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  • 11139-8bx; 12174-15; AEOLD; Aeolian dust sample; ANT-IV/1c; Atlantic Ocean; BC; BCR; BOFS23/7M; BOFS23#7; BOFS29/2M; BOFS29#2; Box corer; Box corer (Reineck); CD53; Cervaro river; Charles Darwin; D11798#2; D11800#5; D11804#4; D11815#5; D11939#3; D11944#5; D11948#1; D11954#4; D177; D187; DC2; DC23; DI135; DI194; Discovery (1962); Discovery II (1929); East Atlantic; eastern Romanche Fracture Zone; Equatorial Atlantic; FGGE-Equator 79 - First GARP Global Experiment; GEOTROPEX 83, NOAMP I; Giant box corer; GIK12309-2; GIK12326-4; GIK12329-5; GIK12330-1; GIK12344-5; GIK13289-1; GIK13557-1; GIK16004-1; GIK16006-1; GIK16030-1; GIK16405-1; GIK16408-2; GIK16458-2; GIK16757-1; GIK16768-1; GIK16770-1; GIK16772-1; GIK16773-1; GIK16775-2; GIK16778-2; GIK16782-1; GIK16785-1; GIK16789-1; GIK16830-1; GIK16857-2; GIK16866-1; GIK16867-1; GIK16869-1; GIK16873-1; GKG; Gravity corer (Kiel type); Guadiana Estuary; KAL; Kasten corer; KOL; M19; M20; M21; M25; M51; M6/5; M60; M65; Meteor (1964); Meteor (1986); MUC; MultiCorer; Northeast Atlantic; off Cote d Ivoire; off Gabun; off Ghana; off Guinea; off Liberia; off Nigeria-Delta; Piston corer (Kiel type); Polarstern; PS08; Sierra Leone Basin/Guinea Basin; SL; SUBTROPEX 82; TAF69; TAF70; TAF9; VA-10/3; Valdivia (1961); van Veen Grab; VGRAB  (1)
  • GDGT
Collection
Keywords
Years
  • 1
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Huang, Yongsong; Dupont, Lydie M; Sarnthein, Michael; Hayes, John M; Eglinton, Geoffrey (2000): Mapping of C4 plant input from North West Africa into North East Atlantic sediments. Geochimica et Cosmochimica Acta, 64(20), 3505-3513, https://doi.org/10.1016/S0016-7037(00)00445-2
    Publication Date: 2024-02-02
    Description: Mapping the abundance of 13C in leaf-wax components in surface sediments recovered from the seafloor off northwest Africa (0–35°N) reveals a clear pattern of delta13C distribution, indicating systematic changes in the proportions of terrestrial C3 and C4 plant input. At 20°N latitude, we find that isotopically enriched products characteristic of C4 plants account for more than 50% of the terrigenous inputs. This signal extends westward beneath the path of the dust-laden Sahara Air Layer (SAL). High C4 contributions, apparently carried by January trade winds, also extend far into the Gulf of Guinea. Similar distributions are obtained if summed pollen counts for the Chenopodiaceae-Amaranthaceae and the Poaceae are used as an independent C4 proxy. We conclude that the specificity of the latitudinal distribution of vegetation in North West Africa and the pathways of the wind systems (trade winds and SAL) are responsible for the observed isotopic patterns observed in the surface sediments. Molecular-isotopic maps on the marine-sedimentary time horizons (e.g., during the last glacial maximum) are thus a robust tool for assessing the phytogeographic changes on the tropical and sub-tropical continents, which have important implications for the changes in climatic and atmospheric conditions.
    Keywords: 11139-8bx; 12174-15; AEOLD; Aeolian dust sample; ANT-IV/1c; Atlantic Ocean; BC; BCR; BOFS23/7M; BOFS23#7; BOFS29/2M; BOFS29#2; Box corer; Box corer (Reineck); CD53; Cervaro river; Charles Darwin; D11798#2; D11800#5; D11804#4; D11815#5; D11939#3; D11944#5; D11948#1; D11954#4; D177; D187; DC2; DC23; DI135; DI194; Discovery (1962); Discovery II (1929); East Atlantic; eastern Romanche Fracture Zone; Equatorial Atlantic; FGGE-Equator 79 - First GARP Global Experiment; GEOTROPEX 83, NOAMP I; Giant box corer; GIK12309-2; GIK12326-4; GIK12329-5; GIK12330-1; GIK12344-5; GIK13289-1; GIK13557-1; GIK16004-1; GIK16006-1; GIK16030-1; GIK16405-1; GIK16408-2; GIK16458-2; GIK16757-1; GIK16768-1; GIK16770-1; GIK16772-1; GIK16773-1; GIK16775-2; GIK16778-2; GIK16782-1; GIK16785-1; GIK16789-1; GIK16830-1; GIK16857-2; GIK16866-1; GIK16867-1; GIK16869-1; GIK16873-1; GKG; Gravity corer (Kiel type); Guadiana Estuary; KAL; Kasten corer; KOL; M19; M20; M21; M25; M51; M6/5; M60; M65; Meteor (1964); Meteor (1986); MUC; MultiCorer; Northeast Atlantic; off Cote d Ivoire; off Gabun; off Ghana; off Guinea; off Liberia; off Nigeria-Delta; Piston corer (Kiel type); Polarstern; PS08; Sierra Leone Basin/Guinea Basin; SL; SUBTROPEX 82; TAF69; TAF70; TAF9; VA-10/3; Valdivia (1961); van Veen Grab; VGRAB
    Type: Dataset
    Format: application/zip, 2 datasets
    Location Call Number Expected Availability
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  • 2
    Publication Date: 2022-05-26
    Description: Author Posting. © American Geophysical Union, 2013. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Geochemistry, Geophysics, Geosystems 14 (2013): 5263–5285, doi:10.1002/2013GC004904.
    Description: Two commonly used proxies based on the distribution of glycerol dialkyl glycerol tetraethers (GDGTs) are the TEX86 (TetraEther indeX of 86 carbon atoms) paleothermometer for sea surface temperature reconstructions and the BIT (Branched Isoprenoid Tetraether) index for reconstructing soil organic matter input to the ocean. An initial round-robin study of two sediment extracts, in which 15 laboratories participated, showed relatively consistent TEX86 values (reproducibility ±3–4°C when translated to temperature) but a large spread in BIT measurements (reproducibility ±0.41 on a scale of 0–1). Here we report results of a second round-robin study with 35 laboratories in which three sediments, one sediment extract, and two mixtures of pure, isolated GDGTs were analyzed. The results for TEX86 and BIT index showed improvement compared to the previous round-robin study. The reproducibility, indicating interlaboratory variation, of TEX86 values ranged from 1.3 to 3.0°C when translated to temperature. These results are similar to those of other temperature proxies used in paleoceanography. Comparison of the results obtained from one of the three sediments showed that TEX86 and BIT indices are not significantly affected by interlaboratory differences in sediment extraction techniques. BIT values of the sediments and extracts were at the extremes of the index with values close to 0 or 1, and showed good reproducibility (ranging from 0.013 to 0.042). However, the measured BIT values for the two GDGT mixtures, with known molar ratios of crenarchaeol and branched GDGTs, had intermediate BIT values and showed poor reproducibility and a large overestimation of the “true” (i.e., molar-based) BIT index. The latter is likely due to, among other factors, the higher mass spectrometric response of branched GDGTs compared to crenarchaeol, which also varies among mass spectrometers. Correction for this different mass spectrometric response showed a considerable improvement in the reproducibility of BIT index measurements among laboratories, as well as a substantially improved estimation of molar-based BIT values. This suggests that standard mixtures should be used in order to obtain consistent, and molar-based, BIT values.
    Description: S.S. thanks the Netherlands Organisation for Scientific Research (NWO) for financial support through a VICI grant and Jaap van der Meer for advice and support on the statistical analysis. A.P. thanks Susan Carter for laboratory assistance and NSF-OCE for funding. A.R.M. thanks Jordi Coello and N uria Moraleda for advice and support on the statistical analysis and Spanish Ministry for research and innovation (MICIIN) for funding. V.G. thanks Xavier Philippon and Carl Johnson for technical assistance. K.G. and M.W. thank the Australian Research Council and John de Laeter Centre for funding toward the LC-MS system, and ARC Fellowship awarded to K.G. C.L.Z. thanks the State Key Laboratory of Marine Geology and the Chinese ‘‘National Thousand Talents’’ program for supporting the LC-MS work performed at Tongji University.
    Description: 2014-06-20
    Keywords: TEX86 ; BIT ; GDGT ; Round robin
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Format: text/plain
    Format: application/msword
    Format: application/pdf
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