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  • Forschungsdaten  (132)
  • 2015-2019  (132)
Publikationsart
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Erscheinungszeitraum
Jahr
  • 1
    facet.materialart.
    Unbekannt
    PANGAEA
    In:  Supplement to: Baxter, Allix J; Hopmans, Ellen C; Russell, James M; Sinninghe Damsté, Jaap S (2019): Bacterial GMGTs in East African lake sediments: Their potential as palaeotemperature indicators. Geochimica et Cosmochimica Acta, 259, 155-169, https://doi.org/10.1016/j.gca.2019.05.039
    Publikationsdatum: 2023-03-14
    Beschreibung: Glycerol monoalkyl glycerol tetraethers (GMGTs) are a group of membrane spanning lipids produced by some species of archaea and bacteria. They differ from the more commonly studied glycerol dialkyl glycerol tetraethers (GDGTs) in having an additional covalent carbon-carbon bond connecting the two alkyl chain. The relative abundance and distribution of bacterial branched GMGTs (brGMGTs) in surface sediments from a set of East African lakes were studied. The abundance of brGMGTs relative to the brGDGTs is positively correlated to measured mean annual air temperature (MAAT), although with a significant amount of scatter. BrGMGT abundance was not correlated to lake water pH. Seven major brGMGTs that vary in degree of methylation were identified, with m/z 1020, 1034 and 1048. Further, the mass chromatograms of the m/z 1020 and 1034 brGMGTs show an interesting distribution of peaks, which likely relates to the occurrence of distinct brGMGT isomers. This structural complexity is higher than previously observed in peats and marine sediments. Principal component analysis of the fractional abundance of bacterial tetraether lipids revealed the brGMGTs behave similarly to one another but differently from both the 5- or 6-methyl brGDGTs. This suggests the brGMGTs are produced by a common source organism and are methylated at a different position. The distribution of the seven brGMGTs showed considerable correlation with MAAT. This variability was captured in a new proxy index (the brGMGTI), which showed a strong positive linear relationship with MAAT. Lacustrine brGMGTs show potential to be applied to ancient settings to provide information about paleoclimate.
    Schlagwort(e): Albert_Lake; Bandara_Lake; Batoda_Lake; Bigata_Lake; Branched glycerol dialkyl glycerol tetraether, Ia; Branched glycerol dialkyl glycerol tetraether, Ia (peak area); Branched glycerol dialkyl glycerol tetraether, Ib; Branched glycerol dialkyl glycerol tetraether, Ib (peak area); Branched glycerol dialkyl glycerol tetraether, Ic; Branched glycerol dialkyl glycerol tetraether, Ic (peak area); Branched glycerol dialkyl glycerol tetraether, IIa; Branched glycerol dialkyl glycerol tetraether, IIa'; Branched glycerol dialkyl glycerol tetraether, IIa' (peak area); Branched glycerol dialkyl glycerol tetraether, IIa (peak area); Branched glycerol dialkyl glycerol tetraether, IIb; Branched glycerol dialkyl glycerol tetraether, IIb'; Branched glycerol dialkyl glycerol tetraether, IIb' (peak area); Branched glycerol dialkyl glycerol tetraether, IIb (peak area); Branched glycerol dialkyl glycerol tetraether, IIIa; Branched glycerol dialkyl glycerol tetraether, IIIa'; Branched glycerol dialkyl glycerol tetraether, IIIa' (peak area); Branched glycerol dialkyl glycerol tetraether, IIIa (peak area); Branched glycerol monoalkyl glycerol tetraethers, H1020a; Branched glycerol monoalkyl glycerol tetraethers, H1020a (peak area); Branched glycerol monoalkyl glycerol tetraethers, H1020b; Branched glycerol monoalkyl glycerol tetraethers, H1020b (peak area); Branched glycerol monoalkyl glycerol tetraethers, H1020c; Branched glycerol monoalkyl glycerol tetraethers, H1020c (peak area); Branched glycerol monoalkyl glycerol tetraethers, H1034a; Branched glycerol monoalkyl glycerol tetraethers, H1034a (peak area); Branched glycerol monoalkyl glycerol tetraethers, H1034b; Branched glycerol monoalkyl glycerol tetraethers, H1034b (peak area); Branched glycerol monoalkyl glycerol tetraethers, H1034c; Branched glycerol monoalkyl glycerol tetraethers, H1034c (peak area); Branched glycerol monoalkyl glycerol tetraethers, H1048; Branched glycerol monoalkyl glycerol tetraethers, H1048 (peak area); Bugwagi_Lake; Bukurungu_East_Lake; Central_Lake; Chibwera_Lake; Country; Crane_Lake; DEPTH, water; Dimtu_Lake; Edward_Lake; Elevation of event; Enchanted_Lake__Lake; Event label; Gallery_Tarn_Lake; Garba_Gurach_Lake; GDGTs; GMGT; Hanging_Tarn_Lake; Hara_Laki_Lake; Hara_Lucas_Lake; Haro_Lakota_Lake; Harris_Tarn_Lake; Hausburg_Tarn_Lake; H-GDGT; Hut_Tarn_Lake; Ibamba_Lake; Kacuba_Lake; Kako_Lake; Kamweru_Lake; Kanyabutetere_Lake; Kanyanchu_Lake; Kasirya_Lake; Katanda_Lake; Katunda_Lake; Kifuruka_Lake; Kisibendi_Lake; Kitere_Lake; Kopello_Lake; Koromi_Lake; Kuware_Lake; Kyasunduka_Lake; Kyerbwato_Lake; Kyogo_Lake; Lake; Lake_Ellis; lakes; Lake surface area; Large_Hall_Tarn_Lake; Latitude of event; Longitude of event; Lower_Kachope_Lake; Lower_Simba_Lake; Mahoma_Lake; Mahuhura_Lake; Mbayo_Lake; membrane lipids; Middle_Kachope_Lake; Mirambi_Lake; MULT; Multiple investigations; Murabio_Lake; Murusi_Lake; Mwengenyi_Lake; Nanyuki_Tarn_Lake; NIOZ_UU; NIOZ Royal Netherlands Institute for Sea Research, and Utrecht University; Njarayabana_Lake; Nkuruba_Lake; Nyamugosani_Lake; Nyamusingere_Lake; Nyantonde_Lake; Oblong_Tarn_Lake; palaeotemperature; pH; Ruhandika_Lake; Rutundu_Lake; sediments; Small_Hall_Tarn_Lake; Square_Tarn_Lake; Sum; Tanganyika_Lake; Teleki_Tarn_Lake; Temperature, air, annual mean; Temperature, water; tetraethers; Thompson_Lake_Lake; Togona_Lake; Veggi_Tarn_Lake; Wandakara_Lake; Wankenzi_Lake
    Materialart: Dataset
    Format: text/tab-separated-values, 2991 data points
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 2
    Publikationsdatum: 2023-03-24
    Schlagwort(e): AWIPEV; AWIPEV_based; Branched and isoprenoid tetraether index; Branched glycerol dialkyl glycerol tetraether; Branched glycerol dialkyl glycerol tetraether, Ia; Branched glycerol dialkyl glycerol tetraether, Ib; Branched glycerol dialkyl glycerol tetraether, Ic; Branched glycerol dialkyl glycerol tetraether, IIa; Branched glycerol dialkyl glycerol tetraether, IIb; Branched glycerol dialkyl glycerol tetraether, IIc; Branched glycerol dialkyl glycerol tetraether, IIIa; Branched glycerol dialkyl glycerol tetraether, IIIb; Branched glycerol dialkyl glycerol tetraether, IIIc; Cyclization ratio of branched tetraethers; DEPTH, soil; Event label; Lilliehookbreen-1; Methylation index of branched tetraethers; Mitra-Peninsula-1; Mitra-Peninsula-2; Mitra-Peninsula-3; Mitra-Peninsula-4; Mitra-Peninsula-5; Mitra-Peninsula-6; MULT; Multiple investigations; NIOZ_UU; NIOZ Royal Netherlands Institute for Sea Research, and Utrecht University; Ny-Alesund-1; Ny-Alesund-2; Spitsbergen; Temperature, annual mean
    Materialart: Dataset
    Format: text/tab-separated-values, 110 data points
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 3
    Publikationsdatum: 2023-03-24
    Schlagwort(e): AWIPEV; AWIPEV_based; Carbon, organic, total; DEPTH, soil; Event label; Latitude of event; Lilliehookbreen-1; Lilliehookbreen-2; Lithology/composition/facies; Longitude of event; Mitra-Peninsula-1; Mitra-Peninsula-2; Mitra-Peninsula-3; Mitra-Peninsula-4; Mitra-Peninsula-5; Mitra-Peninsula-6; MULT; Multiple investigations; NIOZ_UU; NIOZ Royal Netherlands Institute for Sea Research, and Utrecht University; Ny-Alesund-1; Ny-Alesund-2; Ny-Alesund-3; Ny-Alesund-4; pH; Spitsbergen
    Materialart: Dataset
    Format: text/tab-separated-values, 35 data points
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 4
    Publikationsdatum: 2023-03-10
    Schlagwort(e): 64PE395; 64PE395-13_AIR; 64PE395-14_AIR; 64PE395-15_AIR; 64PE395-16_AIR; 64PE395-17_AIR; 64PE395-18_AIR; 64PE395-19_AIR; 64PE395-20_AIR; 64PE395-21_AIR; 64PE395-22_AIR; 64PE395-23_AIR; 64PE395-24_AIR; 64PE395-25_AIR; 64PE395-26_AIR; ALTITUDE; Average chain length; Carbon Preference Index; DUC; Dust collector; DUSTTraffic III; Event label; Latitude of event; Longitude of event; n-Alcohol C27; n-Alcohol C28; n-Alcohol C29; n-Alcohol C30; n-Alcohol C31; n-Alcohol C32; n-Alkane C15; n-Alkane C16; n-Alkane C17; n-Alkane C18; n-Alkane C19; n-Alkane C20; n-Alkane C21; n-Alkane C22; n-Alkane C23; n-Alkane C24; n-Alkane C25; n-Alkane C26; n-Alkane C27; n-Alkane C28; n-Alkane C29; n-Alkane C30; n-Alkane C31; n-Alkane C32; n-Alkane C33; n-Alkane C34; n-fatty acid C27; n-fatty acid C28; n-fatty acid C29; n-fatty acid C30; n-fatty acid C31; n-fatty acid C32; NIOZ_UU; NIOZ Royal Netherlands Institute for Sea Research, and Utrecht University; Pelagia; Ratio; South Atlantic Ocean; sum n-Alcohols C28+C30+C32; Sum n-alkanes C25-C33; sum n-fatty acids C28+C30+C32; Volume
    Materialart: Dataset
    Format: text/tab-separated-values, 600 data points
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 5
    Publikationsdatum: 2023-03-10
    Schlagwort(e): 64PE393; 64PE393_10MUC; 64PE393_11MUC; 64PE393_12MUC; 64PE393_13MUC; 64PE393_14MUC; 64PE393_16MUC; 64PE393_17MUC; 64PE393_1MUC; 64PE393_20MUC; 64PE393_21MUC; 64PE393_22MUC; 64PE393_23MUC; 64PE393_3MUC; 64PE393_5MUC; 64PE393_7MUC; 64PE393_8MUC; 64PE393_9MUC; 64PE406; 64PE406_1MUC; 64PE406_2MUC; 64PE406_3MUC; 64PE406_5MUC; 64PE406_6MUC; 64PE407; 64PE407_10MUC; 64PE407_1MUC; 64PE407_2MUC; 64PE407_3MUC; 64PE407_4MUC; 64PE407_6MUC; 64PE407_7MUC; 64PE407_8MUC; 64PE407_9MUC; 64PE408; 64PE408_2MUC; 64PE410; 64PE410_10MUC; 64PE410_1MUC; 64PE410_2MUC; 64PE410_3MUC; 64PE410_4MUC; 64PE410_5MUC; 64PE410_6MUC; 64PE410_7MUC; 64PE410_9MUC; 64PE418; 64PE418_12MUC; 64PE418_4MUC; Alboran Sea; Alkenone, unsaturation index UK'37; Alkenone C37/C38 ratio; Area/locality; Baltic Sea; Black Sea; DEPTH, sediment/rock; Event label; HCC; Kattegat; Latitude of event; Longitude of event; Mediterranean Sea, Eastern Basin; Mediterranean Sea, Western Basin; MUC; MultiCorer; NESSC Black Sea; NESSC EAST MED; NESSC WEST MED; NIOZ_UU; NIOZ Baltic 2016; NIOZ Royal Netherlands Institute for Sea Research, and Utrecht University; Pelagia; Sea surface temperature, annual mean; Skagerrak; South Atlantic Ocean; Strait of Sicilia; Tropical North Atlantic
    Materialart: Dataset
    Format: text/tab-separated-values, 496 data points
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 6
    Publikationsdatum: 2023-03-10
    Schlagwort(e): 64PE406; 64PE406_1MUC; 64PE406_2MUC; 64PE406_3MUC; 64PE406_5MUC; 64PE406_6MUC; 64PE407; 64PE407_10MUC; 64PE407_1MUC; 64PE407_2MUC; 64PE407_3MUC; 64PE407_4MUC; 64PE407_6MUC; 64PE407_7MUC; 64PE407_8MUC; 64PE407_9MUC; Alboran Sea; Alkenone, unsaturation index UK'37; DEPTH, sediment/rock; Event label; Latitude of event; Longitude of event; Mediterranean Sea, Eastern Basin; Mediterranean Sea, Western Basin; MUC; MultiCorer; NESSC EAST MED; NESSC WEST MED; NIOZ_UU; NIOZ Royal Netherlands Institute for Sea Research, and Utrecht University; Pelagia; South Atlantic Ocean; Strait of Sicilia
    Materialart: Dataset
    Format: text/tab-separated-values, 72 data points
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 7
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    Unbekannt
    PANGAEA
    In:  Supplement to: Schreuder, Laura T; Hopmans, Ellen C; Castañeda, Isla S; Schefuß, Enno; Mulitza, Stefan; Sinninghe Damsté, Jaap S; Schouten, Stefan (2019): Late Quaternary biomass burning in Northwest Africa and interactions with climate, vegetation, and humans. Paleoceanography and Paleoclimatology, 34(2), 153-163, https://doi.org/10.1029/2018PA003467
    Publikationsdatum: 2023-03-03
    Beschreibung: Biomass burning on the African continent is widespread and interactions with climate, vegetation dynamics and biogeochemical cycling are complex. To obtain a better understanding of these complex relationships, African fire history has been widely studied, although mostly on relatively short time-scales (i.e. yrs to kyrs) and less commonly on long-term scales. Here, we present a 192-kyr, continuous biomass-burning record from sub-Saharan Northwest Africa based on the fire biomarker levoglucosan in a marine sediment core offshore Guinea. Notable features of our record include an increase in levoglucosan accumulation at 80 ka and two peaks at 50-60 ka. The event at 80 ka is likely related to an overall increase in sedimentation rates rather than an increase in biomass burning in the Northwest African savanna region. Our record indicates that glacial/interglacial changes in regional climate and vegetation composition (C3 vs. C4 plants) were not a major influence on biomass burning over the last 192 kyrs. However, we suggest that the burning events at 50-60 ka might be caused by increased occurrence of C3 vegetation and human settlement in this region. At this time, the savanna region became wetter and fuel loads likely increased. Therefore, the region was more hospitable for humans, who likely used fire for hunting activities. Collectively, we hypothesize that on longer (glacial/interglacial) timescales, biomass burning, regional climate and African vegetation are not necessarily coupled, while around 50-60 ka, higher fuel loads and human fire-use may have influenced fire occurrence in sub-Saharan Northwest Africa.
    Schlagwort(e): Carbon; Center for Marine Environmental Sciences; charcoal; fire history; indicators; levoglucosan; MARUM; Monsoon; NIOZ_UU; NIOZ Royal Netherlands Institute for Sea Research, and Utrecht University; organic aerosols; preservation; record; sediments
    Materialart: Dataset
    Format: application/zip, 2 datasets
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 8
    Publikationsdatum: 2023-03-11
    Schlagwort(e): 64PE406; 64PE406-E1; Bacteriohopanetetrol stereoisomer (peak area), per unit mass total organic carbon; Carbon, organic, total; Carbon, organic, total, standard deviation; DEPTH, sediment/rock; NESSC EAST MED; NIOZ_UU; NIOZ Royal Netherlands Institute for Sea Research, and Utrecht University; PC; Pelagia; Piston corer; see reference(s); δ13C; δ15N
    Materialart: Dataset
    Format: text/tab-separated-values, 150 data points
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 9
    Publikationsdatum: 2023-03-14
    Schlagwort(e): Ain_AW1; Ain, France, Europe; Carbon, organic, total; Date/Time of event; Delta du Rhone; DEPTH, sediment/rock; DEPTH, soil; DEPTH, water; Doubs_DW1; Doubs, France, Europe; Durance_Du2; Durance, France, Europe; Elevation of event; Event label; Isere_IW1; Isere, France, Europe; Latitude of event; Location of event; Longitude of event; Lower Rhone, France, Europe; MUC; MultiCorer; NIOZ_UU; NIOZ Royal Netherlands Institute for Sea Research, and Utrecht University; pH; Precipitation, annual mean; Rhone_delta_A; Rhone_delta_AK45; Rhone_delta_B; Rhone_delta_C; Rhone_delta_D; Rhone_delta_K; Rhone_delta_L; Rhone_delta_N; Rhone_RW1; Rhone_RW10; Rhone_RW11; Rhone_RW12; Rhone_RW13; Rhone_RW2; Rhone_RW3; Rhone_RW4; Rhone_RW5; Rhone_RW6; Rhone_RW7; Rhone_RW8; Rhone_RW9; RhoS-1; RhoS-10; RhoS-11; RhoS-12; RhoS-13; RhoS-14; RhoS-15-1; RhoS-15-2; RhoS-16; RhoS-17; RhoS-18; RhoS-2; RhoS-20; RhoS-21; RhoS-22-1; RhoS-22-2; RhoS-23; RhoS-24; RhoS-25; RhoS-26; RhoS-27; RhoS-28; RhoS-29-2; RhoS-3; RhoS-30; RhoS-31; RhoS-32; RhoS-33; RhoS-34; RhoS-35; RhoS-36; RhoS-37; RhoS-38; RhoS-39-1; RhoS-4; RhoS-40; RhoS-41; RhoS-42; RhoS-44; RhoS-45; RhoS-46; RhoS-47; RhoS-48; RhoS-49; RhoS-5; RhoS-50; RhoS-6; RhoS-7; RhoS-8; RhoS-9; RHS12-10; RHS12-11; RHS12-12; RHS12-13; RHS12-14; RHS12-15; RHS12-16; RHS12-17; RHS12-18; RHS12-19; RHS12-2; RHS12-20; RHS12-21; RHS12-23-b; RHS12-3; RHS12-5; RHS12-6; RHS12-7; RHS12-8; RHS12-9; Saone_SW1; Saone_SW2; Saone_SW3; Saone_SW4; Saone, France, Europe; SOIL; Soil profile; Suspended particulate matter; Temperature, air, annual mean; Upper Rhone, France, Europe; Upper Rhone, Switzerland, Europe; Water sample; WS
    Materialart: Dataset
    Format: text/tab-separated-values, 372 data points
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 10
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    Unbekannt
    PANGAEA
    In:  Supplement to: Svensson, Elisabeth; Schouten, Stefan; Hopmans, Ellen C; Middelburg, Jack J; Sinninghe Damsté, Jaap S (2016): Factors Controlling the Stable Nitrogen Isotopic Composition (d15N) of Lipids in Marine Animals. PLoS ONE, 11(1), e0146321, https://doi.org/10.1371/journal.pone.0146321
    Publikationsdatum: 2023-03-22
    Beschreibung: Lipid extraction of biomass prior to stable isotope analysis is known to cause variable changes in the stable nitrogen isotopic composition (d15N) of residual biomass. However, the underlying factors causing these changes are not yet clear. Here we address this issue by comparing the d15N of bulk and residual biomass of several marine animal tissues (fish, crab, cockle, oyster, and polychaete), as well as the d15N of the extracted lipids. As observed previously, lipid extraction led to a variable offset in d15N of biomass (differences ranging from -2.3 to +1.8 per mil). Importantly, the total lipid extract (TLE) was highly depleted in 15N compared to bulk biomass, and also highly variable (differences ranging from -14 to +0.7 per mil). The TLE consisted mainly of phosphatidylcholines, a group of lipids with one nitrogen atom in the headgroup. To elucidate the cause for the 15N-depletion in the TLE, the d15N of amino acids was determined, including serine because it is one of the main sources of nitrogen to N-containing lipids. Serine d15N values differed by -7 to +2 per mil from bulk biomass d15N, and correlated well with the 15N depletion in TLEs. On average, serine was less depleted (-3 per mil) than the TLE (-7 per mil), possibly due to fractionation during biosynthesis of N-containing headgroups, or that other nitrogen-containing compounds, such as urea and choline, or recycled nitrogen contribute to the nitrogen isotopic composition of the TLE. The depletion in 15N of the TLE relative to biomass increased with the trophic level of the organisms.
    Schlagwort(e): Carbon/Nitrogen ratio; Dutch_WaddenSea; Lipids; North Sea, Wadden sea; Sample code/label; Sample material; Species; Tissues; δ15N; δ15N, standard deviation
    Materialart: Dataset
    Format: text/tab-separated-values, 1367 data points
    Standort Signatur Einschränkungen Verfügbarkeit
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