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  • 1
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    PANGAEA
    In:  Supplement to: Tabares, Ximena; Zimmermann, Heike Hildegard; Dietze, Elisabeth; Ratzmann, Gregor; Belz, Lukas; Vieth-Hillebrand, Andrea; Dupont, Lydie M; Wilkes, Heinz; Mapani, Benjamin; Herzschuh, Ulrike (2019): Vegetation state changes in the course of shrub encroachment in an African savanna since about 1850 CE and their potential drivers. Ecology and Evolution, https://doi.org/10.1002/ece3.5955
    Publication Date: 2023-11-03
    Description: We present a multi-proxy record (fossil pollen, sedimentary ancient DNA, biomarkers, compound-specific carbon (δ13C) and deuterium (δD) isotopes, bulk carbon isotopes (δ13Corg), grain size, geochemical properties) from Lake Otjikoto, Namibia. Samples were extracted from sediment cores 15OJ10 and 15OJ06. These data document the compositional and environmental changes associated with shrub encroachment in semi-arid savanna environments.
    Keywords: AWI_Envi; Climate change; fossil pollen; land-use change; Polar Terrestrial Environmental Systems @ AWI; savanna ecology; sedimentary ancient DNA; state-and-transition; tree-grass interactions
    Type: Dataset
    Format: application/zip, 9 datasets
    Location Call Number Limitation Availability
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  • 2
    Publication Date: 2023-11-03
    Keywords: 15OJ06; Ancient DNA sequencing; AWI_Envi; Core; CORE; DEPTH, sediment/rock; Lake Otjikoto; Namibia; Number of sequences; Polar Terrestrial Environmental Systems @ AWI; Polymerase chain reaction (PCR); Replicates; Sample ID; savanna ecology; sedimentary ancient DNA; state-and-transition; tree-grass interactions
    Type: Dataset
    Format: text/tab-separated-values, 14774 data points
    Location Call Number Limitation Availability
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  • 3
    Publication Date: 2023-11-03
    Keywords: 15OJ10; Average chain length; AWI_Envi; Calculated; Carbon Preference Index; Climate change; Core; CORE; DEPTH, sediment/rock; fossil pollen; Gas chromatography; Lake Otjikoto; land-use change; n-Alkane C25, per unit mass total organic carbon; n-Alkane C27, per unit mass total organic carbon; n-Alkane C29, per unit mass total organic carbon; n-Alkane C31, per unit mass total organic carbon; n-Alkane C33, per unit mass total organic carbon; n-Alkane C35, per unit mass total organic carbon; n-Alkanol C24, per unit mass total organic carbon; n-Alkanol C26, per unit mass total organic carbon; n-Alkanol C28, per unit mass total organic carbon; n-Alkanol C30, per unit mass total organic carbon; n-Alkanol C32, per unit mass total organic carbon; n-Alkanol C34, per unit mass total organic carbon; Namibia; Polar Terrestrial Environmental Systems @ AWI; Sample ID; savanna ecology; sedimentary ancient DNA; state-and-transition; tree-grass interactions
    Type: Dataset
    Format: text/tab-separated-values, 450 data points
    Location Call Number Limitation Availability
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  • 4
    Publication Date: 2023-11-03
    Keywords: 15OJ10; AWI_Envi; Core; CORE; DEPTH, sediment/rock; End member; End Member Modelling Algorithm (EMMA); Grain size, LASER Particle Sizer; Lake Otjikoto; Namibia; Polar Terrestrial Environmental Systems @ AWI; Sample ID; Size fraction 〈 0.004 mm, clay; Size fraction 〉 2 mm, gravel; Size fraction 0.008-0.004 mm, 7.0-8.0 phi, fine silt; Size fraction 0.015-0.008 mm; Size fraction 0.030-0.015 mm; Size fraction 0.063-0.032 mm; Size fraction 0.125-0.063 mm, 3.0-4.0 phi, very fine sand; Size fraction 0.250-0.125 mm, 2.0-3.0 phi, fine sand; Size fraction 0.500-0.250 mm, 1.0-2.0 phi, medium sand; Size fraction 1.000-0.500 mm, 0.0-1.0 phi, coarse sand; Size fraction 2.000-1.000 mm, (-1.0)-0.0 phi, very coarse sand
    Type: Dataset
    Format: text/tab-separated-values, 527 data points
    Location Call Number Limitation Availability
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  • 5
    Publication Date: 2023-11-03
    Keywords: 15OJ10; AWI_Envi; Core; CORE; DEPTH, sediment/rock; Gas chromatography - Isotope ratio mass spectrometer (GC-IRMS); Lake Otjikoto; n-Alkane C17, δD; n-Alkane C19, δD; n-Alkane C27, δD; n-Alkane C29, δD; n-Alkane C31, δD; n-Alkane C33, δD; n-Alkane C35, δD; n-Alkanol C18, δD; n-Alkanol C28, δD; n-Alkanol C30, δD; n-Alkanol C32, δD; Namibia; Polar Terrestrial Environmental Systems @ AWI; Sample ID; Squalane, δD
    Type: Dataset
    Format: text/tab-separated-values, 215 data points
    Location Call Number Limitation Availability
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  • 6
    Publication Date: 2023-11-03
    Keywords: 15OJ10; AWI_Envi; Calculated; Carbon, inorganic, total; Carbon, organic, total; Carbon, organic/Nitrogen, total ratio; Core; CORE; DEPTH, sediment/rock; Element analyser CNS; Lake Otjikoto; Namibia; Nitrogen, total; Polar Terrestrial Environmental Systems @ AWI; Sample ID
    Type: Dataset
    Format: text/tab-separated-values, 150 data points
    Location Call Number Limitation Availability
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  • 7
    Publication Date: 2023-10-13
    Description: Additionally, we employed a local resident to collect surface water suspended sediment samples at river km 865 throughout the 2017-2018 water year. These samples were collected in a bucket, the sediment was allowed to settle, and then the water was decanted off the top. Recovered sediment was stored in sterile Whirlpak bags, and then dried in an oven at 40°C. We homogenized and disaggregated the dry sediment using a mortar and pestle, and removed coarse plant material 〉1 mm. For each sample, we weighed an aliquot of sediment and loaded the material into aluminum cells for lipid extraction. Total lipid extracts (TLE) were recovered using an accelerated solvent extraction system (Dionex ASE) with 9:1 v/v dichloromethane: methanol. We added exactly 10 µg of internal standard (5-a-Androstane) to the TLE for unknown compound quantification. We then separated the TLE into three fractions using silica gel column chromatography with hexane (alkanes), 1:1 v/v hexane: dichloromethane (ketones), and 1:1 v/v dichloromethane: methanol (alcohols + acids) (Rach et al., 2020; doi:10.1016/j.orggeochem.2020.103995). Unsaturated compounds were removed from the alkane fraction using AgNO3-silica gel column chromatography with n-hexane (saturated n-alkanes) and DCM (unsaturated n-alkanes). n-alkanes were identified and quantified using an Agilent gas chromatograph (GC 7890-A) with flame ionization detection (FID) coupled to a single quadrupole mass spectrometer (MS 5975-C). We quantified n-alkane concentrations relative to the peak response of the internal standard, and then normalized the abundance to the sediment mass. We measured n-alkane d13C via GC-C-IRMS (gas chromatography/combustion/isotope-ratio mass spectrometry) with helium as a carrier gas (Agilent 7890N, ThermoFisher Delta V Plus). All compounds were measured in triplicate with a standard deviation of =0.5‰. Measurement quality was checked regularly by measuring n-alkane standards (nC15, nC20, nC25) with known isotopic composition (provided by Campro Scientific, Germany). d13C values were normalized to the Vienna Pee Dee Belemnite (VPDB) standard. We measured n-alkane d2H via GC-IRMS using a ThermoFisher Scientific Trace GC 1310 coupled to a Delta-V isotope ratio mass spectrometer. All d2H measurements were made in duplicate, and measurement quality was checked with d2H values were normalized to the Vienna Standard Mean Ocean Water (VSMOW) standard using an n-alkane standard mix with known d2H values (nC16 - nC30, from A. Schimmelman/Indiana University).
    Keywords: Accelerated Solvent Extraction (Dionex ASE); Average chain length; Biomarker; Bucket, plastic; Carbon, organic, total; Carbon Preference Index; Compound-specific Isotopes; Date/Time of event; Date/Time of event 2; Distance; Event label; Fraction modern carbon, organic; Fraction modern carbon, organic, error; Gas chromatography (Agilent GC 7890-A) with flame ionization detection (FID) coupled to a single quadrupole mass spectrometer (MS 5975-C); Gas chromatography-combustion-isotope ratio mass spectrometry (GC-C-IRMS) with helium as a carrier gas (Agilent 7890N, ThermoFisher Delta V Plus); Gas chromatography - Isotope ratio mass spectrometer (GC-IRMS) (ThermoFisher Scientific Trace GC 1310) coupled to a Delta-V isotope ratio mass spectrometer; Latitude of event; Longitude of event; Median, grain size; n-Alkane, (C31+C33)/(C27+C29) ratio; n-Alkane, sum, per unit mass total organic carbon; n-Alkane, total per unit sediment mass; n-Alkane C16, per unit sediment mass; n-Alkane C17, per unit sediment mass; n-Alkane C18, per unit sediment mass; n-Alkane C19, per unit sediment mass; n-Alkane C20, per unit sediment mass; n-Alkane C21, per unit sediment mass; n-Alkane C22, per unit sediment mass; n-Alkane C23, per unit sediment mass; n-Alkane C24, per unit sediment mass; n-Alkane C25, per unit sediment mass; n-Alkane C26, per unit sediment mass; n-Alkane C27, per unit sediment mass; n-Alkane C27, δ13C; n-Alkane C27, δ13C, standard deviation; n-Alkane C27, δD; n-Alkane C27, δD, standard deviation; n-Alkane C28, per unit sediment mass; n-Alkane C29, per unit sediment mass; n-Alkane C29, δ13C; n-Alkane C29, δ13C, standard deviation; n-Alkane C29, δD; n-Alkane C29, δD, standard deviation; n-Alkane C30, per unit sediment mass; n-Alkane C31, per unit sediment mass; n-Alkane C31, δ13C; n-Alkane C31, δ13C, standard deviation; n-Alkane C31, δD; n-Alkane C31, δD, standard deviation; n-Alkane C32, per unit sediment mass; n-Alkane C33, per unit sediment mass; n-Alkane C33, δ13C; n-Alkane C33, δ13C, standard deviation; n-Alkane C33, δD; n-Alkane C33, δD, standard deviation; n-Alkane C34, per unit sediment mass; n-Alkane C35, per unit sediment mass; n-alkanes; n-Alkanes, total mass; PLV_01062017; PLV_07092017; PLV_09072017; PLV_11122017; PLV_12012018; PLV_12062017; PLV_16032018; PLV_21022018; Puerto lavalle; River discharge; river sediment; Sample ID; Sample mass; Sampling date; Size fraction 〈 0.030 mm; WB; δ13C, organic carbon
    Type: Dataset
    Format: text/tab-separated-values, 423 data points
    Location Call Number Limitation Availability
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  • 8
    Publication Date: 2023-10-13
    Description: Endmember samples were collected and analyzed to determine the sources of organic material in the river suspended sediment. Endmembers include soil, leaf litter, and floodplain sediment. Soil and leaf litter samples were collected using an ethanol-cleaned hand trowel. Floodplain sediment samples were collected using an Edelman-type hand auger drilled down to a maximum of ~5 m. Samples were stored in paper bags, and then oven-dried at 40°C. n-alkanes were identified and quantified using an Agilent gas chromatograph (GC 7890-A) with flame ionization detection (FID) coupled to a single quadrupole mass spectrometer (MS 5975-C). We quantified n-alkane concentrations relative to the peak response of the internal standard, and then normalized the abundance to the sediment mass. We measured n-alkane d13C via GC-C-IRMS (gas chromatography/combustion/isotope-ratio mass spectrometry) with helium as a carrier gas (Agilent 7890N, ThermoFisher Delta V Plus). All compounds were measured in triplicate with a standard deviation of =0.5‰. Measurement quality was checked regularly by measuring n-alkane standards (nC15, nC20, nC25) with known isotopic composition (provided by Campro Scientific, Germany). d13C values were normalized to the Vienna Pee Dee Belemnite (VPDB) standard. We measured n-alkane d2H via GC-IRMS using a ThermoFisher Scientific Trace GC 1310 coupled to a Delta-V isotope ratio mass spectrometer. All d2H measurements were made in duplicate, and measurement quality was checked with d2H values were normalized to the Vienna Standard Mean Ocean Water (VSMOW) standard using an n-alkane standard mix with known d2H values (nC16 - nC30, from A. Schimmelman/Indiana University).
    Keywords: AR15DS-024-S; AR15DS-027; AR15DS-038-S-10; AR15DS-045-S; AR15DS-046-S-5; AR15DS-048-S-30; AR15DS-048-S-60; AR15DS-052-S; AR15DS-057; AR15DS-057-S; AR15DS-060-S; AR15DS-063-S; AR15DS-38-S-5; AR16JS-01; AR16JS-08; AR16JS-10; AR16JS-10-A; AR17JS10; AR17MR-18; AR17MR-29; AR17MR-38; AR17MR-48; AR17MR-49; AR17MR-54; AR17MR-55; Average chain length; Bermejo at Rio Paraguay; Biomarker; Carbon, organic, total; Carbon Preference Index; Compound-specific Isotopes; Date/Time of event; DEPTH, sediment/rock; Distance; El Colgado; El Colorado; Embarcacion; Event label; Gas chromatography (Agilent GC 7890-A) with flame ionization detection (FID) coupled to a single quadrupole mass spectrometer (MS 5975-C); Gas chromatography-combustion-isotope ratio mass spectrometry (GC-C-IRMS) with helium as a carrier gas (Agilent 7890N, ThermoFisher Delta V Plus); Gas chromatography - Isotope ratio mass spectrometer (GC-IRMS) (ThermoFisher Scientific Trace GC 1310) coupled to a Delta-V isotope ratio mass spectrometer; Grl Mansilla; Latitude of event; Location of event; Longitude of event; MR18-PLV-LL; MR18-SZ-LL; MR18-SZ-Soil; n-Alkane, (C31+C33)/(C27+C29) ratio; n-Alkane, sum, per unit mass total organic carbon; n-Alkane, total per unit sediment mass; n-Alkane C17, per unit sediment mass; n-Alkane C18, per unit sediment mass; n-Alkane C19, per unit sediment mass; n-Alkane C20, per unit sediment mass; n-Alkane C21, per unit sediment mass; n-Alkane C22, per unit sediment mass; n-Alkane C23, per unit sediment mass; n-Alkane C24, per unit sediment mass; n-Alkane C25, per unit sediment mass; n-Alkane C26, per unit sediment mass; n-Alkane C27, per unit sediment mass; n-Alkane C27, δ13C; n-Alkane C27, δ13C, standard deviation; n-Alkane C27, δD; n-Alkane C27, δD, standard deviation; n-Alkane C28, per unit sediment mass; n-Alkane C29, per unit sediment mass; n-Alkane C29, δ13C; n-Alkane C29, δ13C, standard deviation; n-Alkane C29, δD; n-Alkane C29, δD, standard deviation; n-Alkane C30, per unit sediment mass; n-Alkane C31, per unit sediment mass; n-Alkane C31, δ13C; n-Alkane C31, δ13C, standard deviation; n-Alkane C31, δD; n-Alkane C31, δD, standard deviation; n-Alkane C32, per unit sediment mass; n-Alkane C33, per unit sediment mass; n-Alkane C33, δ13C; n-Alkane C33, δ13C, standard deviation; n-Alkane C33, δD; n-Alkane C33, δD, standard deviation; n-Alkane C34, per unit sediment mass; n-Alkane C35, per unit sediment mass; n-Alkane C36, per unit sediment mass; n-Alkane C37, per unit sediment mass; n-alkanes; n-Alkanes, total mass; Pozo Sarmiento; Puente Lavalle; Puerto lavalle; Reserva Natural Formosa; river sediment; RSF-RB confluence; Sample ID; Sample mass; Sample type; Sauzalito; ST15-52; Villa Rio Bermejito; δ13C, organic carbon
    Type: Dataset
    Format: text/tab-separated-values, 1424 data points
    Location Call Number Limitation Availability
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  • 9
    Publication Date: 2023-10-13
    Description: We extracted and analyzed n-alkane compounds from river suspended sediment collected from the Rio Bermejo in Argentina. We collected 24 river depth profile samples collected during March 2017. We collected suspended particulate matter from water depth profiles at four locations along the mainstem Rio Bermejo (river km 135, 420, 865, 1220), one location on the Rio San Francisco (RSF) (river km -15), and one location on the Rio Bermejo upstream from the RSF confluence (river km -10) (Fig. 1a). We homogenized and disaggregated the dry sediment using a mortar and pestle, and removed coarse plant material 〉1 mm. For each sample, we weighed an aliquot of sediment and loaded the material into aluminum cells for lipid extraction. Total lipid extracts (TLE) were recovered using an accelerated solvent extraction system (Dionex ASE) with 9:1 v/v dichloromethane: methanol. We added exactly 10 µg of internal standard (5-a-Androstane) to the TLE for unknown compound quantification. We then separated the TLE into three fractions using silica gel column chromatography with hexane (alkanes), 1:1 v/v hexane: dichloromethane (ketones), and 1:1 v/v dichloromethane: methanol (alcohols + acids) (Rach et al., 2020; doi:10.1016/j.orggeochem.2020.103995). Unsaturated compounds were removed from the alkane fraction using AgNO3-silica gel column chromatography with n-hexane (saturated n-alkanes) and DCM (unsaturated n-alkanes). n-alkanes were identified and quantified using an Agilent gas chromatograph (GC 7890-A) with flame ionization detection (FID) coupled to a single quadrupole mass spectrometer (MS 5975-C). We quantified n-alkane concentrations relative to the peak response of the internal standard, and then normalized the abundance to the sediment mass. We measured n-alkane d13C via GC-C-IRMS (gas chromatography/combustion/isotope-ratio mass spectrometry) with helium as a carrier gas (Agilent 7890N, ThermoFisher Delta V Plus). All compounds were measured in triplicate with a standard deviation of =0.5‰. Measurement quality was checked regularly by measuring n-alkane standards (nC15, nC20, nC25) with known isotopic composition (provided by Campro Scientific, Germany). d13C values were normalized to the Vienna Pee Dee Belemnite (VPDB) standard. We measured n-alkane d2H via GC-IRMS using a ThermoFisher Scientific Trace GC 1310 coupled to a Delta-V isotope ratio mass spectrometer. All d2H measurements were made in duplicate, and measurement quality was checked with d2H values were normalized to the Vienna Standard Mean Ocean Water (VSMOW) standard using an n-alkane standard mix with known d2H values (nC16 - nC30, from A. Schimmelman/Indiana University).
    Keywords: AR17MR-05; AR17MR-06; AR17MR-07; AR17MR-08; AR17MR-11; AR17MR-12; AR17MR-13; AR17MR-14; AR17MR-17; AR17MR-24; AR17MR-25; AR17MR-26; AR17MR-27; AR17MR-30; AR17MR-31; AR17MR-32; AR17MR-33; AR17MR-34; AR17MR-35; AR17MR-36; AR17MR-42; AR17MR-43; AR17MR-44; AR17MR-45; AR17MR-46; AR17MR-57; Average chain length; Biomarker; Carbon, organic, total; Carbon, organic/Nitrogen, total ratio; Carbon Preference Index; Compound-specific Isotopes; Date/Time of event; Depth, relative; DEPTH, water; El Colgado; El Colorado; Embarcacion; Event label; Gas chromatography (Agilent GC 7890-A) with flame ionization detection (FID) coupled to a single quadrupole mass spectrometer (MS 5975-C); Gas chromatography-combustion-isotope ratio mass spectrometry (GC-C-IRMS) with helium as a carrier gas (Agilent 7890N, ThermoFisher Delta V Plus); Gas chromatography - Isotope ratio mass spectrometer (GC-IRMS) (ThermoFisher Scientific Trace GC 1310) coupled to a Delta-V isotope ratio mass spectrometer; General Mansilla; Latitude of event; Location of event; Longitude of event; n-Alkane, (C31+C33)/(C27+C29) ratio; n-Alkane, sum, per unit mass total organic carbon; n-Alkane, total per unit sediment mass; n-Alkane C17, per unit sediment mass; n-Alkane C18, per unit sediment mass; n-Alkane C19, per unit sediment mass; n-Alkane C20, per unit sediment mass; n-Alkane C21, per unit sediment mass; n-Alkane C22, per unit sediment mass; n-Alkane C23, per unit sediment mass; n-Alkane C24, per unit sediment mass; n-Alkane C25, per unit sediment mass; n-Alkane C26, per unit sediment mass; n-Alkane C27, per unit sediment mass; n-Alkane C27, δ13C; n-Alkane C27, δ13C, standard deviation; n-Alkane C27, δD; n-Alkane C27, δD, standard deviation; n-Alkane C28, per unit sediment mass; n-Alkane C29, per unit sediment mass; n-Alkane C29, δ13C; n-Alkane C29, δ13C, standard deviation; n-Alkane C29, δD; n-Alkane C29, δD, standard deviation; n-Alkane C30, per unit sediment mass; n-Alkane C31, per unit sediment mass; n-Alkane C31, δ13C; n-Alkane C31, δ13C, standard deviation; n-Alkane C31, δD; n-Alkane C31, δD, standard deviation; n-Alkane C32, per unit sediment mass; n-Alkane C33, per unit sediment mass; n-Alkane C33, δ13C; n-Alkane C33, δ13C, standard deviation; n-Alkane C33, δD; n-Alkane C33, δD, standard deviation; n-Alkane C34, per unit sediment mass; n-Alkane C35, per unit sediment mass; n-alkanes; n-Alkanes, total mass; Puerto lavalle; Reserva Natural Formosa; Rio San Francisco; river sediment; Sample ID; Sample type; δ13C, organic carbon
    Type: Dataset
    Format: text/tab-separated-values, 1070 data points
    Location Call Number Limitation Availability
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  • 10
    Publication Date: 2023-11-03
    Keywords: 15OJ10; AWI_Envi; Core; CORE; DEPTH, sediment/rock; Gas chromatography - Isotope ratio mass spectrometer (GC-IRMS); Lake Otjikoto; n-Alkane C27, δ13C; n-Alkane C29, δ13C; n-Alkane C31, δ13C; n-Alkane C33, δ13C; n-Alkanol C28, δ13C; n-Alkanol C30, δ13C; n-Alkanol C32, δ13C; Namibia; Polar Terrestrial Environmental Systems @ AWI; Sample ID
    Type: Dataset
    Format: text/tab-separated-values, 160 data points
    Location Call Number Limitation Availability
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