Geochemical characteristics of deep-sea sediments from the Arabian Sea: A high-resolution study

Deep-Sea Research Part II: Topical Studies in Oceanography

Volumn 47, Issue 14, 2000, Pages 2735-2768

  Schnetger, B ^a   Brumsack, H J ^a   Schale, H ^a   Hinrichs, J ^a   Dittert, L ^b  

^a UNIVERSITY OF OLDENBURG   (Germany)

^b UNIVERSITY OF BREMEN   (Germany)

Author keywords

[No Author keywords available]

Indexed keywords

CHEMICAL COMPOSITION; CORE ANALYSIS; DEEP-SEA SEDIMENT; GEOCHEMISTRY; TRACE ELEMENT;

ARABIAN SEA;

EID: 0033813552     PISSN: 09670645     EISSN: None     Source Type: Journal    
DOI: 10.1016/S0967-0645(00)00047-3     Document Type: Article

References (64)

1. 231Pa at ocean margins
2. Oceanic primary production 1. Estimation at global scale from satellite (coastal zone color scanner) chlorophyll
3. 226Ra disequilibria in seawater and suspended particulate matter
4. Seasonal and spatial variations in settling manganese fluxes in the Northern Arabian Sea
5. Morphological and compositional evidence for biotic precipitation of marine barite
6. Bacterial activity in sediments of the deep Arabian Sea in relation to vertical flux
7. Stable sulfur isotopes indicate net sulfate reduction in near-surface sediments of the deep Arabian Sea
8. 3 solid solutions at 20°C: An experimental study
9. First occurence and stable isotope composition of authigenic γ-MnS in the central Gotland Deep (Baltic Sea)
10. Manganese carbonate overgrowths on foraminifera tests
11. Geochemistry of recent TOC-rich sediments from the Gulf of California and the Black Sea
12. Interstitial water trace-metal chemistry of laminated sediments from the Gulf of California, Mexico
13. Sedimentary Geochemistry of Silicon
14. Geochemistry of recent oxic and anoxic marine sediments: Implications for the geological record
15. The geochemical cycle of rhenium: A reconnaissance
16. Post-depositional mobility of platinum, iridium and rhenium in marine sediments
17. Rhenium and molybdenum enrichments in sediments as indicators of oxic, suboxic and sulfidic conditions of depostition
18. Clay mineralogy of Neogene sediments of the western Arabian Sea: Mineral abundances and paleoenvironmental implications
19. Barium in deep-sea sediment: A geochemical proxy for paleoproductivity
20. Climatic influences on the growth rates of Mn crusts during the late Quaternary
21. Diagenetic separation of cadmium and manganese in suboxic continental margin sediments
22. Geochemistry of Pacific pelagic sediments
23. Pore-water distribution and quantification of diffusive benthic fluxes of silicic acid, nitrate and phosphate in surface sediments of the deep Arabian Sea
24. 230Th in Arabian Sea sediments by isotope dilution sector field ICP-MS
25. 18O record
26. Formation and solid solution behavior of Carhodochrosites in marine muds of the Baltic deeps
27. The sedimentation rates of trace elements in the Sargasso Sea by sediment traps
28. Uranium in the oceans: Where it goes and why
29. Surficial sediments of the Arabian Sea
30. Uranium in the open ocean: Concentration and isotope composition
31. Cenozoik sedimentation history of the central North Pacific: Inferences from the elemental geochemistry of core LL44-GPC3
32. Boundary scavenging and deep-sea sediment dating: Constraints from excess 230Th and 231Pa
33. Response of manganese in the oceans to the climatic cycles in the Quaternary
34. Age dating and the orbital theory of the ice ages: Development of a high-resolution 0-300,000-year chronostatigraphy
35. Manganese solubility control in marine porewaters
36. The geochemistry of redox sensitive trace metals in sediments
37. Driving forces of Indian summer monsoon on Milankovitch and sub-Milancovitch time scales: A review
38. Early diagenesis and sulphur speciation in sediments of the Oman Margin, northwestern Arabian Sea
39. Interstitial water chemistry, Leg 117: Contrasts with Peru Margin
40. A 225 kyr record of dust supply, paleoproductivity and the oxygen minimum zone from the Murray Rigde (northern Arabian Sea)
41. The influence of the SW monsoon on the deep-sea organic carbon cycle in the Holocene
42. Authigenic cadmium enrichments in suboxic sediments: Precipitation and postdepositional mobility
43. Manganese and iron in Indian Ocean waters
44. Monsoon related variations in Zaire (Congo) sediment load and influence of fluvial silicate supply on marine productivity in the east equatorial Atlantic during the last 200,000 years
45. Chemical composition of loess from a local and worldwide view
46. Trace element analysis of sediments by HR-ICP-MS using low and medium resolution and different acid digenstions
47. Geochemistry of surface sediments from the Arabian Sea
48. Early diagenesis in differing depositional environments: The response of transition metals in pore water
49. Can sediment geochemistry record changes in coastal upwelling palaeoproductivity? Evidence from northwest Africa and the Arabian Sea
50. The inorganic geochemical record of the Northwest Arabian Sea: A history of productivity variation over the last 400 k.y. from Sites 722 and 724
51. U-series disequilibrium, particle scavenging, and sediment accumulation during the late Pleistocene on the Owen Ridge, site 722
52. Clay mineral accumulation rates in the Arabian Sea during the late Quaternary
53. Teleconnections between the subtropical monsoons and high-latitude climates during the last deglaciation
54. The behavior of manganese in Atlantic carbonate sediments
55. The Cenomanian/Turonian Boundary Event in the Indian Ocean a key to understand the global picture
56. Lack of organic matter accumulation on the upwelling influenced Somalia margin in a glacial interglacial transition
57. Water depth and diagenetic constraints on the use of barium as a palaeoproductivity indicator
58. Turbidite depostion and the origin of the Madeira Abyssal Plain
59. Late Pleistocene upwelling and productivity variations in the Northwest Indian Ocean deduced from spectral analyses of geochemical data from sites 722 and 724
60. Environmental influences on the chemical composition of shales and clays
61. Cyclic variations in the chemical composition of eastern Mediterranean Pliocene sediments: A key for understanding sapropel formation