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  • 1
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    Unbekannt
    PANGAEA
    In:  Supplement to: Sinninghe Damsté, Jaap S; Verschuren, Dirk; Ossebaar, Jort; Blokker, Jord; van Houten, Rianne; van der Meer, Marcel T J; Plessen, Birgit; Schouten, Stefan (2011): A 25,000-year record of climate-induced changes in lowland vegetation of eastern equatorial Africa revealed by the stable carbon-isotopic composition of fossil plant leaf waxes. Earth and Planetary Science Letters, 302(1-2), 236-246, https://doi.org/10.1016/j.epsl.2010.12.025
    Publikationsdatum: 2023-06-27
    Beschreibung: The debate of climate versus CO2 in controlling the long-term dynamics of tropical African vegetation has focused on events at the upper tree-line, since the relevant paleodata tend to be from mid-elevation sites (~2000-3000 m). Less well known is the relative importance of CO2 in regulating the dynamics of tropical lowland (〈1500 m) vegetation, particularly that of the dry open woodlands, bush- and grasslands covering much of eastern equatorial Africa. Here we examine the stable carbon isotopic composition of n-alkanes in the sediment record of Lake Challa, a lowland crater lake near Mt. Kilimanjaro, covering the last 25,000 years. The distributions of the n-alkanes, with dominance of the long-chain odd-carbon-numbered components, and their isotopic composition reveal a mixed origin. The C23 and C25 n-alkanes are depleted in 13C, with d13C values between-30 and-50 per mil. In shallow lakes these n-alkanes are thought to derive from non-emergent aquatic plants, but this is unlikely in this steep-sided crater lake as it lacks a significant littoral habitat. The C27+ n-alkanes are predominantly derived from leaf wax lipids of terrestrial plants, brought into the lake predominantly by local soil run-off. Their d13C values, in particular that of the n-C31 alkane, reveal a marked transition in local lowland vegetation from being dominated (~70-100%) by C4 plants during the glacial period until 16.5 cal kyr BP, to a more mixed C3/C4 composition (~30-60% C4) during the Holocene. The start of the late-glacial trend towards a greater proportion of C3 plants coincided with the start of increasing monsoon rainfall, ~1500 years after the onset of the rise in atmospheric CO2 and ~3500 years after the onset of post-glacial warming. The transition was interrupted during the dry Younger Dryas period (13.0-11.7 cal kyr BP), when C4 plants again became much more prevalent, almost reaching their glacial-period abundance. Notably, the principal trend in leaf-wax ?13C values infers C4 dominance during both wet and dry phases of the glacial period, and a mixed C3/C4 vegetation during both wet and dry phases of the Holocene. Our results indicate that long-term variation in pCO2 exerted important control on the composition of drought-adapted savanna vegetation in this currently semi-arid lowland region of equatorial East Africa.
    Schlagwort(e): Lake_Challa; Mount Kilimanjaro, Tanzania; NIOZ_UU; NIOZ Royal Netherlands Institute for Sea Research, and Utrecht University; PCUWI; Piston corer, UWITEC
    Materialart: Dataset
    Format: application/zip, 2 datasets
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 2
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    Unbekannt
    PANGAEA
    In:  Supplement to: Sinninghe Damsté, Jaap S; Ossebaar, Jort; Schouten, Stefan; Verschuren, Dirk (2012): Distribution of tetraether lipids in the 25-ka sedimentary record of Lake Challa: extracting reliable TEX86 and MBT/CBT palaeotemperatures from an equatorial African lake. Quaternary Science Reviews, 50, 43-54, https://doi.org/10.1016/j.quascirev.2012.07.001
    Publikationsdatum: 2023-06-27
    Beschreibung: The distribution of isoprenoid and branched glycerol dialkyl glycerol tetraether (GDGT) lipids was studied in the sedimentary record of Lake Challa, a permanently stratified, partly anoxic crater lake on the southeastern slope of Mt. Kilimanjaro (Kenya/Tanzania), to examine if the GDGTs could be used to reconstruct past variation in regional temperature. The study material comprised 230 samples from a continuous sediment sequence spanning the last 25 ka with excellent age control based on high-resolution AMS 14C dating. The distribution of GDGTs showed large variation through time. In some time intervals (i.e., from 20.4 to 15.9 ka BP and during the Younger Dryas, 12.9?11.7 ka BP) crenarchaeol was the most abundant GDGT, whereas at other times (i.e., during the Early Holocene) branched GDGTs and GDGT-0 were the major GDGT constituents. In some intervals of the sequence the relative abundance of GDGT-0 and GDGT-2 was too high to be derived exclusively from lacustrine Thaumarchaeota, suggesting a sizable contribution from methanogens and other archaea. This severely complicated application of TEX86 palaeothermometry in this lake, and limited reliable reconstruction of lake water temperature to the time interval 25-13 ka BP, i.e. the Last Glacial Maximum and the period of post-glacial warming. The TEX86-inferred timing of this warming is similar to that recorded previously in two of the large African rift lakes, while its magnitude is slightly or much higher than that recorded at these other sites, depending on which lake-based TEX86 calibration is used. Application of calibration models based on distributions of branched GDGTs developed for lakes inferred temperatures of 15-18 °C for the Last Glacial Maximum and 19-22 °C for the Holocene. However, the MBT/CBT palaeothermometer reconstructs temperatures as low as 12 °C for a Lateglacial period centred on 15 ka BP. Variation in down-core values of the BIT index are mainly determined by the varying production rate of crenarchaeol relative to in-situ produced branched GDGTs. The apparent relationship of the BIT index with climatic moisture balance can be explained either by the direct influence of lake level and wind strength on nutrient recycling, or by influx of soil nutrients promoting aquatic productivity and nitrification. This study shows that GDGTs can aid in obtaining climatic information from lake records but that the obtained data should be interpreted with care.
    Schlagwort(e): Lake_Challa; Mount Kilimanjaro, Tanzania; NIOZ_UU; NIOZ Royal Netherlands Institute for Sea Research, and Utrecht University; PCUWI; Piston corer, UWITEC
    Materialart: Dataset
    Format: application/zip, 3 datasets
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 3
    Publikationsdatum: 2023-06-27
    Schlagwort(e): AGE; Branched and isoprenoid tetraether index; Branched glycerol dialkyl glycerol tetraether; Crenarchaeol regio-isomer; Cyclization ratio of branched tetraethers; DEPTH, sediment/rock; Lake_Challa; Methylation index of branched tetraethers; Mount Kilimanjaro, Tanzania; NIOZ_UU; NIOZ Royal Netherlands Institute for Sea Research, and Utrecht University; PCUWI; pH; Piston corer, UWITEC; Sample code/label; Temperature, air, annual mean
    Materialart: Dataset
    Format: text/tab-separated-values, 4574 data points
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 4
    Publikationsdatum: 2023-06-27
    Schlagwort(e): AGE; Branched and isoprenoid tetraether index; Dicyclic glycerol dialkyl glycerol tetraether; Lake_Challa; Mount Kilimanjaro, Tanzania; NIOZ_UU; NIOZ Royal Netherlands Institute for Sea Research, and Utrecht University; PCUWI; Piston corer, UWITEC; Ratio; Tetraether index of 86 carbon atoms
    Materialart: Dataset
    Format: text/tab-separated-values, 248 data points
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 5
    Publikationsdatum: 2023-06-27
    Schlagwort(e): Acyclic glycerol dialkyl glycerol tetraether; AGE; Branched and isoprenoid tetraether index; Branched glycerol dialkyl glycerol tetraether; Crenarchaeol; DEPTH, sediment/rock; Lake_Challa; Mount Kilimanjaro, Tanzania; NIOZ_UU; NIOZ Royal Netherlands Institute for Sea Research, and Utrecht University; PCUWI; Piston corer, UWITEC; Sample code/label
    Materialart: Dataset
    Format: text/tab-separated-values, 1116 data points
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 6
    Publikationsdatum: 2023-06-27
    Schlagwort(e): AGE; Average chain length; Carbon Preference Index; DEPTH, sediment/rock; Lake_Challa; Mount Kilimanjaro, Tanzania; n-Alkane C23, δ13C; n-Alkane C23, δ13C, standard deviation; n-Alkane C25, δ13C; n-Alkane C25, δ13C, standard deviation; n-Alkane C27, δ13C; n-Alkane C27, δ13C, standard deviation; n-Alkane C29, δ13C; n-Alkane C29, δ13C, standard deviation; n-Alkane C31, δ13C; n-Alkane C31, δ13C, standard deviation; n-Alkane C33, δ13C; n-Alkane C33, δ13C, standard deviation; NIOZ_UU; NIOZ Royal Netherlands Institute for Sea Research, and Utrecht University; PCUWI; Piston corer, UWITEC; Ratio
    Materialart: Dataset
    Format: text/tab-separated-values, 802 data points
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 7
    Publikationsdatum: 2023-06-27
    Schlagwort(e): AGE; Lake_Challa; Mount Kilimanjaro, Tanzania; NIOZ_UU; NIOZ Royal Netherlands Institute for Sea Research, and Utrecht University; PCUWI; Piston corer, UWITEC; δ13C, organic carbon
    Materialart: Dataset
    Format: text/tab-separated-values, 204 data points
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 8
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    Unbekannt
    PANGAEA
    In:  Supplement to: Schouten, Stefan; Ossebaar, Jort; Schreiber, Karolin; Kienhuis, Michiel V M; Langer, Gerald; Benthien, Albert; Bijma, Jelle (2006): The effect of temperature, salinity and growth rate on the stable hydrogen isotopic composition of long chain alkenones produced by Emiliania huxleyi and Gephyrocapsa oceanica. Biogeosciences, 3(1), 113-119, https://doi.org/10.5194/bg-3-113-2006
    Publikationsdatum: 2023-12-22
    Beschreibung: Two haptophyte algae, Emiliania huxleyi and Gephyrocapsa oceanica, were cultured at different temperatures and salinities to investigate the impact of these factors on the hydrogen isotopic composition of long chain alkenones synthesized by these algae. Results showed that alkenones synthesized by G. oceanica were on average depleted in D by 30 compared to those of E. huxleyi when grown under similar temperature and salinity conditions. The fractionation factor, alpha alkenones-H2O, ranged from 0.760 to 0.815 for E. huxleyi and from 0.741 to 0.788 for G. oceanica. There was no significant correlation of alpha alkenones-H2O with temperature but a positive linear correlation was observed between alpha alkenones-H2O and salinity with ~3 change in fractionation per salinity unit and a negative correlation between alpha alkenones-H2O and growth rate. This suggests that both salinity and growth rate can have a substantial impact on the stable hydrogen isotopic composition of long chain alkenones in natural environments.
    Schlagwort(e): Alkenone, unsaturation index UK'37; Fractionation factor; Growth rate; Salinity; Species; Strain; Temperature, water; δ Deuterium, alkenone, C37; δ Deuterium, alkenone, C38; δ Deuterium, standard deviation; δ Deuterium, water
    Materialart: Dataset
    Format: text/tab-separated-values, 247 data points
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 9
    Publikationsdatum: 2014-06-25
    Beschreibung: wo 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.
    Repository-Name: EPIC Alfred Wegener Institut
    Materialart: Article , isiRev
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 10
    Publikationsdatum: 2022-05-26
    Beschreibung: 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.
    Beschreibung: 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.
    Beschreibung: 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.
    Beschreibung: 2014-06-20
    Schlagwort(e): TEX86 ; BIT ; GDGT ; Round robin
    Repository-Name: Woods Hole Open Access Server
    Materialart: Article
    Format: text/plain
    Format: application/msword
    Format: application/pdf
    Standort Signatur Einschränkungen Verfügbarkeit
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