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  • 1
    Keywords: Forschungsbericht
    Type of Medium: Online Resource
    Pages: Online-Ressource (9 S., 74,89 KB)
    Language: German
    Note: Förderkennzeichen BMBF 03G0806B. - Verbund-Nr. 01088026 , Engl. Berichtsbl. u.d.T.: CARIMA - Natural vs. anthropogenic controls of past monsoon variability in central Asia recorded in marine archives; TP1.1 - Palaeproductivity and changes of carbon- and nitrogen cycling , Unterschiede zwischen dem gedruckten Dokument und der elektronischen Ressource können nicht ausgeschlossen werden , Systemvoraussetzungen: Acrobat reader.
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  • 2
    Publication Date: 2024-01-02
    Keywords: Age; AGE; Alkenone, unsaturation index UK'37; Arabian Sea; BCR; Box corer (Reineck); Calculated from UK'37 (Sonzogni et al., 1997); Calculated moving averages; DEPTH, sediment/rock; Event label; KL; MAKRAN 2; PAKOMIN; Piston corer (BGR type); Sea surface temperature, annual mean; SO130; SO130_275KL; SO90; SO90_39KG; Sonne
    Type: Dataset
    Format: text/tab-separated-values, 506 data points
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  • 3
    Publication Date: 2024-01-02
    Keywords: Age; AGE; Calculated moving averages; DEPTH, sediment/rock; KL; MAKRAN 2; Piston corer (BGR type); SO130; SO130_275KL; Sonne; Strontium/Calcium ratio
    Type: Dataset
    Format: text/tab-separated-values, 1446 data points
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  • 4
    Publication Date: 2024-01-02
    Keywords: Age; AGE; Beella digitata; Candeina nitida; Counting, foraminifera, planktic; Dentagloborotalia anfracta; DEPTH, sediment/rock; Globigerina bulloides; Globigerina falconensis; Globigerinella adamsi; Globigerinella calida; Globigerinella siphonifera; Globigerinita glutinata; Globigerinoides conglobatus; Globigerinoides ruber white; Globigerinoides sacculifer sacculifer; Globigerinoides sacculifer trilobus; Globoquadrina conglomerata; Globorotalia crassaformis; Globorotalia hirsuta; Globorotalia inflata; Globorotalia menardii; Globorotalia scitula; Globorotalia truncatulinoides dextral; Globorotalia truncatulinoides sinistral; Globorotalia tumida; Globorotaloides hexagonus; Globoturborotalita rubescens; Globoturborotalita tenella; Hastigerina pelagica; KL; MAKRAN 2; Neogloboquadrina dutertrei; Neogloboquadrina incompta; Neogloboquadrina pachyderma sinistral; Orbulina universa; Piston corer (BGR type); Pulleniatina obliquiloculata; SO130; SO130_275KL; Sonne; Specimen count; Sphaeroidinella dehiscens; Tenuitella iota; Tenuitella parkerae; Turborotalia humilis; Turborotalita quinqueloba; Δ depth
    Type: Dataset
    Format: text/tab-separated-values, 8619 data points
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  • 5
    Publication Date: 2024-01-02
    Keywords: Age; AGE; Arabian Sea; BCR; Box corer (Reineck); Bray-Curtis dissimilarities, minimum; DEPTH, sediment/rock; PAKOMIN; Principal component 1; Sea surface temperature, January-March; SO90; SO90_39KG; Sonne; Transfer Function Technique (TFT)
    Type: Dataset
    Format: text/tab-separated-values, 80 data points
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  • 6
    Publication Date: 2024-01-02
    Keywords: AGE; Beella digitata; Candeina nitida; Counting 〉150 µm fraction; Dentagloborotalia anfracta; DEPTH, sediment/rock; Foraminifera, planktic; Foraminifera, planktic, other; Foraminifera, planktic indeterminata; Globigerina bulloides; Globigerina falconensis; Globigerinella adamsi; Globigerinella calida; Globigerinella siphonifera; Globigerinita glutinata; Globigerinoides conglobatus; Globigerinoides ruber white; Globigerinoides sacculifer sac; Globigerinoides sacculifer wo sac; Globoquadrina conglomerata; Globoquadrina hexagona; Globorotalia crassaformis; Globorotalia hirsuta; Globorotalia inflata; Globorotalia menardii; Globorotalia menardii flexuosa; Globorotalia scitula; Globorotalia theyeri; Globorotalia truncatulinoides dextral; Globorotalia truncatulinoides sinistral; Globorotalia tumida; Globoturborotalita rubescens; Globoturborotalita tenella; Gravity corer (Kiel type); M74/1b; M74/1b_944-6; Meteor (1986); Neogloboquadrina dutertrei; Neogloboquadrina incompta; Neogloboquadrina pachyderma sinistral; Oman Margin; Orbulina universa; Pulleniatina obliquiloculata; SL; SL 163; Sphaeroidinella dehiscens; Tenuitella iota; Turborotalita humilis; Turborotalita quinqueloba
    Type: Dataset
    Format: text/tab-separated-values, 5460 data points
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  • 7
    Publication Date: 2024-01-02
    Keywords: AGE; DEPTH, sediment/rock; Gravity corer (Kiel type); M74/1b; M74/1b_944-6; Meteor (1986); Oman Margin; Sea surface temperature, July-September; Sea surface temperature, standard error; SL; SL 163; Transfer function (Imbrie & Kipp, 1971, in Turekian, Yale Univ Press); Weighted averaging partial least squares (WA-PLS) regression
    Type: Dataset
    Format: text/tab-separated-values, 700 data points
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  • 8
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    PANGAEA
    In:  Supplement to: Munz, Philipp; Steinke, Stephan; Böll, Anna; Lückge, Andreas; Groeneveld, Jeroen; Kucera, Michal; Schulz, Hartmut (2017): Decadal resolution record of Oman upwelling indicates solar forcing of the Indian summer monsoon (9-6 ka). Climate of the Past, 13(5), 491-509, https://doi.org/10.5194/cp-13-491-2017
    Publication Date: 2024-01-02
    Description: The Indian summer monsoon (ISM) is an important conveyor in the ocean-atmosphere coupled system on a transregional scale. Here we present a study of a sediment core from the northern Oman margin, revealing early- to mid Holocene ISM conditions on a near 20-year resolution. We assess multiple independent proxies indicative of sea surface temperatures (SST) during the upwelling season together with bottom water conditions. We use geochemical parameters, transfer functions of planktic foraminiferal assemblages and Mg/Ca paleothermometry and find evidence corroborating previous studies that upwelling intensity varies significantly in coherence to solar sunspot cycles. The dominant ~80-90-year Gleissberg cycle was apparently also affecting bottom water oxygen conditions. Although the interval from 8.4 to 5.8 ka B.P. is relatively short, the gradually decreasing trend of summer monsoon conditions was interrupted by short events of intensified ISM conditions. Results from both independent SST proxies are linked to phases of weaker OMZ conditions and enhanced carbonate preservation. This indicates that atmospheric forcing was intimately linked to bottom water properties and state of the OMZ on decadal time scales.
    Keywords: Gravity corer (Kiel type); M74/1b; M74/1b_944-6; Meteor (1986); Oman Margin; SL; SL 163
    Type: Dataset
    Format: application/zip, 5 datasets
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  • 9
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    PANGAEA
    In:  Supplement to: Munz, Philipp; Siccha, Michael; Lückge, Andreas; Böll, Anna; Kucera, Michal; Schulz, Hartmut (2015): Decadal-resolution record of winter monsoon intensity over the last two millennia from planktic foraminiferal assemblages in the northeastern Arabian Sea. The Holocene, 25(11), 1756-1771, https://doi.org/10.1177/0959683615591357
    Publication Date: 2024-01-02
    Description: The Indian monsoon system is an important climate feature of the northern Indian Ocean. Small variations of the wind and precipitation patterns have fundamental influence on the societal, agricultural, and economic development of India and its neighboring countries. To understand current trends, sensitivity to forcing, or natural variation, records beyond the instrumental period are needed. However, high-resolution archives of past winter monsoon variability are scarce. One potential archive of such records are marine sediments deposited on the continental slope in the NE Arabian Sea, an area where present-day conditions are dominated by the winter monsoon. In this region, winter monsoon conditions lead to distinctive changes in surface water properties, affecting marine plankton communities that are deposited in the sediment. Using planktic foraminifera as a sensitive and well-preserved plankton group, we first characterize the response of their species distribution on environmental gradients from a dataset of surface sediment samples in the tropical and sub-tropical Indian Ocean. Transfer functions for quantitative paleoenvironmental reconstructions were applied to a decadal-scale record of assemblage counts from the Pakistan Margin spanning the last 2000 years. The reconstructed temperature record reveals an intensification of winter monsoon intensity near the year 100 CE. Prior to this transition, winter temperatures were 〉1.5°C warmer than today. Conditions similar to the present seem to have established after 450 CE, interrupted by a singular event near 950 CE with warmer temperatures and accordingly weak winter monsoon. Frequency analysis revealed significant 75-, 40-, and 37-year cycles, which are known from decadal- to centennial-scale resolution records of Indian summer monsoon variability and interpreted as solar irradiance forcing. Our first independent record of Indian winter monsoon activity confirms that winter and summer monsoons were modulated on the same frequency bands and thus indicates that both monsoon systems are likely controlled by the same driving force.
    Type: Dataset
    Format: application/zip, 5 datasets
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  • 10
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    PANGAEA
    In:  Supplement to: Böll, Anna; Lückge, Andreas; Munz, Philipp; Forke, Sven; Schulz, Hartmut; Ramaswamy, Venkitasubramani; Rixen, Tim; Gaye, Birgit; Emeis, Kay-Christian (2014): Late Holocene primary productivity and sea surface temperature variations in the northeastern Arabian Sea: Implications for winter monsoon variability. Paleoceanography, 29(8), 778-794, https://doi.org/10.1002/2013PA002579
    Publication Date: 2024-01-02
    Description: Variability in the oceanic environment of the Arabian Sea region is strongly influenced by the seasonal monsoon cycle of alternating wind directions. Prominent and well studied is the summer monsoon, but much less is known about late Holocene changes in winter monsoon strength with winds from the northeast that drive convective mixing and high surface ocean productivity in the northeastern Arabian Sea. To establish a high-resolution record of winter monsoon variability for the late Holocene, we analyzed alkenone-derived sea surface temperature (SST) variations and proxies of primary productivity (organic carbon and d15N) in a well-laminated sediment core from the Pakistan continental margin. Weak winter monsoon intensities off Pakistan are indicated from 400 B.C. to 250 A.D. by reduced productivity and relatively high SST. At about 250 A.D., the intensity of the winter monsoon increased off Pakistan as indicated by a trend to lower SST. We infer that monsoon conditions were relatively unstable from ~500 to 1300 A.D., because primary production and SST were highly variable. Declining SST and elevated biological production from 1400 to 1900 A.D. suggest invigorated convective winter mixing by strengthening winter monsoon circulation, most likely a regional expression of colder climate conditions during the Little Ice Age on the Northern Hemisphere. The comparison of winter monsoon intensity with records of summer monsoon intensity suggests that an inverse relationship between summer and winter monsoon strength exists in the Asian monsoon system during the late Holocene, effected by shifts in the Intertropical Convergence Zone.
    Type: Dataset
    Format: application/zip, 5 datasets
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