Late Quaternary insolation forcing on total organic carbon and C37 alkenone variations in the Arabian Sea

Paleoceanography

Volumn 15, Issue 3, 2000, Pages 307-321

  Budziak, Dörte ^a   Schneider, Ralph R ^a   Rostek, Frauke ^b   Müller, Peter J ^a   Bard, Edouard ^b   Wefer, Gerold ^a  

^a UNIVERSITY OF BREMEN   (Germany)

^b CEREGE   (France)

Author keywords

[No Author keywords available]

Indexed keywords

ALKENONE; CARBON ISOTOPE; INSOLATION; MONSOON; PALEOCEANOGRAPHY; PALEOPRODUCTIVITY; QUATERNARY; TOTAL ORGANIC CARBON;

ARABIAN SEA;

EID: 0034451771     PISSN: 08838305     EISSN: None     Source Type: Journal    
DOI: 10.1029/1999PA000433     Document Type: Review

References (58)

1. 14N
2. 14N rations
3. A 300 kyr record of upwelling off Oman during the late Quaternary: Evidence of the Asian southwest monsoon
4. Coarse fraction fluctuations in pelagic carbonate sediments from the tropical Indian Ocean: A 1500-kyr record of carbonate dissolution
5. Insolation changes as a major control of equatorial Indian Ocean primary productivity
6. Long-term variations of daily insolation and Quaternary climatic change
7. Interannual variability in phytoplankton blooms observed in the northwestern Arabian Sea during the Southwest Monsoon
8. Meteorology of the Indian summer monsoon
9. Paleoproductivity in the equatorial Indian Ocean for the last 260,000 yr: A transfer function based on planktonic foraminifera
10. Late Pleistocene variability of Arabian Sea summer monsoon winds and continental aridity: Eolian records from the lithogenic component of deep-sea sediments
11. One million year record of summer monsoon winds and continental aridity from the Owen Ridge (Site 722), northwest Arabian Sea
12. Forcing mechanisms of the Indian Ocean monsoon
13. Sensitivity of Asian and African climate to variations in seasonal insolation, glacial ice cover, sea surface temperature, and Asian orography
14. Sea-surface temperatures and the history of monsoon upwelling in the northwestern Arabian Sea during the last 500,000 years
15. A major low level air current near the Indian Ocean during the northern summer
16. Seasonality and interannual variability of particle fluxes to the deep Arabian Sea
17. Spatial and temporal variations of total organic carbon in the Arabian Sea
18. 18O record
19. Oceanic response to orbital forcing in the Late Quaternary: Observational and experimental strategies
20. Organic carbon removal in the sea: The continental connection
21. Evaluation of the Plio-Pleistocene astronomical timescale
22. Variability in upwelling fields in the northwestern Indian Ocean, 1, Model experiments for the past 18,000 years
23. Productivity, sedimentation rate, and sedimentary organic matter in the oceans. I, Organic carbon preservation
24. 13C and alkenone temperatures
25. Late Pliocene and Pleistocene climatic oscillations and monsoon upwelling recorded in sediments from the Owen Ridge, northwestern Arabian Sea
26. A high-resolution record of late Quaternary upwelling along the Oman Margin, Arabian Sea based on planktonic foraminifera
27. Increased particle flux to the deep ocean related to monsoons
28. Oxygen and carbon isotope stratigraphy at Site 723, Oman Margin
29. Macintosh program performs time series analysis
30. Precession control on sedimentary burial of organic matter and redox sensitive metals in the tropical Indian Ocean
31. A critical evaluation of depositional parameters controlling the variability of organic carbon in Arabian Sea sediments
32. Lack of enhanced preservation of organic matter in sediments under the oxygen minimum on the Oman Margin
33. Monsoonal climate of the Arabian Sea during the late Quaternary: A response to changing solar radiation
34. Monsoon variability over the past 150,000 years
35. Sensitivity of the Indian monsoon to forcing parameters and implications for its evolution
36. Evolution of the climatological near-surface thermal structure of the tropical Indian Ocean, 1, Description of mean monthly layer depth, and sea surface temperature, surface current, and surface meteorological fields
37. Temporal variability in the northern Arabian Sea oxygen minimum zone (OMZ) during the last 225,000 years
38. Coupling between SW monsoon-related surface and deep ocean processes as discerned from continuous particle flux measurements and correlated satellite data
39. Fluctuations of the Indian monsoon regime during the last 170,000 years: Evidence from sea surface temperature, salinity and organic carbon records
40. Sea surface temperature and productivity records for the past 240 kyr in the Arabian Sea
41. Transfer functions to reconstruct ocean palaeoproductivity: A comparison
42. Stable phytoplankton community structure in the Arabian Sea over the past 200,000 years
43. Variations of oxygen-minimum and primary productivity recorded in sediments of the Arabian Sea
44. Spectrum: Sspectral analysis of unevenly spaced paleoclimatic time series
45. A 350 ka history of the Indian Southwest Monsoon: Evidence from deep-sea cores, northwest Arabian Sea
46. Century-scale events in monsoonal climate over the past 24,000 years
47. Core-top calibration of the alkenone index vs sea surface temperature in the Indian ocean
48. Some aspects of the physical oceanography of the Indian Ocean
49. Climatic conditions deduced from a 150-kyr oxygen isotope-pollen record from the Arabian Sea
50. Determination of organic carbon and nitrogen in marine sediments using the Carlo Erba NA-1500 Analyzer
51. Alkenones in Gephyrocapsa oceanica: Implications for studies of paleoclimate
52. The elementary monsoon
53. Physical oceanography of the Indian Ocean