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  • GEOMAR Catalogue / E-Books  (1)
  • Data  (17)
  • 2020-2024  (18)
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  • GEOMAR Catalogue / E-Books  (1)
  • Data  (17)
  • OceanRep  (2)
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  • 1
    Keywords: Forschungsbericht ; Südchinesisches Meer ; Perlfluss ; Delta ; Megastadt ; Schadstoffbelastung ; Eutrophierung
    Type of Medium: Online Resource
    Pages: 1 Online-Ressource (23 Seiten, 1,55 MB) , Illustrationen, Diagramme
    Language: German , English
    Note: Förderkennzeichen BMBF 03G0269B , Verbundnummer 01184657 , Literaturverzeichnis: Seite 18-19 , Unterschiede zwischen dem gedruckten Dokument und der elektronischen Ressource können nicht ausgeschlossen werden , Sprache der Kurzfassungen: Deutsch, Englisch
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  • 2
    Publication Date: 2024-06-29
    Description: The Indian Summer Monsoon (ISM) with its rainfall is the lifeline for people living on the Indian subcontinent today and possibly was the driver of the rise and fall of early agricultural societies in the past. Intensity and position of the ISM have shifted in response to orbitally forced thermal land-ocean contrasts. At the northwestern monsoon margins, interactions between the subtropical westerly jet (STWJ) and the ISM constitute a tipping element in the Earth's climate system, because their non-linear interaction may be a first-order influence on rainfall. We reconstructed marine sea surface temperature (SST), supply of terrestrial material and vegetation changes from a very well-dated sediment core from the northern Arabian Sea to reconstruct the STWJ-ISM interaction. The Holocene record (from 11,000 years) shows a distinct, but gradual, southward displacement of the ISM in the Early to Mid-Holocene, increasingly punctuated by phases of intensified STWJ events that are coeval with interruptions of North Atlantic overturning circulation (Bond events). Effects of the non-linear interactions culminate between 4.6-3 ka BP, marking a climatic transition period during which the ISM shifted southwards and the influence of SWTJ became prominent. The lithogenic input shows an up to 4-fold increase after this time period signaling the strengthened influence of agricultural activities of the Indus civilization with enhanced erosion of soils amplifying the impact of Bond events and adding to the marine sedimentation rates adjacent to the continent.
    Keywords: Alkenones; Arabian Sea; CAHOL; CAME-II_CAHOL; Crossing Climatic Tipping Points - Central Asian Holocene Climate; Grain Size; KAL; Kasten corer; n-alkanes; PAKOMIN; SO90; SO90_63KA; Sonne
    Type: Dataset
    Format: application/zip, 4 datasets
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  • 3
    Publication Date: 2024-06-29
    Description: The data sets contains the age model as well as bulk organic and n-alkane data of sediment core GeoTü SL167 to reconstruct changes of the oxygen minimum zone strength for the late Quaternary. The age model is based on 14C AMS measurements of planktonic foraminifera and is calibrated with the BACON v. 2.5.6 software for R (Blauuw & Christen, 2011) and a marine reservoir age of ΔR = 93 ± 61 years. The ΔR is based on the weighted mean of two regional marine reservoir corrections (Muscat) by Southon et al. (2002) using the marine calibration database (Reimer and Reimer, 2001, http://calib.org/marine/). Total organic carbon and nitrogen measurements were carried out with an Euro EA3000 elemental analyser and δ15N measurements with a Thermo Scientific Flash EA1112 coupled to a Finnigan MAT 252 IRMS. Total organic carbon mass accumulation rates (TOC MAR) based on calculation using the organic carbon content and total mass accumulation rates. A description of the calculation of the total mass accumulations rates is given in Burdanowitz et al 2021. The measurements of n-alkanes were carried out using Thermo Scientific Trace 1310 GC-FID and Thermo Scientific DSQ II (GC-MS). Gravity core GeoTü SL167, was retrieved at station no. 960 during R.V. METEOR cruise M74/1b in 2007 (Bohrmann et al., 2010) from the northwestern Arabian Sea off Oman, at 22°37.2'N, 59°41.5'E, 774 m water depth, core recovery 7.39 m. The sediment core was retrieved for the reconstruction of circulation and productivity changes in the eastern Mediterranean Sea during the late Quaternary with particular focus on changes in the Indian monsoon system.
    Keywords: Age model; Arabian Sea; CLICCS; Cluster of Excellence: Climate, Climatic Change, and Society; Denitrification; n-alkanes; OMZ; Quaternary
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 4
    Publication Date: 2024-06-29
    Description: This large set of sediment trap samples was collected in different oceanic areas between 1993 and 2017 from shelf seas to the deep ocean. The samples were compiled from previous studies and used for statistical analyses in order to better understand particle dynamics and organic matter cycling in the ocean and to test and refine amino acid (AA) and hexosamine (HA) based biogeochemical indicators. Samples were analysed for total nitrogen (N) using a Carlo Erba nitrogen analyser 1500. Total organic carbon (TOC) was measured with the same instrument after treatment of weighed samples with 1N HCl to remove carbonate. Stable nitrogen isotopes of total particulate nitrogen (δ15N-TPN) were analysed with the mass spectrometer ThermoFisher Scientific MAT 252. AA and HA contents and their individual monomers were analysed by liquid chromatography using a Biochrom 30 amino acid analyzer. Total fluxes, TOC and AA fluxes were calculated in mg m-2 d-1. Contents of AA and HA are presented in µmol/g and µg/g. AAC, AAN, HAC, HAN are presented in µg/g and as percentages of TOC (AA-C/C, HA-C/C) or TN (AA-N/N, HA-N/N). AA and HA monomers are presented in Mol% and comprise aspartic acid (ASP), glutamic acid (Glu), threonine (Thr), serine (Ser), glycine (Gly), alanine (Ala), valine (Val), methionine (Met), isoleucine (Ile), leucine (Leu), tyrosine (Tyr), phenylalanine (Phe), β-Alanine (β-Ala), γ-aminobutyric acid (γ-Aba), histidine (His), ornithine (Orn), lysine (Lys) and arginine (Arg), glucosamine (GlcN) and galactosamine (GalN), cysteic acid (CYA), taurine (TAU), methionine sulfoximine (MSO) and tryptophane (TRP) were determined only in the more recent samples. Data gaps indicate that measurements were not carried out or that they were not stored in the older data sets. The RI was calculated according to Jennerjahn and Ittekkot (1997; https://archimer.ifremer.fr/doc/00093/20403/) and the DI after Dauwe et al. (1999; doi:10.4319/lo.1999.44.7.1809). Definitions of biogeochemical indicators SDI, RTI, ox/anox and a detailed description of the methods can be found in Gaye et al. (2022; doi:org/10.5194/bg-19-807-2022).
    Keywords: Akademik Boris Petrov; Alanine; Amino acid, carbon; Amino acid, carbon of total organic carbon; Amino acid, flux; Amino acid, nitrogen; Amino acid analyser, Biochrom 30; Amino acid nitrogen of total nitrogen; amino acids; Amino acids; Amino acids/hexosamines ratio; Amino acids non-protein; Amino sugar, carbon; Amino sugar, carbon of total organic carbon; Amino sugar, nitrogen; Amino sugar, nitrogen of total nitrogen; Arabian Sea; Arginine; Aspartic acid; Aspartic acid/beta-Alanine ratio; beta-Alanine; BP00; BP00-24a-Yenisei_02; BP01; BP01-61a-Kara_02; BP02; BP02-04-Yenisei_04; BP99; BP99-01-Ob01; BP99-15-Yen01; Calculated after Dauwe et al. 1999; Calculated after Gaye et al. (2022); Calculated after Jennerjahn and Ittekkot (1997); Carbon, organic, flux; Carbon, organic, total; CAST; Central Arabian Sea Trap Station; Cysteic acid; DATE/TIME; Degradation index; degradation indicators; Deployment: BP00-24a; Recovery: BP01-02; Deployment: BP01-61a; Recovery: BP02-01A; Deployment: BP02-04; Recovery: BP03-04a; Deployment: BP99-01; Deployment: M44/1_7ST; Recovery: M44/4_ST244; Deployment: MSM17/3_223-2; Recovery: MSM17/3_258-2; DEPTH, water; EAST; Eastern Arabian Sea Trap Station; Eastern Basin; East Pakistan Trap Station; ENAT; EPT; Event label; Galactosamine; gamma-Aminobutyric acid; Gas chromatography with Carlo Erba NA1500 after treatment with HCL; Gas chromatography with Carlo Erba NA-1500 CNS elemental analyzer; Glucosamine; Glucosamine/Galactosamine ratio; Glutamic acid; Glutamic acid/gamma-Aminobutyric acid ratio; Glycine; hexosamines; Hexosamines; Histidine; INDEX2016_TRAP_01-01; INDEX2016_TRAP_03-01; Indian Ocean; Isoleucine; JAM-1; Kara Sea; Leucine; Location; Lysine; M44/1; M44/1_7-MID; Maria S. Merian; Mass spectrometer, ThermoFisher Scientific MAT 252; Meteor (1986); Methionine; Methionine sulfoximine; MOOR; Mooring; Mooring (long time); MOORY; MSM17/3; MSM17/3_222-M; MSM17/3_223-D; MSM59/2_Deployment_01-01,SO259_Recovery_01-01; MSM59/2_Deployment_03-01,SO259_Recovery_03-01; NAST; NEAST; Nitrogen, total; Northeastern Arabian Sea Trap Station; Northern Arabian Sea Trap Station; off south Java; organic matter degradability; Ornithine; Other event; Ox/Anox ratio; Phenylalanine; Reactivity index of amino acids (Jennerjahn & Ittekkot, 1997); Recovery: MSM17/3_222-4; Reference/source; Reference of data; Residence time index; Sample ID; SAST; Sediment degradation index; sediment trap samples; Serine; sinking particles; South Atlantic Ocean; Southern Arabian Sea Trap Station; Station label; Taurine; Threonine; Total mass, flux per day; Trap; TRAP; Trap, sediment; TRAPS; Tryptophan; Tyrosine; Valine; WAST; Western Arabian Sea Trap Station; West Pakistan Trap Station; WNAT; WPT; δ15N
    Type: Dataset
    Format: text/tab-separated-values, 11335 data points
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  • 5
    Publication Date: 2024-06-29
    Description: This large set of suspended matter (SPM) samples was collected in different oceanic areas between 1999 and 2017 from shelf seas to the deep ocean. The samples were compiled from previous studies and used for statistical analyses in order to better understand particle dynamics and organic matter cycling in the ocean and to test and refine amino acid (AA) and hexosamine (HA) based biogeochemical indicators. Samples were analysed for total nitrogen (N) and total carbon (C) using a Carlo Erba nitrogen analyser 1500. Total organic carbon (TOC) was measured with the same instrument after treatment of weighed samples with 1N HCl to remove carbonate. Stable nitrogen isotopes of total particulate nitrogen (δ15N-TPN) were analysed with the mass spectrometer Thermo Finnigan MAT 252. AA and HA contents and their individual monomers were analysed by liquid chromatography using a Biochrom 30 amino acid analyzer. Contents of AA and HA are presented in nmol/g and µg/g. AAC, AAN, HAC, HAN are presented in µg/g and as percentages of TOC (AAC/C, HAC/C) or TN (AAN/N, HAN/N). AA and HA monomers are presented in Mol% and comprise aspartic acid (ASP), glutamic acid (Glu), threonine (Thr), serine (Ser), glycine (Gly), alanine (Ala), valine (Val), methionine (Met), isoleucine (Ile), leucine (Leu), tyrosine (Tyr), phenylalanine (Phe), β-Alanine (β-Ala), γ-aminobutyric acid (γ-Aba), histidine (His), ornithine (Orn), lysine (Lys) and arginine (Arg), glucosamine (Gluam) and galactosamine (Galam). Cysteic acid (CYA), taurine (TAU), methionine sulfoximine (MSO) and tryptophane (TRP) were determined only in the more recent samples. Data gaps indicate that measurements were not carried out or that they were not stored in the older data sets. The RI was calculated according to Jennerjahn and Ittekkot (1997; https://archimer.ifremer.fr/doc/00093/20403/) and the DI after Dauwe et al. (1999; doi:10.4319/lo.1999.44.7.1809). Definitions of biogeochemical indicators SDI, RTI, ox/anox and a detailed description of the methods can be found in Gaye et al. (2022).
    Keywords: Akademik Boris Petrov; Alanine; Amino acid, carbon; Amino acid, carbon of total organic carbon; Amino acid, nitrogen; Amino acid analyser, Biochrom 30; Amino acid nitrogen of total nitrogen; amino acids; Amino acids; Amino acids/hexosamines ratio; Amino acids non-protein; Amino sugar, carbon; Amino sugar, carbon of total organic carbon; Amino sugar, nitrogen; Amino sugar, nitrogen of total nitrogen; Arabian Sea; Arginine; Aspartic acid; Aspartic acid/beta-Alanine ratio; beta-Alanine; BP00; BP00-02; BP00-03; BP00-04; BP00-05; BP00-06; BP00-07; BP00-08; BP00-09; BP00-13; BP00-15; BP00-16; BP00-17; BP00-19; BP00-20; BP00-21; BP00-22; BP00-23; BP00-24; BP00-26; BP00-27; BP00-28; BP00-29; BP00-30; BP00-31; BP00-35; BP00-36; BP00-38; BP99; BP99-01; BP99-03; BP99-08; BP99-11; BP99-13; BP99-17; BP99-20; BP99-21; BP99-25; BP99-26; BP99-30; BP99-31; BP99-32; BP99-35; BP99-37; BP99-FEM; BP99-Ob-Salechard_1; BP99-Ob-Salechard_2; BP99-Soil; BUCKET; Bucket water sampling; Calculated after Dauwe et al. 1999; Calculated after Gaye et al. (2022); Calculated after Jennerjahn and Ittekkot (1997); Campaign of event; Carbon, organic, total; Carbon, total; CTD/Rosette; CTD-RO; Cysteic acid; Date/Time of event; Degradation index; degradation indicators; DEPTH, water; Dredge; DRG; Elevation of event; Event label; Galactosamine; gamma-Aminobutyric acid; Gas chromatography with Carlo Erba NA1500 after treatment with HCL; Gas chromatography with Carlo Erba NA-1500 CNS elemental analyzer; Glucosamine; Glucosamine/Galactosamine ratio; Glutamic acid; Glutamic acid/gamma-Aminobutyric acid ratio; Glycine; hexosamines; Hexosamines; Histidine; INDEX2016_2; INDEX2017; Indian Ocean; Isoleucine; Kara Sea; Latitude of event; Leucine; Location; Longitude of event; Lysine; M103/1; M103/1_10-2; M103/1_1-1; M103/1_11-2; M103/1_20-4; M103/1_2-2; M103/1_22-2; M103/1_2283-1; M103/1_2284-4; M103/1_2285-4; M103/1_2286-1; M103/1_2287-1; M103/1_2288-1; M103/1_2289-4; M103/1_2290-3; M103/1_2291-4; M103/1_28-5; M103/1_30-4; M103/1_3-1; M103/1_34-1; M103/1_4-1; M103/1_43-1; M103/1_44-2; M103/1_45-2; M103/1_46-2; M103/1_47-2; M103/1_48-5; M103/1_5-1; M103/1_53-1; M103/1_59-1; M103/1_6-2; M103/1_65-1; M103/1_67-1; M103/1_7-2; M103/1_8-4; M103/1_9-1; M74/1b; M74/1b_944-1; M74/1b_945-1; M74/1b_946-3; M74/1b_947-1; M74/1b_948-1; M74/1b_949-1; M74/1b_950-3; M74/1b_951-3; M74/1b_953-3; M74/1b_954-1; M74/1b_955-1; M74/1b_956-3; M74/1b_957-4; M74/1b_958-1; M76/2; M76/2_195_WS; M76/2_198_WS; M76/2_200_WS; M76/2_201_WS; M76/2_202_WS; M76/2_204_WS; M76/2_206_WS; M76/2_252_WS; Maria S. Merian; Mass spectrometer, ThermoFisher Scientific MAT 252; Meteor (1986); Methionine; Methionine sulfoximine; MSM59/2; MSM59/2_734-2; MSM59/2_734-3; MSM59/2_739-1; MSM59/2_739-2; MSM59/2_749-1; MSM59/2_749-2; MSM59/2_751-1; MSM59/2_769-1; MSM59/2_769-2; MSM59/2_783-1; MSM59/2_783-2; MULT; Multiple investigations; Namibia upwelling, Southeast Atlantic; Nitrogen, total; organic matter cycling; organic matter degradation; Ornithine; Ox/Anox ratio; Phenylalanine; Reactivity index of amino acids (Jennerjahn & Ittekkot, 1997); Residence time index; Sample ID; Sediment degradation index; Serine; SO259; SO259_100-1; SO259_1-1; SO259_15-1; SO259_16-1; SO259_2-1; SO259_3-1; SO259_4-1; SO259_49-1; SO259_50-1; SO259_5-1; SO259_60-1; SO259_6-1; SO259_61-1; SO259_99-1; Sonne_2; Suspended particulate matter; Taurine; Threonine; Tryptophan; Tyrosine; Valine; Water sample; WS; δ15N, total particulate nitrogen
    Type: Dataset
    Format: text/tab-separated-values, 30425 data points
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  • 6
    Publication Date: 2024-06-29
    Description: Raw data acquired by position sensors on board RV SONNE during expedition SO303 were processed to receive a validated master track which can be used as reference of further expedition data. During SO303 the motion reference unit Kongsberg SeaTex AS MRU-5 combined with Kongsberg SeaTex AS Seapath 320 and two GPS receivers SAAB MGL-4 were used as navigation sensors. Data were downloaded from DAVIS SHIP data base (https://dship.bsh.de) with a resolution of 1 sec. Processing and evaluation of the data is outlined in the data processing report. Processed data are provided as a master track with 1 sec resolution derived from the position sensors' data selected by priority and a generalized track with a reduced set of the most significant positions of the master track.
    Keywords: BIOGIN (IIEO2); Calculated; Course; CT; DAM_Underway; DAM Underway Research Data; DATE/TIME; LATITUDE; LONGITUDE; SO303; SO303-track; Sonne_2; Speed; Underway cruise track measurements
    Type: Dataset
    Format: text/tab-separated-values, 11600 data points
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  • 7
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    PANGAEA
    In:  University of Hamburg, Germany
    Publication Date: 2024-06-29
    Description: Raw data acquired by position sensors on board RV SONNE during expedition SO303 were processed to receive a validated master track which can be used as reference of further expedition data. During SO303 the motion reference unit Kongsberg SeaTex AS MRU-5 combined with Kongsberg SeaTex AS Seapath 320 and two GPS receivers SAAB MGL-4 were used as navigation sensors. Data were downloaded from DAVIS SHIP data base (https://dship.bsh.de) with a resolution of 1 sec. Processing and evaluation of the data is outlined in the data processing report. Processed data are provided as a master track with 1 sec resolution derived from the position sensors' data selected by priority and a generalized track with a reduced set of the most significant positions of the master track.
    Keywords: 1 sec resolution; BIOGIN (IIEO2); CT; DAM_Underway; DAM Underway Research Data; SO303; SO303-track; Sonne_2; Underway cruise track measurements
    Type: Dataset
    Format: application/zip, 146.8 MBytes
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  • 8
    Publication Date: 2024-06-29
    Description: This data set contains the unsaturation ratio of C37 alkenones and the alkenone-derived sea surface temperature reconstructions of sediment core GeoTü SL167. The measurements of the alkenones were carried out using a Thermo Scientific Trace 1310 GC-FID. The unsaturation ratio of C37 alkenones were converted into sea surface temperatures using a regional core top calibration of Indian Ocean sediments by Sonzogni et al. (1997). Gravity core GeoTü SL167, was retrieved at station no. 960 during R.V. METEOR cruise M74/1b in 2007 (Bohrmann et al., 2010) from the northwestern Arabian Sea off Oman, at 22°37.2'N, 59°41.5'E, 774 m water depth, core recovery 7.39 m. The sediment core was retrieved for the reconstruction of circulation and productivity changes in the northwestern Arabian Sea during the late Quaternary with particular focus on changes in the Indian monsoon system.
    Keywords: AGE; Alkenone, unsaturation index UK'37; alkenone SST; Alkenone Uk'37 index; Arabian Sea; Calculated from UK'37 (Sonzogni et al., 1997); DEPTH, sediment/rock; Depth, sediment/rock, bottom/maximum; Depth, sediment/rock, top/minimum; Gas chromatography - Flame Ionization Detection (GC-FID), Thermo Scientific, Trace 1310; Gravity corer (Kiel type); Indian Monsoon; M74/1b; M74/1b_960-1; Meteor (1986); Oman Margin; Quaternary paleoclimatic records; Sea surface temperature; Sea surface temperature, standard deviation; SL; SL 167
    Type: Dataset
    Format: text/tab-separated-values, 1095 data points
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  • 9
    Publication Date: 2024-06-29
    Keywords: Accumulation rate, lithogenic; AGE; Alkenones; Arabian Sea; CAHOL; CAME-II_CAHOL; Crossing Climatic Tipping Points - Central Asian Holocene Climate; DEPTH, sediment/rock; Grain Size; KAL; Kasten corer; n-alkanes; PAKOMIN; SO90; SO90_63KA; Sonne
    Type: Dataset
    Format: text/tab-separated-values, 172 data points
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  • 10
    Publication Date: 2024-06-29
    Keywords: AGE; Alkenones; Arabian Sea; CAHOL; CAME-II_CAHOL; Crossing Climatic Tipping Points - Central Asian Holocene Climate; DEPTH, sediment/rock; Grain Size; KAL; Kasten corer; n-alkanes; PAKOMIN; Size fraction; SO90; SO90_63KA; Sonne
    Type: Dataset
    Format: text/tab-separated-values, 9344 data points
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