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  • 1
    Publication Date: 2023-12-07
    Description: Dinoflagellate cysts are useful for reconstructing upper water conditions. For adequate reconstructions detailed information is required about the relationship between modern day environmental conditions and the geographic distribution of cysts in sediments. This Atlas summarises the modern global distribution of 71 organicwalled dinoflagellate cyst species. The synthesis is based on the integration of literature sources together with data of 2405 globally distributed surface sediment samples that have been preparedwith a comparable methodology and taxonomy. The distribution patterns of individual cyst species are being comparedwith environmental factors that are knownto influence dinoflagellate growth, gamete production, encystment, excystment and preservation of their organic-walled cysts: surface water temperature, salinity, nitrate, phosphate, chlorophyll-a concentrations and bottom water oxygen concentrations. Graphs are provided for every species depicting the relationship between seasonal and annual variations of these parameters and the relative abundance of the species. Results have been compared with previously published records; an overview of the ecological significance as well as information about the seasonal production of each individual species is presented. The relationship between the cyst distribution and variation in the aforementioned environmental parameters was analysed by performing a canonical correspondence analysis. All tested variables showed a positive relationship on the 99% confidence level. Sea-surface temperature represents the parameter corresponding to the largest amount of variance within the dataset (40%) followed by nitrate, salinity, phosphate and bottom-water oxygen concentration, which correspond to 34%, 33%, 25% and 24% of the variance, respectively. Characterisations of selected environments as well as a discussion about how these factors could have influenced the final cyst yield in sediments are included.
    Keywords: Alexandrium tamarense; Ataxiodinium choane; Bitectatodinium spongium; Bitectatodinium tepikiense; Brigantedinium spp.; Calculated; Caspidinium rugosum; Center for Marine Environmental Sciences; Chlorophyll a, interpolated; Cryodinium meridianum; Dalella chathamensis; DEPTH, sediment/rock; Dinoflagellate cyst; Dinoflagellate cyst, reworked; Dissolved oxygen, in water, interpolated; Dubridinium caperatum; Echinidinium aculeatum; Echinidinium bispiniformum; Echinidinium delicatum; Echinidinium granulatum; Echinidinium karaense; Echinidinium spp.; Echinidinium transparantum; Glaphyrocysta semitecta; Gymnodinium catenatum; Gymnodinium nolleri; Impagidinium aculeatum; Impagidinium caspienense; Impagidinium pallidum; Impagidinium paradoxum; Impagidinium patulum; Impagidinium plicatum; Impagidinium sphaericum; Impagidinium strialatum; Impagidinium variaseptum; Impagidinium velorum; Islandinium cezare; Islandinium minutum; LATITUDE; Lejeunecysta oliva; Lejeunecysta sabrina; Lingulodinium machaerophorum; LONGITUDE; MARUM; Nematosphaeropsis labyrinthus; Nitrate, in water, interpolated; Operculodinium centrocarpum; Operculodinium israelianum; Operculodinium janduchenei; Operculodinium longispinigerum; Operculodinium spp.; Pentapharsodinium dalei; Peridinium ponticum; Phosphate, in water, interpolated; Polykrikos kofoidii; Polykrikos schwarzii; Polykrikos var. arctica; Polysphaeridium zoharyi; Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas; Protoperidiniaceae; Protoperidinium americanum; Protoperidinium monospinum; Pyxidinopsis psilata; Pyxidinopsis reticulata; Quinquecuspis concreta; Reference/source; Selenopemphix antarctica; Selenopemphix nephroides; Selenopemphix quanta; Spiniferites bentori; Spiniferites cruciformis; Spiniferites delicatus; Spiniferites elongatus; Spiniferites lazus; Spiniferites membranaceus; Spiniferites mirabilis; Spiniferites pachydermus; Spiniferites ramosus; Spiniferites spp.; SPP1158; Station label; Stelladinium robustum; Stelladinium stellatum; Tectatodinium pellitum; Temperature, annular; Temperature, autumn; Temperature, spring; Temperature, summer; Temperature, winter; Trinovantedinium applanatum; Tuberculodinium vancampoae; Uniform resource locator/link to file; Votadinium calvum; Votadinium spinosum; Xandarodinium xanthum
    Type: Dataset
    Format: text/tab-separated-values, 230152 data points
    Location Call Number Limitation Availability
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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
    Location Call Number Limitation Availability
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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
    Location Call Number Limitation Availability
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  • 4
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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
    Location Call Number Limitation Availability
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  • 5
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    PANGAEA
    In:  Supplement to: Munz, Philipp; Lückge, Andreas; Siccha, Michael; Böll, Anna; Forke, Sven; Kucera, Michal; Schulz, Hartmut (2016): The Indian winter monsoon and its response to external forcing over the last two and a half centuries. Climate Dynamics, https://doi.org/10.1007/s00382-016-3403-1
    Publication Date: 2024-01-02
    Description: The Indian winter monsoon (IWM) is a key component of the seasonally changing monsoon system that affects the densely populated regions of South Asia. Cold winds originating in high northern latitudes provide a link of continental-scale Northern Hemisphere climate to the tropics. Western Disturbances (WD) associated with the IWM play a critical role for the climate and hydrology in northern India and the western Himalaya region. It is vital to understand the mechanisms and teleconnections that influence IWM variability to better predict changes in future climate. Here we present a study of regionally calibrated winter (January) temperatures and according IWM intensities, based on a planktic foraminiferal record with biennial (2.55 years) resolution. Over the last ~250 years, IWM intensities gradually weakened, based on the long-term trend of reconstructed January temperatures. Furthermore, the results indicate that IWM is connected on interannual- to decadal time scales to climate variability of the tropical and extratropical Pacific, via El Niño Southern Oscillation (ENSO) and Pacific Decadal Oscillation (PDO). However, our findings suggest that this relationship appeared to begin to decouple since the beginning of the 20th century. Cross-spectral analysis revealed that several distinct decadal-scale phases of colder climate and accordingly more intense winter monsoon centered at the years ~1800, ~1890 and ~1930 can be linked to changes of the North Atlantic Oscillation (NAO).
    Keywords: Arabian Sea; BCR; Box corer (Reineck); PAKOMIN; SO90; SO90_39KG; Sonne
    Type: Dataset
    Format: application/zip, 2 datasets
    Location Call Number Limitation Availability
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  • 6
    Publication Date: 2024-01-02
    Keywords: Age; AGE; Arabian Sea; BCR; Box corer (Reineck); Calculated moving averages; DEPTH, sediment/rock; Event label; KL; MAKRAN 2; Mass spectrometer Finnigan MAT 252; PAKOMIN; Piston corer (BGR type); SO130; SO130_275KL; SO90; SO90_39KG; Sonne; δ15N
    Type: Dataset
    Format: text/tab-separated-values, 500 data points
    Location Call Number Limitation Availability
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  • 7
    Publication Date: 2024-01-02
    Keywords: Age; AGE; Arabian Sea; BCR; Box corer (Reineck); Carbon, organic, total; DEPTH, sediment/rock; Element analyser CNS, Carlo Erba NA1500; Event label; KL; MAKRAN 2; PAKOMIN; Piston corer (BGR type); SO130; SO130_275KL; SO90; SO90_39KG; Sonne
    Type: Dataset
    Format: text/tab-separated-values, 554 data points
    Location Call Number Limitation Availability
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  • 8
    Publication Date: 2024-01-02
    Keywords: Age; AGE; Arabian Sea; BCR; Box corer (Reineck); Calcium carbonate; Carbonate/opal ratio; DEPTH, sediment/rock; Event label; Index; KL; MAKRAN 2; Opal, biogenic silica; PAKOMIN; Piston corer (BGR type); SO130; SO130_275KL; SO90; SO90_39KG; Sonne
    Type: Dataset
    Format: text/tab-separated-values, 415 data points
    Location Call Number Limitation Availability
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  • 9
    Publication Date: 2024-01-02
    Keywords: Age; AGE; Arabian Sea; BCR; Beella digitata; Box corer (Reineck); Counting 〉150 µm fraction; Dentagloborotalia anfracta; DEPTH, sediment/rock; Foraminifera, planktic, other; Globigerina bulloides; Globigerina falconensis; Globigerina hexagona; Globigerinella calida; Globigerinella siphonifera; Globigerinita glutinata; Globigerinoides conglobatus; Globigerinoides ruber white; Globigerinoides sacculifer sac; Globigerinoides sacculifer trilobus; Globorotalia hirsuta; Globorotalia menardii; Globorotalia scitula; Globoturborotalita rubescens; Globoturborotalita tenella; Neogloboquadrina dutertrei; Neogloboquadrina pachyderma sinistral; Orbulina universa; PAKOMIN; Pulleniatina obliquiloculata; SO90; SO90_39KG; Sonne; Turborotalita iota; Turborotalita quinqueloba; Δ depth
    Type: Dataset
    Format: text/tab-separated-values, 2626 data points
    Location Call Number Limitation Availability
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  • 10
    Publication Date: 2024-01-02
    Keywords: Age; AGE; Arabian Sea; BCR; Box corer (Reineck); DEPTH, sediment/rock; PAKOMIN; Root mean square error of prediction; Sea surface temperature, January anomaly; SO90; SO90_39KG; Sonne; Δ depth
    Type: Dataset
    Format: text/tab-separated-values, 404 data points
    Location Call Number Limitation Availability
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