (sinistral) for AA geochronology, especially for younger samples. Material-specific regression equations developed in this study successfully convert IEC A/I to RP-HPLC D/L values for aspartic acid, glutamic acid and alanine, enabling integration of geochronologies developed using different methods for this class of biomineral. |
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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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: 2022-02-22
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