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  • 1
    Online Resource
    Online Resource
    Cham :Springer International Publishing AG,
    Keywords: Marine geophysics. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (290 pages)
    Edition: 1st ed.
    ISBN: 9783030406592
    Series Statement: Society of Earth Scientists Series
    DDC: 353.00823200000002
    Language: English
    Note: Intro -- Series Editor Foreword -- Foreword -- Preface -- Contents -- About the Editors -- Introduction-Scientific Drilling in the Indian Ocean: An Earth System Process Perspective -- 1 Himlayan-Tibetan Orogeny and Long Term Climate Evolution -- 1.1 Indian Monsoon Rainfall (IODP Expedition 353) -- 1.2 Bengal Fan -- 1.3 Indus Fan -- 2 The Indonesian Throughflow Expedtion -- 2.1 Indonesian Throughflow (ITF) and the Australian Monsoon -- 3 Maldives and Equatorial Indian Ocean -- 3.1 Maldives Monsoon and Sea Level -- 4 South African Climates -- 4.1 The South African Climates and Agulhas Current Density Profile -- 5 Plate Deformation Zones -- 5.1 "The Nature of the Lower Crust and Moho at Slower Spreading Ridges"-SloMo -- 5.2 To Understand the Role of Input Materials in the Northern Sumatra Subduction -- 6 Concluding Remarks -- References -- Morphological and Chemical Properties of Microtektite Grains from Bay of Bengal (IODP Expedition 354) -- 1 Introduction -- 2 Materials and Methods -- 3 Results and Discussion -- 4 Morphological Characteristics of the Microtektites -- 5 Shapes, Size and Color -- 6 Surface Sculpturing -- 7 Compositional Characteristics of Microtektites -- 8 Evidence of Extraterrestrial Materials Within the Microtektite Layer -- 9 Conclusions -- References -- Assessing Mid-pleistocene to Holocene Sea-Ice Extent and Carbonate Compensation Depth Fluctuations in the Japan Sea: A Multiproxy Approach -- 1 Introduction -- 2 Location, Lithology, and Hydrography of Japan Sea -- 2.1 Material and Methods -- 3 Results -- 3.1 Distribution of IRD and Detrital -- 3.2 Distribution of Foraminifera -- 3.3 Environmental Preferences of Dominant Planktic Species -- 4 Discussion -- 5 Conclusion -- References -- Modern Radiolarians Recovered from the Mudline Samples at IODP-341 Sites in the South Alaska Basin, North East Pacific Ocean -- 1 Introduction. , 2 Radiolarians from Mudline Samples -- 3 Results -- 3.1 Radiolarians in the Mudline, Hole U1417D -- 3.2 Radiolarians in the Mudline, Hole U1418C -- 3.3 Radiolarians in the Mudline Hole U1419A -- 3.4 Radiolarians in the Mudline, Hole U1421A -- 4 Conclusion -- References -- Carbon Stable Isotope Source Signature of Bulk Organic Matter in Middle Bengal Fan Sediment Collected During IODP Expedition 354 -- 1 Introduction -- 2 Site -- 3 Materials and Method -- 4 Results -- 4.1 TOC, N, C/N Ratio and δ13C of Sedimentary OM -- 5 Discussion -- 5.1 Preservation of OM -- 5.2 Source of OM -- 6 Conclusion -- References -- Geochemistry of Marine Carbonates from Hole 1394, off the Coast of Montserrat, IODP Expedition-340 -- Implications on Provenance, Paleoenvironment and Lesser Antilles Arc Migration -- 1 Introduction -- 2 Materials and Methods -- 3 Stratigraphy and Nature of Sediments -- 4 Results -- 4.1 Geochemistry -- 5 Discussion -- 5.1 Europium Anomalies (Eu/Eu*) -- 5.2 Cerium Anomalies (Ce/Ce*) -- 5.3 Er/Nd Ratios -- 5.4 Age of the Carbonates -- 5.5 Depth Wise Variation in Geochemical Parameters -- 5.6 Source Weathering and Alteration Characteristics -- 5.7 Contamination and Diagenetic Alterations -- 5.8 Temperate (Cool Water) Versus Tropical (Warm Water) Carbonates -- 5.9 Th/U Ratios -- 5.10 Paleo-redox Characteristics -- 5.11 Total Carbon and Carbonate Content -- 5.12 Shifting of Platformal Carbonates to Deep Ocean: Evidence from Ce and La (Pr/Pr*) Anomalies -- 5.13 Tectonic Setting -- 6 Conclusions -- References -- Morpho-taxonomy of Corycaeid Cyclopoids from Lakshadweep Sea, South Eastern Arabian Sea-A Part of the Indian Ocean -- 1 Introduction -- 2 Materials and Methods -- 3 Results -- 4 Discussion and Conclusion -- References. , Sedimentological Attributes and Quartz Microtexture in the Levee Sediments of a Submarine Channel in Context of the East Antarctic Ice Sheet Fluctuations: A Study from Site U-1359 of IODP-318 Expedition -- 1 Introduction -- 2 Site U1359 -- 3 Materials and Methods -- 4 Results -- 4.1 Grain Size Analysis -- 4.2 Quartz Grain Microtextures -- 5 Discussion -- 5.1 Sedimentary Processes -- 5.2 Depositional Environment -- 6 Conclusions -- References -- Late Quaternary Sedimentation and Slope Failure Events on the Costa Rican Margin -- 1 Introduction -- 2 Materials and Methods -- 2.1 Samples and Data -- 2.2 Sample Processing for XRD Analysis -- 2.3 Quantification of Clay Minerals -- 2.4 Sample Processing for XRF Analysis -- 2.5 Sample Processing for IRMS Analysis -- 2.6 Age Model -- 3 Results and Discussion -- 3.1 Clay Minerals -- 3.2 Quantification of Major Elements -- 3.3 Carbon and Nitrogen Isotopes -- 4 Summary and Conclusions -- References -- mtCOI Sequence-Based Barcoding of Calanoid Copepods from Lagoon Waters of Lakshadweep, South-west Coast of India -- 1 Introduction -- 2 Materials and Methods -- 3 Results -- 3.1 Molecular Records and Systematics of the Calanoid Copepods -- 3.2 Barcode Library Developed for the Calanoid Copepods -- 4 Discussion -- References -- A Summary of the South China Sea Evolution -- 1 Introduction -- 2 Regional Geological Setting -- 3 Evolution History -- 4 Dynamics of the South China Sea -- 4.1 The Tectonic Extrusion Model -- 4.2 Backarc Extension Model -- 4.3 Two-Stage Rifting Model -- 4.4 Proto-SCS Dragging Model -- 4.5 Models that Involve Extension Induced by Mantle Plume -- 4.6 Combined Model -- References -- Microbial Community Profile of Deep-Sea Sediment from Eastern Arabian Sea (IODP 355) -- 1 Introduction -- 2 Materials and Methods -- 2.1 Deep Sea Sediment Cores IODP -- 2.2 DNA Extraction. , 2.3 16S rRNA Gene Sequencing -- 3 Quality Control, Taxonomic Assignment, Diversity Estimation and Total Cell Counts -- 4 Result and Discussion -- 4.1 Total Cell Counts -- 4.2 Taxonomic Assignment and Microbial Diversity -- References.
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  • 2
    Keywords: Geochemistry. ; Paleontology . ; Sedimentology. ; Aufsatzsammlung ; Integrated Ocean Drilling Program ; Indien ; Geowissenschaftler ; Meeresgeologie
    Description / Table of Contents: Scientific drilling in the Indian Ocean: An Earth system process perspective -- Morphological and chemical properties of microtektite grains from Bay of Bengal (IODP Expedition 354) -- Assessing Mid-Pleistocene to Holocene Sea-ice Extent and Carbonate Compensation Depth fluctuations in the Japan Sea: a multiproxy approach -- Modern Radiolarians Recovered from the mudline samples at IODP-341 sites in the South Alaska Basin, North East Pacific Ocean -- Carbon Stable Isotope Source Signature of Bulk Organic Matter in Middle Bengal Fan Sediment Collected During IODP Expedition 354 -- Geochemistry of Marine Carbonates from Hole 1394, off the coast of Montserrat, IODP Expedition-340; Implications on provenance, paleoenvironment and Lesser Antilles arc migration -- Morpho-taxonomy of Corycaeid cyclopoids from Lakshadweep Sea, South Eastern Arabian Sea- a part of the Indian Ocean -- Sedimentological attributes and quartz microtexture in the levee sediments of a submarine channel in context of the East Antarctic ice sheet fluctuations: A study from site U-1359 of IODP-318 expedition -- Late Quaternary sedimentation and slope failure events on the Costa Rican margin -- Mt COI sequence-based barcoding of calanoid copepods from lagoon waters of Lakshadweep, South-West coast of India -- A Summary of the South China Sea Evolution -- Microbial Community Profile and Deep-sea sediment of Eastern Arabian Sea (IODP 355).
    Type of Medium: Online Resource
    Pages: 1 Online-Ressource(XIV, 283 p. 121 illus., 80 illus. in color.)
    Edition: 1st ed. 2020.
    ISBN: 9783030406592
    Series Statement: Society of Earth Scientists Series
    Language: English
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  • 3
    Publication Date: 2024-01-29
    Description: Deep-sea sediments from the International Ocean Discovery Program (IODP) Site U1457 (Laxmi basin, Northern Indian Ocean) at ~1100 meters below the seafloor (mbsf) of the Danian period (c. 66 – 61.6 Ma) are examined, which suggest that the foraminifera subsisted across the major geologic events. A foraminiferal census count (%) was performed under a microscope and species belonging to Bolivina, Bulimina, Cassidulina, Cibicidoides, Epistominella, and Oolina genera are found to be dominant in the region (Table 1). The species were grouped under relative abundance (benthic/planktic), habitual preference (infauna/epifauna), and shell composition (calcareous/agglutinated) with literature references (Table 2). Calcium carbonate (%) was calculated from inorganic carbon values analyzed in a coulometer (Table 2). Magnetic susceptibility of low frequency is measured through a Bartington MS2B sensor and the units of measurement are defined in Table 2. The assemblage of benthic foraminifera belonging to each morphogroup (Table 3). Oxic, Suboxic, Dysoxic benthic foraminifera and Oxygen content were calculated through transfer function from oxyphillic species (Table 4). Benthic foraminifera diversity pattern Fisher alpha calculated through PAST software. All the foraminifera representations are made in percentage and depth in the units of meters below the seafloor.
    Keywords: Calcium Carbonate; Danian; Foraminifera; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; Laxmi basin; Northern Indian Ocean
    Type: Dataset
    Format: application/zip, 5 datasets
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  • 4
    Publication Date: 2024-01-29
    Keywords: 355-U1457C; Calcium Carbonate; Danian; DEPTH, sediment/rock; DRILL; Drilling/drill rig; Exp355; Foraminifera; Foraminifera, benthic, biserial; Foraminifera, benthic, planispiral; Foraminifera, benthic, triserial; Foraminifera, benthic, trochospiral; Foraminifera, benthic, tubular; Foraminifera, benthic, unilocular; Foraminifera, benthic, uniserial; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; Joides Resolution; Laxmi basin; Miliolinae; Northern Indian Ocean
    Type: Dataset
    Format: text/tab-separated-values, 88 data points
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  • 5
    Publication Date: 2024-01-29
    Keywords: 355-U1457C; Calcium Carbonate; Danian; DEPTH, sediment/rock; DRILL; Drilling/drill rig; Exp355; Fishers alpha index of diversity; Foraminifera; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; Joides Resolution; Laxmi basin; Northern Indian Ocean; PAST software
    Type: Dataset
    Format: text/tab-separated-values, 11 data points
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  • 6
    Publication Date: 2024-01-29
    Keywords: 355-U1457C; Calcium Carbonate; Danian; DEPTH, sediment/rock; Dissolved oxygen index; DRILL; Drilling/drill rig; Exp355; Foraminifera; Foraminifera, benthic, dysoxic fauna; Foraminifera, benthic, oxic fauna; Foraminifera, benthic, suboxic fauna; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; Joides Resolution; Laxmi basin; Northern Indian Ocean; Oxygen transfer function of Drinia et al. (2004)
    Type: Dataset
    Format: text/tab-separated-values, 44 data points
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  • 7
    Publication Date: 2024-01-29
    Keywords: 355-U1457C; Bolivina spp.; Bulimina spp.; Calcium Carbonate; Cassidulina spp.; Cibicidoides spp.; Danian; DEPTH, sediment/rock; DRILL; Drilling/drill rig; Epistominella spp.; Exp355; Foraminifera; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; Joides Resolution; Laxmi basin; Northern Indian Ocean; Oolina spp.
    Type: Dataset
    Format: text/tab-separated-values, 66 data points
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  • 8
    Publication Date: 2024-01-29
    Keywords: 355-U1457C; Calcium carbonate; Calcium Carbonate; Danian; DEPTH, sediment/rock; DRILL; Drilling/drill rig; Exp355; Foraminifera; Foraminifera, benthic; Foraminifera, benthic, epifaunal; Foraminifera, benthic, infaunal; Foraminifera, benthic agglutinated; Foraminifera, benthic calcareous; Foraminifera, planktic; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; Joides Resolution; Laxmi basin; Northern Indian Ocean; Susceptibility, specific
    Type: Dataset
    Format: text/tab-separated-values, 88 data points
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  • 9
    Publication Date: 2020-12-23
    Description: Highlights • Sediment accumulation rates in Nicobar Fan abruptly increase 9.5 Ma. • Increased sediment flux to eastern Indian Ocean and restructuring of sediment routing. • Nicobar Fan holds significant record of Indian Ocean sedimentation in late Neogene. • Shillong Plateau and Indo–Burmese wedge uplift drive sediment south in late Miocene. A holistic view of the Bengal–Nicobar Fan system requires sampling the full sedimentary section of the Nicobar Fan, which was achieved for the first time by International Ocean Discovery Program (IODP) Expedition 362 west of North Sumatra. We identified a distinct rise in sediment accumulation rate (SAR) beginning ∼9.5 Ma and reaching 250–350 m/Myr in the 9.5–2 Ma interval, which equal or far exceed rates on the Bengal Fan at similar latitudes. This marked rise in SAR and a constant Himalayan-derived provenance necessitates a major restructuring of sediment routing in the Bengal–Nicobar submarine fan. This coincides with the inversion of the Eastern Himalayan Shillong Plateau and encroachment of the west-propagating Indo–Burmese wedge, which reduced continental accommodation space and increased sediment supply directly to the fan. Our results challenge a commonly held view that changes in sediment flux seen in the Bengal–Nicobar submarine fan were caused by discrete tectonic or climatic events acting on the Himalayan–Tibetan Plateau. Instead, an interplay of tectonic and climatic processes caused the fan system to develop by punctuated changes rather than gradual progradation.
    Type: Article , PeerReviewed
    Format: text
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  • 10
    Publication Date: 2020-02-06
    Description: Plate-boundary fault rupture during the 2004 Sumatra-Andaman subduction earthquake extended closer to the trench than expected, increasing earthquake and tsunami size. International Ocean Discovery Program Expedition 362 sampled incoming sediments offshore northern Sumatra, revealing recent release of fresh water within the deep sediments. Thermal modeling links this freshening to amorphous silica dehydration driven by rapid burial-induced temperature increases in the past 9 million years. Complete dehydration of silicates is expected before plate subduction, contrasting with prevailing models for subduction seismogenesis calling for fluid production during subduction. Shallow slip offshore Sumatra appears driven by diagenetic strengthening of deeply buried fault-forming sediments, contrasting with weakening proposed for the shallow Tohoku-Oki 2011 rupture, but our results are applicable to other thickly sedimented subduction zones including those with limited earthquake records.
    Type: Article , PeerReviewed
    Format: text
    Format: text
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