Abstract
We discuss geochemical proxies, reflecting processes of primary productivity, CaCO3 dissolution, and sediment redistribution in a piston core (RNDB 74P) from the Ontong Java Plateau. Due to the shallow water depth, biogenic carbonate is well preserved and a very goodδ 18O stratigraphy is available down to isotopic stage 11.230Thex gives evidence that the sediment accumulation pattern is driven mainly by processes of sediment focusing or winnowing. Due to the constant production of230Th in the water column, the bulk sediment accumulation rates could be corrected for the particle rain deriving from the water column above. The230Thex 0/CaCO3 ratio reflects the well-known Pacific CaCO3 preservation pattern with ice growth dissolution spikes and deglacial preservation spikes. The record of the grain size fraction >63 µm supports these results. The downcore concentrations and accumulation rates of barium (Ba) are on a higher level during interglacials and show several peaks. Normalization of Ba with230Thex 0 delivers a more uniform level of the Ba accumulation rates throughout the core. This pattern suggests a constantly higher biological productivity (nearly tenfold) in this area throughout the past 200 kyr compared with an open ocean environment. Barium peaks observed at the climatic transitions 2/1 and 6/5 and in stage 5 are in contrast to a predicted reduction of interglacial productivity at this location. A possible explanation might be the onset of the modern circulation pattern. The transition from Ba-enriched deep water to lower contents in the Atlantic might have resulted in an enhanced deposition of Ba in the Pacific.
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References
Anderson RF, Bacon MP, Brewer PG (1983) Removal of230Th and231Pa from the open ocean. Earth Planet Sci Lett 62:7–23
Archer D, Maier-Reimer E (1994) Effect of deep sea sedimentary calcite preservation on atmospheric CO2 concentration. Nature 367:260–263
Arrhenius GOS (1952) Sediment cores from the east Pacific: properties of the sediments. Rep Swed Deep Sea Exped, 1951–1952:1–227
Arrhenius GOS (1988) Rate of production, dissolution, and accumulation of biogenic solids in the ocean. Palaeogeogr Palaeoclimatol Palaeoecol 67:119–146
Baksi AK, Hsu V, McWilliams MO, Farrar E (1992)40Ar/39Ar dating of the Brunhes-Matuyama geomagnetic field reversal. Science 256:356–357
Bassinot FC, Beaufort L, Vincent E, Labeyrie LD, Rostek F, Müller PJ, Quidelleur X, Lancelot Y (1994) Coarse fraction fluctuations in pelagic carbonate sediments from the tropical Indian Ocean: a 1500-kyr record of carbonate dissolution. Paleoceanography 4:579–600
Berger WH (1973) Deep-sea carbonates: Pleistocene dissolution cycles. J Foraminiferal Res 3:187–195
Berger WH (1977) Deep-sea carbonate and the deglaciation preservation spike in pteropods and foraminifera. Nature 269:301–304
Berger WH, Vincent E (1981) Chemostratigraphy and biostratigraphic correlation: exercises in systematic stratigraphy. Oceanol Acta 4 (Suppl): 115–127
Berger WH et al. (1992) The record of the Ontong Java Plateau: main results of ODP Leg 130. Geol Soc Am Bull 104:954–972
Berger WH, Herguera JC, Lange CB, Schneider R (1994) Paleoproductivity: flux proxies versus nutrient proxies and other problems concerning the quaternary productivity record. In: Zahn R et al. (eds) Carbon cycling in the glacial ocean: constraints on the ocean’s role in the global change. Springer, Berlin Heidelberg New York, NATO ASI series I, vol 17, pp 385–412
Berger WH, Bickert T, Wefer G, Yasuda MK (1995) Brunhes-Matuyama boundary: 790 k.y. date consistent with ODP Leg 130 oxygen isotope records based on fit to Milankowitch template. Geophys Res Lett 22:1525–1528
Bishop JKB (1988) The barite-opal-organic carbon association in oceanic particulate matter. Nature 332:341–343
Boyle EA (1988) Vertical oceanic nutrient fractionation and glacial/interglacial CO2 cycles. Nature 331:55–56
Burke SK, Berger WH, Coulbourn WT, Vincent E (1993) Benthic foraminifera in box core ERDC 112, Ontong Java Plateau. J Foraminiferal Res 23:19–39
Chen JH, Edwards RL, Wasserburg GJ (1986)238U,234U and232Th in seawater. Earth Planet Sci Lett 80:241–251
Cochran JK, Osmond JK (1976) Sedimentation patterns and accumulation rates in the Tasman Basin. Deep Sea Res 23:193–210
Dehairs F, Goeyensm L, Stroobants N, Bernard P, Goyet C, Poisson A, Chesselet R (1990) On suspended barite and the oxygen minimum in the Southern Ocean. Global Biogeochem Cycles 4:85–102
Dymond J, Suess E, Lyle M (1992) Barium in deep-sea sediments: a geochemical proxy for paleoproductivity. Paleoceanography 7:163–181
Emerson S, Archer D (1992) Glacial carbonate dissolution cycles and atmospheric pCO2: a view from the ocean bottom. Paleoceanography 7:319–331
Finney BP, Lyle WL, Heath GR (1988) Sedimentation at MA-NOP Site H (eastern equatorial Pacific) over the past 400 000 years: climatically induced redox variations and their effects on transition metal cycling. Paleoceanography 3:169–189
Francois R, Bacon MP, Altabet MA, Labeyrie LD (1993) Glacial/interglacial changes in sediment rain rate in the SW Indian sector of subantarctic waters as recorded by230Th,231Pa, U, andδ 15N. Paleoceanography 8:611–629
Frank M, Eckhardt JD, Eisenhauer A, Kubik PW, Dittrich-Hannen B, Segl M, Mangini A (1994) Beryllium 10, thorium 230, and protactinium 231 in Galapagos microplate sediments: implications of hydrothermal activity and paleoproductivity changes during the last 100 000 years. Paleoceanography 9:559–578
Frank M, Eisenhauer A, Bonn WJ, Walter P, Grobe H, Kubik PW, Dittrich-Hannen B, Mangini A (1995) Sediment redistribution versus paleoproductivity change: Weddell Sea margin sediment stratigraphy for the last 250 000 years deduced from230Thex,10Be, and biogenic barium profiles. Earth Planet Sci Lett 136:559–573
Gingele F, Dahmke A (1994) Discrete barite particles and barium as tracers of paleoproductivity in South Atlantic sediments. Paleoceanography 9:151–168
Goldberg E, Arrhenius G (1958) Chemistry of pelagic sediments. Geochim Cosmochim Acta 13:153–212
Grötsch J, Wu G, Berger WH (1991) Carbonate cycles in the Pacific: reconstruction of saturation fluctuations. In: Einsele G et al. (eds) Cycles and events in stratigraphy. Springer, Berlin Heidelberg New York, pp 111–125
Hebbeln D, Wefer G, Berger WH (1990) Pleistocene dissolution fluctuations from apparent depth of deposition in core ERDC-127P, west-equatorial Pacific. Mar Geol 92:165–176
Herguera JC, Berger WH (1991) Paleoproductivity from benthic foraminifera abundance: glacial to postglacial change in the west-equatorial Pacific. Geology 19:1173–1176
Howard WR, Prell WL (1994) Late Quaternary CaCO3 production and preservation in the Southern Ocean: implications for oceanic and atmospheric carbon cycling. Paleoceanography 9:453–482
Imbrie J, Hays JD, Martinson DG, McIntyre A, Mix AC, Morley JJ, Pisias NG, Prell WL, Shackleton NJ (1984) The orbital theory of Pleistocene climate: support from a revised chronology of the marineδ 18O record. In: Berger A et al. (eds) Milankovitch and climate, part I. Reidel Publishing Company, Dordrecht, NATO ASI Series C, vol 126, pp 269–305
Keir RS (1988) On the late Pleistocene ocean geochemistry and circulation. Paleoceanography 3:413–445
Keir RS, Berger WH (1983) Atmospheric CO2 content in the last 120 000 years: the phosphate-extraction model. J Geophys Res 88:6027–6038
Kroenke LW (1972) Geology of the Ontong-Java Plateau. PhD thesis, University of Hawaii HIG-72-5
Kyte FT, Leinen M, Heath GR, Zhou L (1993) Cenozoic sedimentation history of the central North Pacific: inferences from the elemental geochemistry of core LL44-GPC3. Geochim Cosmochim Acta 57:1719–1740
Lange CB, Berger WH (1993) Diatom productivity and preservation in the western equatorial Pacific: the Quaternary record. In: Berger WH et al. (eds) Proc ODP Sci Results 130. Ocean Drilling Program, College Station, Texas, pp 509–523
Le J, Shackleton NJ (1992) Carbonate dissolution fluctuations in the western equatorial Pacific during the late Quaternary. Paleoceanography 7:21–42
Lea DW, Boyle EA (1990) Foraminiferal reconstruction of barium distribution in water masses of the glacial ocean. Paleoceanography 5:719–742
Lyle M, Murray DW, Finney BP, Dymond J, Robbins JM, Brooksforce K (1988) The record of late Pleistocene biogenic sedimentation in the eastern tropical Pacific Ocean. Paleoceanography 3:39–59
Mahoney JJ, Storey M, Duncan RA, Spencer KJ, Pringle M (1993) Geochemistry and geochronology of Leg 130 basement lavas: nature and origin of the Ontong Java Plateau. In: Berger WH et al. (eds) Proc ODP Sci Results 130. Ocean Drilling Program, College Station, Texas, pp 3–22
Mangini A, Sonntag C, Bertsch G, Müller E (1979) Evidence for a higher, natural U-content in world rivers. Nature 79:337–339
Mayer LA, Shipley TH, Winterer EL, Mosher D, Hagen RA (1991) Seabeam and seismic reflection surveys on the Ontong Java Plateau. In: Kroenke LW et al. (eds) Proc ODP Init Rep 130. Ocean Drilling Program, College Station, Texas, pp 45–75
Mayer LA, Jansen E, Backman J, Takayama T (1993) Climatic cyclicity at site 806:the GRAPE record. In: Berger WH et al. (eds) Proc ODP Sci Results 130. Ocean Drilling Program, College Station, Texas, pp 623–639
Pedersen TF (1983) Increased productivity in the eastern equatorial Pacific during the last glacial maximum. Geology 11:16–19
Prell WL, Imbrie J, Martinson DG, Morley JJ, Pisias NG, Shackleton NJ, Streeter HF (1986) Graphic correlation of oxygen isotope stratigraphy application to the late Quaternary. Paleoceanography 1:137–162
Rutsch HJ, Mangini A, Bonani G, Dittrich-Hannen B, Kubik PW, Suter M, Segl M (1995)10Be and Ba concentations in West African sediments trace productivity in the past. Earth Planet Sci Lett 133:129–143
Schmitz B (1987) Equatorial high productivity, and the northward wandering of the Indian continent. Paleoceanography 2:63–77
Shackleton NJ, Berger A, Peltier WR (1990) An alternative astronomical calibration of the lower Pleistocene timescale based on ODP site 677. Trans R Soc Edinburgh Earth Sci 81:251–261
Suman DO, Bacon MP (1989) Variations in Holocene sedimentation in the North American Basin determined from230Th measurements. Deep Sea Res 36:869–878
Tarduno JA, Sliter WV, Kroenke L, Leckie M, Mayer H, Mahoney JJ, Musgrave R, Storey M, Winterer EL (1991) Rapid formation of Ontong Java Plateau by Aptian mantle plume volcanism. Science 254:399–403
Wedepohl (1995) The composition of the continental crust. Geochim Cosmochim Acta 59:1217–1232
Wu G, Berger WH (1991) Pleistoceneδ 18O records from Ontong Java Plateau: effects of winnowing and dissolution. Mar Geol 96:193–209
Wu G, Yasuda MK, Berger WH (1991) Late Pleistocene carbonate stratigraphy on Ontong Java Plateau in the western equatorial Pacific. Mar Geol 99:135–150
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Schwarz, B., Mangini, A. & Segl, M. Geochemistry of a piston core from Ontong Java Plateau (western equatorial Pacific): evidence for sediment redistribution and changes in paleoproductivity. Geol Rundsch 85, 536–545 (1996). https://doi.org/10.1007/BF02369008
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DOI: https://doi.org/10.1007/BF02369008