50
Weferetal.
rate, and sedimentary organic matter in the oceans.
1. Organic carbon preservation. Deep-Sea Res 26:
\347-\362
Muller P J, Erlenkeuser H, Grafenstein R (1983) Glacialinterglacial cycles in oceanic productivity inferred
from organic carbon contents in eastern North
Atlantic sediment cores. In: Thiede J, Suess E (eds)
Coastal upwelling: Its Sediment Record (Part B).
Plenum Press, New York, pp 365-398
MUller PJ, Schneider R, Ruhland G (1994) Late Quaternary PC0 2 variations in the Angola Current: evidence
from organic carbon Ol3C and alkenone temperatures.
In: Zahn R, Pedersen TF, Kaminski MA, Labeyrie L
(eds) Carbon Cycling in the Glacial Ocean: Constraints on the Ocean's Role in Global Change.
NATO ASI Series, Vol 17, Springer, Berlin Heidelberg
NewYork,pp343-366
MUller PJ, Cepek M, Ruhland G, Schneider RR (1997)
Alkenone and coccolithophorid species changes in
late Quaternary sediments from the Walvis Ridge:
Implications for the alkenone paleotemperature
method. Palaeogeogr Palaeoclimatol Palaeoecol135:
71-%
MUller PJ, Kirst G, Ruhland G, von Storch I, Rosell-Mele
A (1998) Calibration of the alkenone paleotemperature index Uk' J7 based on core-tops from the eastern
South Atlantic and the global ocean (60 0 N-600S),
Geochim Cosmochim Acta 62: 1757-1772
Murray J (1897). On the distribution of the pelagic
foraminifera at the surface and on the floor of the
ocean, Nat Sci (Ecology) II: 17-27
Murray RW, Leinen M (1993) Chemical transport to the
seafloor of the Equatorial Pacific across a latitudinal
transect at 135°W; Tracking sedimentary major,
trace, and rare earth element fluxes at the Equator
and theITCZ, Geochim Cosmochim Acta 57: 41414163
Murray RW, LeinenM, Isern AR(1993) Biogenic flux of
Al to sediment in the equatorial Pacific Ocean; Evidence for increased productivity during glacial episodes, Paleoceanography 8: 651-670
Nelson DM, Gordon LI (1982) Production and pelagic
dissolution of biogenic silica in the Southern Ocean,
Geochim Cosmochim Acta 46: 491-50 I
Nelson DM, Trt!guer P, Brzenzinski MA, Leynaert A,
Queguiner B (1995) Production and dissolution of
biogenic silica in the ocean: Revised global estimates,
comparison with regional data and realtionship to
biogenic sedimentation, Global Biogeochem Cycles
9:359-372
NUrnberg D (1995) Magnesium in tests of Neogloboquadrina pachyderma sinistral from high northern
and southern latitudes, J Foram Res 25: 350-368
NUrnberg D, Bijma J, Hemleben C (1996a) Assessing the
reliability of magnesium in foraminiferal calcite as a
proxy for water mass temperatures, Geochim
Cosmochim Acta 60: 803-814
NUrnberg D, Bijma J, Hemleben C (1996b) Erratum,
Geochim Cosmochim Acta 60: 2483-2484
Oberhansli H, Benier C, Meinecke G, Schmidt H, Schneider R, Wefer G (1992) Planktic foraminifers as tracers of ocean currents in the eastern South Atlantic,
Paleoceanography 7: 607-632
O'Neil JR, Clayton RN, Mayeda TK (1969) Oxygen isotope fractionation in divalent metal carbonates, J
ChemPhys51: 5547-5558
Oppo DW, Fairbanks RG (1989) Carbon isotope composition of tropical surface water during the past 22,000
years. Palaeoceanography 4: 333-351
Oppo DW, Rosenthal Y (1994) Cd/Ca changes in a deep
Cape Basin core over the past 730,000 years: Response of circumpolar deepwater variability to
nothern hemisphere ice sheet melting?
Paleoceanography 9: 661-675
Oppo DW, Fairbanks RG, Gordon AL, Shackleton NJ
(1990) Late pleistocene southern ocean C 13 variability, Paleoceanography 5: 43-54
Ortiz JD, Mix AC (1997) Comparison ofImbrie-Kipp
transfer function and modern analog temperature
estimates using sediment trap and core top foraminiferal faunas, Paleoceanography 12: 175-190
Owens NJP (1987) Natural variations in l5N in the marine environment. Adv Mar Bioi 24: 390-451
Palmer MR, Edmond JM (1989) The strontium isotope
budget of the modem ocean, Earth Planet Sci Lett
92: 11-26
Parker FL (1958) Eastern Mediterranean foraminifera,
Reports ofthe Swedish Deep-Sea Expedition, 19471948,8: 217-283
Parker FL, Berger WH (1971) Faunal and solution patterns of planktonic foraminifera in surface sediments
of the South Pacific, Deep-Sea Res 18: 73-107
Pay tan A, Kastner M (1996) Benthic Ba fluxes in the
central equatorial Pacific, implications for the oceanic Bacycle, Earth Planet Sci Lett 142: 439-450
Pay tan A, Kastner M, Martin EE, Macdougall JD,
Herbert T (1993) Marine barite as a monitor of
seawater strontium isotope composition, Nature 366:
445-449
Paytan A, Kastner M, Chavez FP (1996) Glacial to Interglacial fluctuations in productivity in the Equatorial
Pacific as indicated by marine barite, Science 274:
1355-1357
Peltier WR, Tushingham AM (1989) Global sea level rise
Weferetal.
rate, and sedimentary organic matter in the oceans.
1. Organic carbon preservation. Deep-Sea Res 26:
\347-\362
Muller P J, Erlenkeuser H, Grafenstein R (1983) Glacialinterglacial cycles in oceanic productivity inferred
from organic carbon contents in eastern North
Atlantic sediment cores. In: Thiede J, Suess E (eds)
Coastal upwelling: Its Sediment Record (Part B).
Plenum Press, New York, pp 365-398
MUller PJ, Schneider R, Ruhland G (1994) Late Quaternary PC0 2 variations in the Angola Current: evidence
from organic carbon Ol3C and alkenone temperatures.
In: Zahn R, Pedersen TF, Kaminski MA, Labeyrie L
(eds) Carbon Cycling in the Glacial Ocean: Constraints on the Ocean's Role in Global Change.
NATO ASI Series, Vol 17, Springer, Berlin Heidelberg
NewYork,pp343-366
MUller PJ, Cepek M, Ruhland G, Schneider RR (1997)
Alkenone and coccolithophorid species changes in
late Quaternary sediments from the Walvis Ridge:
Implications for the alkenone paleotemperature
method. Palaeogeogr Palaeoclimatol Palaeoecol135:
71-%
MUller PJ, Kirst G, Ruhland G, von Storch I, Rosell-Mele
A (1998) Calibration of the alkenone paleotemperature index Uk' J7 based on core-tops from the eastern
South Atlantic and the global ocean (60 0 N-600S),
Geochim Cosmochim Acta 62: 1757-1772
Murray J (1897). On the distribution of the pelagic
foraminifera at the surface and on the floor of the
ocean, Nat Sci (Ecology) II: 17-27
Murray RW, Leinen M (1993) Chemical transport to the
seafloor of the Equatorial Pacific across a latitudinal
transect at 135°W; Tracking sedimentary major,
trace, and rare earth element fluxes at the Equator
and theITCZ, Geochim Cosmochim Acta 57: 41414163
Murray RW, LeinenM, Isern AR(1993) Biogenic flux of
Al to sediment in the equatorial Pacific Ocean; Evidence for increased productivity during glacial episodes, Paleoceanography 8: 651-670
Nelson DM, Gordon LI (1982) Production and pelagic
dissolution of biogenic silica in the Southern Ocean,
Geochim Cosmochim Acta 46: 491-50 I
Nelson DM, Trt!guer P, Brzenzinski MA, Leynaert A,
Queguiner B (1995) Production and dissolution of
biogenic silica in the ocean: Revised global estimates,
comparison with regional data and realtionship to
biogenic sedimentation, Global Biogeochem Cycles
9:359-372
NUrnberg D (1995) Magnesium in tests of Neogloboquadrina pachyderma sinistral from high northern
and southern latitudes, J Foram Res 25: 350-368
NUrnberg D, Bijma J, Hemleben C (1996a) Assessing the
reliability of magnesium in foraminiferal calcite as a
proxy for water mass temperatures, Geochim
Cosmochim Acta 60: 803-814
NUrnberg D, Bijma J, Hemleben C (1996b) Erratum,
Geochim Cosmochim Acta 60: 2483-2484
Oberhansli H, Benier C, Meinecke G, Schmidt H, Schneider R, Wefer G (1992) Planktic foraminifers as tracers of ocean currents in the eastern South Atlantic,
Paleoceanography 7: 607-632
O'Neil JR, Clayton RN, Mayeda TK (1969) Oxygen isotope fractionation in divalent metal carbonates, J
ChemPhys51: 5547-5558
Oppo DW, Fairbanks RG (1989) Carbon isotope composition of tropical surface water during the past 22,000
years. Palaeoceanography 4: 333-351
Oppo DW, Rosenthal Y (1994) Cd/Ca changes in a deep
Cape Basin core over the past 730,000 years: Response of circumpolar deepwater variability to
nothern hemisphere ice sheet melting?
Paleoceanography 9: 661-675
Oppo DW, Fairbanks RG, Gordon AL, Shackleton NJ
(1990) Late pleistocene southern ocean C 13 variability, Paleoceanography 5: 43-54
Ortiz JD, Mix AC (1997) Comparison ofImbrie-Kipp
transfer function and modern analog temperature
estimates using sediment trap and core top foraminiferal faunas, Paleoceanography 12: 175-190
Owens NJP (1987) Natural variations in l5N in the marine environment. Adv Mar Bioi 24: 390-451
Palmer MR, Edmond JM (1989) The strontium isotope
budget of the modem ocean, Earth Planet Sci Lett
92: 11-26
Parker FL (1958) Eastern Mediterranean foraminifera,
Reports ofthe Swedish Deep-Sea Expedition, 19471948,8: 217-283
Parker FL, Berger WH (1971) Faunal and solution patterns of planktonic foraminifera in surface sediments
of the South Pacific, Deep-Sea Res 18: 73-107
Pay tan A, Kastner M (1996) Benthic Ba fluxes in the
central equatorial Pacific, implications for the oceanic Bacycle, Earth Planet Sci Lett 142: 439-450
Pay tan A, Kastner M, Martin EE, Macdougall JD,
Herbert T (1993) Marine barite as a monitor of
seawater strontium isotope composition, Nature 366:
445-449
Paytan A, Kastner M, Chavez FP (1996) Glacial to Interglacial fluctuations in productivity in the Equatorial
Pacific as indicated by marine barite, Science 274:
1355-1357
Peltier WR, Tushingham AM (1989) Global sea level rise