GLORIA

GEOMAR Library Ocean Research Information Access

feed icon rss

Your email was sent successfully. Check your inbox.

An error occurred while sending the email. Please try again.

Proceed reservation?

Export
Filter
Document type
Keywords
Language
  • 1
    Online Resource
    Online Resource
    San Diego :Elsevier,
    Keywords: Coastal zone management-Indonesia. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (484 pages)
    Edition: 1st ed.
    ISBN: 9780128150511
    DDC: 577.5109598
    Language: English
    Note: Front Cover -- Science for the Protection of Indonesian Coastal Ecosystems (SPICE) -- Science for the Protection of Indonesian Coastal Ecosystems (SPICE) -- Copyright -- Contents -- Contributors -- Reviewers -- Foreword -- 1 - Introduction-Science for the Protection of Indonesian Coastal Ecosystems (SPICE) -- 1.1 Rationale -- 1.2 Development and implementation of the research and education program SPICE -- 1.3 Research, education, and outreach activities -- 1.4 Summary and synthesis of SPICE results -- Acknowledgments -- References -- 2 - Physical environment of the Indonesian Seas with focus on the western region -- 2.1 Introduction -- 2.2 The marine circulation -- 2.2.1 The global context -- 2.2.2 The regional circulation -- 2.2.3 Tides -- 2.3 Seasonal variability and long-term changes -- 2.3.1 Seasonality of circulation -- 2.3.2 Seasonality of temperature and salinity -- 2.3.3 Long-term development of sea surface temperature and sea surface salinity -- 2.4 Water residence times -- 2.5 Sources and sinks of freshwater -- 2.6 Remote sensing methods applied in coastal process studies -- 2.6.1 Available satellite data -- 2.6.2 Ocean color and its variation in Indonesian coastal waters -- 2.6.3 Satellite-based studies of phytoplankton and coastal processes -- 2.6.3.1 Distribution of phytoplankton -- 2.6.3.2 Coastal discharge and influence of tidal and monsoon phases -- 2.6.3.3 Climatological aspects -- Acknowledgments -- References -- 3 - Human interventions in rivers and estuaries of Java and Sumatra -- 3.1 Introduction -- 3.2 Drivers of environmental change affecting river fluxes -- 3.3 Natural factors, human interventions, and extreme events controlling river fluxes -- 3.3.1 The Brantas River, Java, as an example of high suspended matter rivers -- 3.3.1.1 Variations in sources, composition, and fate of nutrients. , 3.3.1.2 Variations in sources, composition, and fate of suspended sediments and particulate organic matter -- 3.3.1.3 Effects on phytoplankton abundance and community composition -- 3.3.1.4 Effects on the dissolved oxygen regime of the lower Brantas -- 3.3.2 The Siak River, Sumatra, as an example of blackwater rivers -- 3.3.2.1 Variations in dissolved organic carbon and dissolved oxygen -- 3.3.2.2 Sources and fate of nutrients -- 3.4 Governance and management programs -- Acknowledgments -- References -- 4 - Carbon cycle in tropical peatlands and coastal seas -- 4.1 Introduction -- 4.2 Background information -- 4.2.1 Peat -- 4.2.2 Peatland types -- 4.2.3 Vegetation and biodiversity -- 4.2.4 Peatland distribution and carbon storage -- 4.3 Indonesian peatlands -- 4.3.1 History of Indonesian peat swamps -- 4.3.2 Peat properties -- 4.3.3 Peat carbon accumulation -- 4.3.4 Land use and cover changes in Indonesia -- 4.3.5 The hydrological cycle of Indonesian peatlands -- 4.4 Peat carbon losses -- 4.4.1 CO2 emissions caused by peat and forest fires -- 4.4.2 CO2 emissions caused by peat soil oxidations -- 4.4.3 Off-site CO2 emission -- 4.5 Land-ocean continuum -- 4.5.1 SPICE study area -- 4.5.2 Dissolved organic carbon -- 4.5.3 Dissolved organic carbon yields -- 4.5.4 CO2 emission from rivers -- 4.5.5 Dissolved inorganic carbon yields -- 4.5.6 Leaching and erosion -- 4.5.7 Priming -- 4.6 Estuaries and the ocean -- 4.6.1 Dissolved organic carbon -- 4.6.1.1 The microbial organic carbon pump in the ocean -- 4.6.1.2 Dissolved organic carbon discharges into the ocean -- 4.6.1.3 The fate of dissolved organic carbon in the ocean -- 4.6.2 CO2 emissions from the coastal ocean -- 4.6.3 Organic carbon burial -- 4.6.4 The invisible carbon footprint -- 4.6.5 The marine peat carbon budget -- 4.6.6 Emission factors -- 4.7 Ecosystem CO2 emissions. , 4.7.1 Net on-site ecosystem CO2 exchange -- 4.7.2 CO2 emission from pristine peat swamps -- 4.7.3 CO2 emission from disturbed peatlands -- 4.8 Evaluation of CO2 emissions -- 4.8.1 Climate response to cumulative emissions of CO2 -- 4.8.2 CO2 reduction potential -- 4.8.3 CO2 emissions and land losses -- 4.8.4 Climate pledges and gaps -- 4.9 Socioeconomic implications -- 4.9.1 REDD+ -- 4.9.2 SPICE field experiments -- 4.10 Outlook -- References -- 5 - Coral reef social-ecological systems under pressure in Southern Sulawesi -- 5.1 Introduction-coral reefs in Indonesia and the Spermonde Archipelago -- 5.2 Functioning of coral reefs -- 5.2.1 Water quality and biogeochemical processes -- 5.2.2 Benthic coral reef community dynamics of Spermonde Archipelago -- 5.2.3 Bacterial communities and biofilms -- 5.2.4 Coral reef recruitment processes -- 5.2.5 Coral physiology -- 5.2.6 Relationships between benthic and fish communities -- 5.2.7 Consequences of disturbances for coral reef functioning -- 5.3 Genetic connectivity of reefs in the Coral Triangle region -- 5.3.1 Large-scale connectivity across the Coral Triangle region -- 5.3.2 Small-scale connectivity in the Spermonde Archipelago -- 5.3.3 Self-recruitment at the islands of Barrang Lompo and Samalona -- 5.3.4 Application of connectivity data in marine-protected area network design -- 5.4 Social systems associated with the use of coral-based resources and reef-specific challenges -- 5.4.1 Participatory assessment of Spermonde's coral reef fisheries -- 5.4.2 Investigating marine social-ecological feedbacks and dynamics -- 5.4.3 Reef-related livelihoods and implications for the present and future health of fishers and reefs -- 5.4.4 Changing target species, perceptions of reef resources, and implications for food security. , 5.4.5 Conclusions for the management of coral reef resources in the Spermonde Archipelago -- 5.5 Modeling to support the management of reef systems -- 5.5.1 Simulating the impact of fisheries on coral reef dynamics -- 5.5.2 A model on gear choices of fishermen -- 5.5.3 Spatial patterns of fishing ground distribution -- 5.6 Summary and outlook -- Acknowledgments -- References -- Appendix A5 -- 6 - Ecology of seagrass beds in Sulawesi-Multifunctional key habitats at the risk of destruction -- 6.1 General introduction to tropical Southeast Asian seagrass meadows -- 6.1.1 High biodiversity of seagrasses in the coral triangle of the tropical Indo-West Pacific -- 6.1.2 Introduction to the Spermonde Archipelago and its seagrasses and mangroves -- 6.2 The current distribution of seagrasses in the Spermonde Archipelago -- 6.2.1 Area estimates and seagrass mapping -- 6.2.2 The structure of tropical seagrass bed systems -- 6.3 Seagrass ecology -- 6.3.1 The historic loss of megaherbivores and today's important role of burrowing shrimp -- 6.3.2 Macrobenthic communities -- 6.3.3 The food web and the trophic pyramid in tropical seagrass beds -- 6.3.4 The function of seagrass meadows as water filters and buffers for land runoff -- 6.3.5 Carbon storage -- 6.3.6 Seagrass beds as carbon sinks -- 6.3.7 Trophic transfers from seagrass meadows to nearby ecosystems -- 6.4 Tropical seagrass beds as key habitat for fish species -- 6.4.1 Tropical seagrasses and their associated fish communities -- 6.4.2 The seagrass canopy as a driver of fish communities -- 6.4.3 Differences in fish habitat utilization across seagrass meadows with distinct canopy structures -- 6.5 Human-seagrass interactions -- 6.5.1 Ecological value and ecosystem services -- 6.5.2 Fisheries on fish and invertebrates in seagrass beds -- 6.5.3 Seaweed farms -- 6.5.4 Human-made infrastructure. , 6.5.5 Current threats -- 6.6 Conclusions and outlook -- Acknowledgments -- References -- 7 - Mangrove ecosystems under threat in Indonesia: the Segara Anakan Lagoon, Java, and other examples -- 7.1 Introduction -- 7.2 The study areas -- 7.3 Environmental setting and natural resource use -- 7.3.1 The physical setting -- 7.3.2 Water quality, biogeochemistry, and pollution -- 7.3.3 Carbon sources and storage -- 7.3.4 Flora and fauna -- 7.3.5 Population and natural resource use in the Segara Anakan region -- 7.4 Environmental change in the Segara Anakan Lagoon region: causes, drivers, and impacts -- 7.4.1 Decline of marine species and fisheries -- 7.4.2 Sedimentation and its causes -- 7.4.3 Reclamation of land and conflicts over new land -- 7.5 Threats to mangrove forests and their ecosystem services in Indonesia -- 7.6 Management programs -- Acknowledgments -- References -- 8 - Impact of megacities on the pollution of coastal areas-the case example Jakarta Bay -- 8.1 Introduction -- 8.2 Hydrological system and nutrient dispersion -- 8.3 Organic and inorganic pollution in Jakarta Bay -- 8.3.1 Types, quantity, and distribution of pollutants -- 8.3.1.1 Trace hazardous elements -- 8.3.1.2 Organic pollutants -- 8.3.2 Characterizing emission sources -- 8.3.2.1 Source apportionment of trace elements -- 8.3.2.2 The insect repellent N,N-diethyl-m-toluamide as tracer for municipal sewage and the implications for coastal management -- 8.3.3 Industrial emissions in the Greater Jakarta area and their role for the contamination of the Jakarta Bay ecosystem -- 8.3.4 The flushing-out phenomenon -- 8.3.5 Accumulation in biota -- 8.4 Water quality and biological responses -- 8.4.1 Water pollution in Jakarta Bay and the Thousand Islands -- 8.4.2 Biological responses to anthropogenic stressors -- 8.4.3 Impacts on the physiology of key coral reef organisms. , 8.4.4 Impacts on reef composition.
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 2
    Keywords: Marine bacteria. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (208 pages)
    Edition: 1st ed.
    ISBN: 9780128151662
    DDC: 579.177
    Language: English
    Note: Front Cover -- Microbial Communities in Coastal Sediments -- Copyright Page -- Contents -- Introduction -- 1 Source and composition of organic matter and its role in designing sediment microbial communities -- 1.1 Introduction -- 1.2 Organic matter in coastal sediments -- 1.2.1 Types of sedimentary organic matter -- 1.2.1.1 Total organic matter/total organic carbon -- 1.2.1.2 Particulate organic matter/particulate organic carbon -- 1.2.1.3 Dissolved organic matter/dissolved organic carbon -- 1.2.1.4 Dissolved inorganic carbon -- 1.2.1.5 Labile organic matter -- 1.2.1.6 Refractory organic matter -- 1.2.1.7 Microbial biomass carbon -- 1.2.1.8 Biopolymeric carbon -- 1.3 Source of organic matter: autochthonous and allochthonous -- 1.3.1 Autochthonous organic matter -- 1.3.2 Allochthonous organic matter -- 1.3.2.1 Transport by rivers -- 1.3.2.2 Agricultural and urban runoff -- 1.4 Quality of organic matter in sediments -- 1.4.1 Organic matter quality indices -- 1.5 Microbial degradation of organic matter -- 1.6 Role of organic matter in designing sediment microbial communities -- 1.7 Microbial diversity and ecology in coastal sediments -- 1.7.1 Diversity of bacterial communities -- 1.7.1.1 Hydrolytic bacteria -- 1.7.1.2 Denitrifying bacteria -- 1.7.1.3 Iron and manganese reducers -- 1.7.1.4 Sulfate reducers -- 1.8 Diversity of archaeal communities -- 1.8.1 Methanogenic archaea -- References -- 2 Sources, types, and effects of nutrients (N and P) in coastal sediments -- 2.1 Introduction -- 2.2 Nutrient sources of coastal ecosystems -- 2.2.1 Agriculture -- 2.2.2 Animal husbandry and marine aquaculture -- 2.2.3 Fossil fuel burning and atmospheric deposition -- 2.3 Nutrient enrichment: forms and types -- 2.4 Effect of hypernutrification -- 2.4.1 Eutrophication and consequences for ecology -- 2.4.2 Hypoxia and anoxia in water and sediment. , 2.4.3 Eutrophication-induced changes in sediment microbial communities -- References -- 3 Environmental variables and factors regulating microbial structure and functions -- 3.1 Introduction -- 3.2 Spatial and temporal heterogeneity -- 3.3 Geological factors -- 3.3.1 Sediment granulometry -- 3.3.2 Sediment depth -- 3.3.2.1 Shift in substrate availability with depth -- 3.3.2.2 Decrease in lability of organic matter with depth -- 3.4 Hydrological factors -- 3.5 Physicochemical factors -- 3.5.1 pH -- 3.5.2 Salinity -- 3.5.3 Pore water chemistry/presence of nutrients or chemicals -- 3.5.4 Redox potential -- 3.5.5 Changes in availability of electron acceptors -- 3.5.5.1 Aerobic respiration -- 3.5.5.2 Nitrate reduction -- 3.5.5.3 Mn and Fe reduction -- 3.5.5.4 Sulfate reduction -- 3.5.5.5 Methanogenesis -- 3.5.6 Role of electron donors -- 3.6 Biological factors -- 3.6.1 Trophic interactions -- 3.6.1.1 Syntrophy and interspecies hydrogen transfer -- 3.6.2 Evolutionary mechanisms and diversification -- 3.6.3 Ecological coherence -- 3.6.4 Microbial characteristics -- 3.6.5 Bioturbation and ventilation -- 3.6.6 Plant interactions -- 3.7 Nutritional factors -- 3.8 Natural and anthropogenic disturbances -- 3.9 Presence of contaminants/toxic substances -- References -- 4 Biogeocycling of nutrients (C, N, P, S, and Fe) and implications on greenhouse gas emissions -- 4.1 Introduction -- 4.2 Biogeocycling of nutrients -- 4.2.1 Carbon -- 4.2.2 Nitrogen -- 4.2.3 Sulfur -- 4.2.4 Manganese (Mn) and iron (Fe) -- 4.3 Greenhouse gas dynamics in coastal ecosystems -- 4.3.1 Carbon dioxide -- 4.3.2 Methane -- 4.3.3 Nitrous oxide -- References -- 5 Biodegradation and biotransformation of persistent organic pollutants by microbes in coastal sediments -- 5.1 Introduction -- 5.2 Why persistent organic pollutants? -- 5.3 Anaerobic degradation and pathways. , 5.3.1 Phenols and chlorinated phenols -- 5.3.2 3-Chlorobenzoate -- 5.3.3 Polycyclic aromatic hydrocarbons -- 5.3.4 Polychlorinated biphenyls -- 5.3.5 Polychlorinated dibenzo-p-dioxins and dibenzofurans -- 5.4 Anaerobic microorganisms involved -- 5.5 Limitations for anaerobic degradation: electron acceptors -- 5.6 Future prospects -- References -- 6 Assessment of microbial structure and functions in coastal sediments -- 6.1 Introduction -- 6.2 Culture-dependent methods: the "great plate count anomaly" -- 6.3 Molecular tools used to examine microbial diversity of coastal sediments -- 6.3.1 Gene amplification and sequencing of 16S rDNA -- 6.3.2 Fluorescence in situ hybridization -- 6.3.3 Terminal restriction fragment length polymorphism -- 6.3.4 Denaturing gradient gel electrophoresis/temperature gradient gel electrophoresis -- 6.4 High-throughput sequencing technologies -- 6.4.1 Metagenomics: an approach based on small subunit ribosomal RNA -- 6.5 Functional diversity of coastal sediment microbes -- 6.5.1 Stable isotope probing -- 6.6 Microbial activity in coastal sediment: study of biogeochemical reaction rates in laboratory microcosms -- 6.7 Conclusion and future prospects -- References -- Appendix 1: Conclusions and future perspectives -- Index -- Back Cover.
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 3
    Keywords: Forschungsbericht ; Mangrove
    Type of Medium: Online Resource
    Pages: 1 Online-Ressource (99 Seiten, 6,58 MB) , Illustrationen, Diagramme, Karten
    Language: German
    Note: Förderkennzeichen BMBF 03F0644A-C. - Verbund-Nummer 01108427 , Unterschiede zwischen dem gedruckten Dokument und der elektronischen Ressource können nicht ausgeschlossen werden
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 4
    facet.materialart.
    Unknown
    Nature Research
    In:  Nature Communications, 8 (1). Art.Nr. 1015.
    Publication Date: 2020-02-06
    Description: Changes in tropical zonal atmospheric (Walker) circulation induce shifts in rainfall patterns along with devastating floods and severe droughts that dramatically impact the lives of millions of people. Historical records and observations of the Walker circulation over the 20th century disagree on the sign of change and therefore, longer climate records are necessary to better project tropical circulation changes in response to global warming. Here we examine proxies for thermocline depth and rainfall in the eastern tropical Indian Ocean during the globally colder Last Glacial Maximum (19–23 thousand years ago) and for the past 3000 years. We show that increased thermocline depth and rainfall indicate a stronger-than-today Walker circulation during the Last Glacial Maximum, which is supported by an ensemble of climate simulations. Our findings underscore the sensitivity of tropical circulation to temperature change and provide evidence for a further weakening of the Walker circulation in response to greenhouse warming.
    Type: Article , PeerReviewed
    Format: text
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 5
    Publication Date: 2019-07-15
    Description: Mangrove ecosystems are an important natural carbon sink that accumulate and store large amounts of organic carbon (Corg), in particular in the sediment. However, the magnitude of carbon stocks and the rate of carbon accumulation (CAR) vary geographically due to a large variation of local factors. In order to better understand the blue carbon sink of mangrove ecosystems, we measured organic carbon stocks, sources and accumulation rates in three Indonesian mangrove ecosystems with different environmental settings and conditions; (i) a degraded estuarine mangrove forest in the Segara Anakan Lagoon (SAL), Central Java, (ii) an undegraded estuarine mangrove forest in Berau region, East Kalimantan, and (iii) a pristine marine mangrove forest on Kongsi Island, Thousand Islands, Jakarta. In general, Corg stocks were higher in estuarine than in marine mangroves, although a large variation was observed among the estuarine mangroves. The mean total Corg stock in Berau (615 ± 181 Mg C ha−1) is twice as high as that in SAL (298 ± 181 Mg C ha−1). However, the Segara Anakan Lagoon displayed large within-system variation with a much higher Corg stock in the eastern (483 ± 124 Mg C ha−1) than in the central lagoon (167 ± 36 Mg C ha−1). The predominant accumulation of autochthonous mangrove organic matter likely contributed to the higher Corg stocks in Berau and the eastern SAL. Interestingly, the CAR distribution pattern in SAL is opposite to that of its Corg stocks. The central SAL that receives high sediment inputs from the hinterland has a much higher CAR than the eastern SAL (658 ± 311 g C m−2 yr−1 and 194 ± 46 g C m−2 yr−1, respectively), while Berau has one of the highest CAR (1722 ± 183 g C m−2 yr−1) ever measured. It appears that these large differences are driven by the environmental setting and conditions, mainly sediment dynamics and hydrodynamics, landform, and vegetation conditions. It is inferred that quantifying carbon accumulation in sediments is a useful tool in estimating the present-day carbon storage of mangrove ecosystems. This is a precondition for taking measures under REDD+ (Reducing Emissions from Deforestation and Forest Degradation and the role of conservation, sustainable management of forests and enhancement of forest carbon stocks in developing countries) schemes.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
    Format: application/pdf
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 6
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Baumgart, Anne; Jennerjahn, Tim C; Mohtadi, Mahyar; Hebbeln, Dierk (2010): Distribution and burial of organic carbon in sediments from the Indian Ocean upwelling region off Java and Sumatra, Indonesia. Deep Sea Research Part I: Oceanographic Research Papers, 57(3), 458-467, https://doi.org/10.1016/j.dsr.2009.12.002
    Publication Date: 2023-03-03
    Description: Sediments were sampled and oxygen profiles of the water column were determined in the Indian Ocean off west and south Indonesia in order to obtain information on the production, transformation, and accumulation of organic matter (OM). The stable carbon isotope composition (d13Corg) in combination with C/N ratios depicts the almost exclusively marine origin of sedimentary organic matter in the entire study area. Maximum concentrations of organic carbon (Corg) and nitrogen (N) of 3.0% and 0.31%, respectively, were observed in the northern Mentawai Basin and in the Savu and Lombok basins. Minimum d15N values of 3.7 per mil were measured in the northern Mentawai Basin, whereas they varied around 5.4 per mil at stations outside this region. Minimum bottom water oxygen concentrations of 1.1 mL L**1, corresponding to an oxygen saturation of 16.1%, indicate reduced ventilation of bottom water in the northern Mentawai Basin. This low bottom water oxygen reduces organic matter decomposition, which is demonstrated by the almost unaltered isotopic composition of nitrogen during early diagenesis. Maximum Corg accumulation rates (CARs) were measured in the Lombok (10.4 g C m**-2 yr**-1) and northern Mentawai basins (5.2 g C m**-2 yr**-1). Upwelling-induced high productivity is responsible for the high CAR off East Java, Lombok, and Savu Basins, while a better OM preservation caused by reduced ventilation contributes to the high CAR observed in the northern Mentawai Basin. The interplay between primary production, remineralisation, and organic carbon burial determines the regional heterogeneity. CAR in the Indian Ocean upwelling region off Indonesia is lower than in the Peru and Chile upwellings, but in the same order of magnitude as in the Arabian Sea, the Benguela, and Gulf of California upwellings, and corresponds to 0.1-7.1% of the global ocean carbon burial. This demonstrates the relevance of the Indian Ocean margin off Indonesia for the global OM burial.
    Keywords: Center for Marine Environmental Sciences; GeoB10008-4; GeoB10010-1; GeoB10014-1; GeoB10015-1; GeoB10016-2; GeoB10022-6; GeoB10024-3; GeoB10025-3; GeoB10026-2; GeoB10027-3; GeoB10028-4; GeoB10029-3; GeoB10031-3; GeoB10033-5; GeoB10034-3; GeoB10036-3; GeoB10037-2; GeoB10038-3; GeoB10039-3; GeoB10040-3; GeoB10041-3; GeoB10042-2; GeoB10043-2; GeoB10044-3; GeoB10047-1; GeoB10049-5; GeoB10050-1; GeoB10058-1; GeoB10059-1; GeoB10061-4; GeoB10063-5; GeoB10064-5; GeoB10065-9; GeoB10066-6; GeoB10067-5; GeoB10068-2; GeoB10069-4; GeoB10070-6; MARUM; MUC; MultiCorer; PABESIA; SO184/1; SO184/2; Sonne
    Type: Dataset
    Format: application/zip, 2 datasets
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 7
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Contreras-Rosales, Lorena Astrid; Jennerjahn, Tim C; Tharammal, Thejna; Meyer, Vera D; Lückge, Andreas; Paul, André; Schefuß, Enno (2014): Evolution of the Indian Summer Monsoon and terrestrial vegetation in the Bengal region during the past 18 ka. Quaternary Science Reviews, 102, 133-148, https://doi.org/10.1016/j.quascirev.2014.08.010
    Publication Date: 2023-03-03
    Description: The Indian Summer Monsoon (ISM) is a major global climatic phenomenon. Long-term precipitation proxy records of the ISM, however, are often fragmented and discontinuous, impeding an estimation of the magnitude of precipitation variability from the Last Glacial to the present. To improve our understanding of past ISM variability, we provide a continuous reconstructed record of precipitation and continental vegetation changes from the lower Ganges-Brahmaputra-Meghna catchment and the Indo-Burman ranges over the last 18,000 years (18 ka). The records derive from a marine sediment core from the northern Bay of Bengal (NBoB), and are complemented by numerical model results of spatial moisture transport and precipitation distribution over the Bengal region. The isotopic composition of terrestrial plant waxes (dD and d13C of n-alkanes) are compared to results from an isotope-enabled general atmospheric circulation model (IsoCAM) for selected time slices (pre-industrial, mid-Holocene and Heinrich Stadial 1). Comparison of proxy and model results indicate that past changes in the dD of precipitation and plant waxes were mainly driven by the amount effect, and strongly influenced by ISM rainfall. Maximum precipitation is detected for the Early Holocene Climatic Optimum (EHCO; 10.5-6 ka BP), whereas minimum precipitation occurred during the Heinrich Stadial 1 (HS1; 16.9-15.4 ka BP). The IsoCAM model results support the hypothesis of a constant moisture source (i.e. the NBoB) throughout the study period. Relative to the pre-industrial period the model reconstructions show 20% more rain during the mid-Holocene (6 ka BP) and 20% less rain during the Heinrich Stadial 1 (HS1), respectively. A shift from C4-plant dominated ecosystems during the glacial to subsequent C3/C4-mixed ones during the interglacial took place. Vegetation changes were predominantly driven by precipitation variability, as evidenced by the significant correlation between the dD and d13C alkane records. When compared to other records across the ISM domain, precipitation and vegetation changes inferred from our records and the numerical model results provide evidence for a coherent regional variability of the ISM from the Last Glacial to the present.
    Keywords: Center for Marine Environmental Sciences; Leibniz Centre for Tropical Marine Research; MARUM; ZMT
    Type: Dataset
    Format: application/zip, 2 datasets
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 8
    Publication Date: 2023-03-03
    Keywords: Accumulation rate, mass; Accumulation rate, total organic carbon; Carbon, organic, total; Center for Marine Environmental Sciences; Chlorophyll a; DEPTH, sediment/rock; Element analyser, Carlo Erba NA2100; Elevation of event; Event label; GeoB10029-3; GeoB10033-5; GeoB10038-3; GeoB10059-1; GeoB10065-9; GeoB10069-4; Latitude of event; Longitude of event; MARUM; MUC; MultiCorer; PABESIA; Sedimentation rate; see reference(s); SO184/1; SO184/2; Sonne
    Type: Dataset
    Format: text/tab-separated-values, 30 data points
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 9
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Contreras-Rosales, Lorena Astrid; Jennerjahn, Tim C; Steinke, Stephan; Mohtadi, Mahyar; Schefuß, Enno (2019): Holocene changes in biome size and tropical cyclone activity around the Northern South China Sea. Quaternary Science Reviews, 215, 45-63, https://doi.org/10.1016/j.quascirev.2019.05.004
    Publication Date: 2023-03-03
    Description: The South China Sea (SCS), characterized by a large continental shelf, is located at the edge of the Asian monsoon domain. In this study, two marine sediment cores from the northern SCS (NSCS) continental slope were investigated to construct composite vegetation and precipitation isotopic composition records based on the δ13C and δD values of plant-wax n-alkanes throughout the Holocene (last 11,200 years; i.e. 11.2 ka). The composite δ13Cwax record indicates an overall predominance of C3 vegetation over the last 11.2 ka. Before 8 ka BP, higher δ13Cwax values are attributed to preferential wax input from grassland and wetland biomes on the exposed continental shelf. After the inundation of the shelf by eustatic sea level rise until ca. 8 ka BP grassland and wetland biomes suffered a major size reduction and arboreal vegetation became better represented in the δ13Cwax record. The composite temperature corrected δDwax-T record suggests that moisture source variability drove precipitation isotopic composition changes during the Holocene. Lower δDwax-T values before 8.3 ka BP are interpreted as a larger moisture contribution by Pacific Ocean tropical cyclones, whereas higher δDwax-T values after 8.5 ka BP are interpreted as a larger moisture contribution from the Indian Ocean summer monsoon. Higher incidence of tropical cyclones in the NSCS during the Early Holocene was related to a temporary westward shift of the Western Pacific Warm Pool and enhanced insolation over the Northern Hemisphere. Both external and internal forcing mechanisms regulated moisture source changes in East Asia during the Holocene.
    Keywords: Center for Marine Environmental Sciences; Leibniz Centre for Tropical Marine Research; MARUM; ZMT
    Type: Dataset
    Format: application/zip, 5 datasets
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 10
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Unger, Daniela; Jennerjahn, Tim C (2009): Impact of regional Indian Ocean characteristics on the biogeochemical variability of settling particles. In: Wiggert, J; Naqvi, SWA; Smith, S; Hood, RR (eds.) Indian Ocean Biogeochemical Processes and Ecological Variability. AGU, Geophysical Monograph Series, 185, 257-280, https://doi.org/10.1029/2008GM000703
    Publication Date: 2023-05-12
    Description: The Asian monsoon system governs seasonality and fundamental environmental characteristics in the study area from which two distinct peculiarities are most notable: upwelling and convective mixing in the Arabian Sea and low surface salinity and stratification in the Bay of Bengal due to high riverine input and monsoonal precipitation. The respective oceanography sets the framework for nutrient availability and productivity. Upwelling ensures high nitrate concentration with temporal/spatial Si limitation; freshwater-induced stratification leads to reduced nitrogen input from the subsurface but Si enrichment in surface waters. Ultimately, both environments support high abundance of diatoms, which play a central role in the export of organic matter. It is speculated that, additional to eddy pumping, nitrogen fixation is a source of N in stratified waters and contributes to the low-d15N signal in sinking particles formed under riverine impact. Organic carbon fluxes are best correlated to opal but not to carbonate, which is explained by low foraminiferal carbonate fluxes within the river-impacted systems. This observation points to the necessity of differentiating between carbonate sources for carbon flux modeling. As evident from a compilation of previously published and new data on labile organic matter composition (amino acids and carbohydrates), organic matter fluxes are mainly driven by direct input from marine production, except the site off Pakistan where sedimentary input of (marine) organic matter is dominant during the NE monsoon. The explanation of apparently different organic carbon export efficiency calls for further investigations of, for example, food web structure and water column processes.
    Keywords: Arabian Sea; Bay of Bengal; CBBT; Center for Marine Environmental Sciences; East Pakistan Trap Station; EIOT; EPT; Equatorial Indian Ocean Trap Station; Indian Ocean; JAM-1; Lakshadweep Sea; MARUM; MOOR; Mooring; NBBT-N; NBBT-S; Northern Bay of Bengal Trap Station - North; Northern Bay of Bengal Trap Station - South; off south Java; SBBT; Southern Bay of Bengal Trap Station; Trap, sediment; TRAPS
    Type: Dataset
    Format: application/zip, 7 datasets
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
Close ⊗
This website uses cookies and the analysis tool Matomo. More information can be found here...