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  • 158-957C; 158-957G; 158-957H; 158-957O; 158-957P; 169-1035F; 169-1035H; 169-1038I; 169-856H; Area/locality; Conductivity, thermal; Dead Dog vent field, North Pacific Ocean; Density, grain; Density, wet bulk; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Elevation of event; Escanaba Trough, North Pacific Ocean; Event label; Joides Resolution; Latitude of event; Leg158; Leg169; Longitude of event; North Pacific Ocean; Ocean Drilling Program; ODP; Piece; Porosity; Sample code/label; Sample comment; South Atlantic Ocean; Volume, porewater  (1)
  • Andaman Sea  (1)
  • Bay of Bengal  (1)
  • CDRILL; Core drilling; DEPTH, sediment/rock; Dispersion parameter; Event label; India National Gas Hydrate Program Expedition 01; Joides Resolution; Magnetic susceptibility; Mass; NGHP-01; NGHP-01-10D; NGHP-01-16A; Parameter; Sample code/label; Saturation isothermal remanent magnetisation; Volume  (1)
  • CDRILL; Core drilling; DEPTH, sediment/rock; Event label; India National Gas Hydrate Program Expedition 01; Iron/susceptibility, volume ratio; Joides Resolution; NGHP-01; NGHP-01-10D; NGHP-01-16A  (1)
Document type
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  • 1
    Publication Date: 2024-01-09
    Keywords: 158-957C; 158-957G; 158-957H; 158-957O; 158-957P; 169-1035F; 169-1035H; 169-1038I; 169-856H; Area/locality; Conductivity, thermal; Dead Dog vent field, North Pacific Ocean; Density, grain; Density, wet bulk; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Elevation of event; Escanaba Trough, North Pacific Ocean; Event label; Joides Resolution; Latitude of event; Leg158; Leg169; Longitude of event; North Pacific Ocean; Ocean Drilling Program; ODP; Piece; Porosity; Sample code/label; Sample comment; South Atlantic Ocean; Volume, porewater
    Type: Dataset
    Format: text/tab-separated-values, 666 data points
    Location Call Number Limitation Availability
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  • 2
    Publication Date: 2024-06-12
    Keywords: CDRILL; Core drilling; DEPTH, sediment/rock; Event label; India National Gas Hydrate Program Expedition 01; Iron/susceptibility, volume ratio; Joides Resolution; NGHP-01; NGHP-01-10D; NGHP-01-16A
    Type: Dataset
    Format: text/tab-separated-values, 346 data points
    Location Call Number Limitation Availability
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  • 3
    Publication Date: 2024-06-12
    Keywords: CDRILL; Core drilling; DEPTH, sediment/rock; Dispersion parameter; Event label; India National Gas Hydrate Program Expedition 01; Joides Resolution; Magnetic susceptibility; Mass; NGHP-01; NGHP-01-10D; NGHP-01-16A; Parameter; Sample code/label; Saturation isothermal remanent magnetisation; Volume
    Type: Dataset
    Format: text/tab-separated-values, 332 data points
    Location Call Number Limitation Availability
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  • 4
    Publication Date: 2022-05-26
    Description: Author Posting. © American Geophysical Union, 2015. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Geochemistry, Geophysics, Geosystems 16 (2015): 505–521, doi:10.1002/2014GC005586.
    Description: The Late Quaternary variability of the South Asian (or Indian) monsoon has been linked with glacial-interglacial and millennial scale climatic changes but past rainfall intensity in the river catchments draining into the Andaman Sea remains poorly constrained. Here we use radiogenic Sr, Nd, and Pb isotope compositions of the detrital clay-size fraction and clay mineral assemblages obtained from sediment core NGHP Site 17 in the Andaman Sea to reconstruct the variability of the South Asian monsoon during the past 60 kyr. Over this time interval εNd values changed little, generally oscillating between −7.3 and −5.3 and the Pb isotope signatures are essentially invariable, which is in contrast to a record located further northeast in the Andaman Sea. This indicates that the source of the detrital clays did not change significantly during the last glacial and deglaciation suggesting the monsoon was spatially stable. The most likely source region is the Irrawaddy river catchment including the Indo-Burman Ranges with a possible minor contribution from the Andaman Islands. High smectite/(illite + chlorite) ratios (up to 14), as well as low 87Sr/86Sr ratios (0.711) for the Holocene period indicate enhanced chemical weathering and a stronger South Asian monsoon compared to marine oxygen isotope stages 2 and 3. Short, smectite-poor intervals exhibit markedly radiogenic Sr isotope compositions and document weakening of the South Asian monsoon, which may have been linked to short-term northern Atlantic climate variability on millennial time scales.
    Description: Part of this work was funded by German Science Foundation (DFG), grant HA5751/3-1.
    Description: 2015-08-24
    Keywords: Marine sediments ; Clay minerals ; Radiogenic isotopes ; Andaman Sea ; South Asian monsoon
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Format: application/msword
    Format: application/pdf
    Location Call Number Limitation Availability
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  • 5
    Publication Date: 2022-05-26
    Description: Author Posting. © American Geophysical Union, 2012. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Geophysical Research Letters 39 (2012): L03704, doi:10.1029/2011GL050722.
    Description: Spanning a latitudinal range typical for deserts, the Indian peninsula is fertile instead and sustains over a billion people through monsoonal rains. Despite the strong link between climate and society, our knowledge of the long-term monsoon variability is incomplete over the Indian subcontinent. Here we reconstruct the Holocene paleoclimate in the core monsoon zone (CMZ) of the Indian peninsula using a sediment core recovered offshore from the mouth of Godavari River. Carbon isotopes of sedimentary leaf waxes provide an integrated and regionally extensive record of the flora in the CMZ and document a gradual increase in aridity-adapted vegetation from ~4,000 until 1,700 years ago followed by the persistence of aridity-adapted plants after that. The oxygen isotopic composition of planktonic foraminifer Globigerinoides ruber detects unprecedented high salinity events in the Bay of Bengal over the last 3,000 years, and especially after 1,700 years ago, which suggest that the CMZ aridification intensified in the late Holocene through a series of sub-millennial dry episodes. Cultural changes occurred across the Indian subcontinent as the climate became more arid after ~4,000 years. Sedentary agriculture took hold in the drying central and south India, while the urban Harappan civilization collapsed in the already arid Indus basin. The establishment of a more variable hydroclimate over the last ca. 1,700 years may have led to the rapid proliferation of water-conservation technology in south India.
    Description: This study was supported by grants from the National Science Foundation (OCE-0841736 and OCE- 0623766) and Woods Hole Oceanographic Institution.
    Description: 2012-08-14
    Keywords: Bay of Bengal ; Core Monsoon Zone ; Monsoon ; Neolithic
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Format: text/plain
    Format: application/pdf
    Format: application/vnd.ms-excel
    Location Call Number Limitation Availability
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