Clues to Ocean History: a BriefOverview of Proxies
47
vegetation belts. "Meteor" Forsch Ergebn C 40:
87-135
Howard WR, Prell WL (1992) Late Quaternary surface
circulation of the southern indian ocean and its relationship to orbital variations. Paleoceanography
7:79-117
Hutchins DA, Bruland KW (1998) Iron-limited diatom
growth and Si:N uptake ratios in a coastal upwelling
regime. Nature 393: 561-564
Hutson WH (1977) Transfer functions underno-analog
conditions: Experiments with Indian Ocean planktonic foraminifera. Quat Res 8: 355-367
Hutson WH (1980) The Agulhas current during the late
Pleistocene: analysis of modem faunal analogs.
Science 207: 64-66
Imbrie J, Kipp NG (1971) A new micropaleontological
method for quantitative paleolimatology: Application to a Late Pleistocene Carribian core. In: Turekian
K (ed) The Late Cenozoic Glacial Ages. Yale Univ
Press, New Haven, Conn, pp 71-181
Imbrie J, Hays ID, 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 marine /i"0 record.
In: Berger A, Imbrie J, Hays J, Kukla G, Saltzman B
(eds) Milankovitch and climate, Part I. D. Reidel,
Dordrecht, pp 269-305
JahnkeRA, Craven DB, GaillardJ-F (1994) The influence
of organic matter diagenesis on CaCO, dissolution
at the deep-sea floor. Geochim Cosmochim Acta 58:
2799-2809
Jansen JHF, vanIperenIM (1991) A 220,000-yearclimatic
record for the East Equatorial Atlantic ocean and
Equatorial Africa: Evidence from diatom and opal
phytoliths in the Zaire (Congo) deep-sea fan.
Paleoceanography 6: 573-591
Jansen JHF, Anderliesten C, Houston CM, de Jong
AFM, van derBorg K, van Iperen IM (1989) Aridity
in tropical Africa during the last 225,000 years, a
record of phytoliths/freshwater diatoms from the
Zaire (Congo) deep-sea fan (northeast Angola
Basin). Radiocarbon 31: 557-569
Jasper JP, Hayes IM (1990) A carbon isotope record of
C0 2 1eveis during the Late Quaternary. Nature 347:
462464
Jasper JP, Hayes JM (1994) Reconstruction of
paleoceanic pC0 2 1eveis from carbon isotopic compositions of sedimentary biogenic components. In:
Zahn R, Pedersen TF, Kaminski M, Labeyrie L (eds)
Carbon Cycling in the Glacial Ocean: Constraints on
the Oceans' Role in Global Change. NATO ASI Series, Elsevier, pp 323-341
Jasper JP, Hayes IM, Mix AC, Prahl FG (1994) Photosynthetic fractionation of l3C and concentrations of
dissolved CO 2 in the central equatorial pacific during the last 255,000 years. Paleoceanography 9:
781-798
Johnson TC, Hamilton EL, Berger WH (1977) Physical
properties of calcareous ooze: control by dissolution at depth. Mar Geo124: 259-277
Jouzel J, Barkov NI, Bamola IM, Bender M, Chappellaz
J, Genthon C, Kotlyakov VM, Lipenkov V, Lorius C,
Petit JR, Raynaud D, Raisbeck G, Ritz C, Sowers T,
Stievenard M, Yiou F, Yiou P (1993) Extending the
Vostok ice-core record of palaeoclimate to the penultimate glacial period. Nature 364: 407-412
Kakihana H, Kotaka M, Satoh S, Nomura M, Okamota
M (1977) Fundamental studies on the ion-exchange
separation of boron isotopes. Bull Chern Soc Jpn 50:
158-163
Kalberer M, FischerG, Piitzold J, Donner B, Segl M, Wefer
G (1993) Seasonal sedimentation and stable isotope
record of pteropods off Cap Blanc. Mar Geol 113:
305-320
Karl D, Letelier R, Tupas L, Dore J, Christian J, Hebel D
(1997) The role of nitrogen fIXation in biogeochemical
cycling in the subtropical North Pacific Ocean. Nature388: 533-538
Keir RS (1991) The effect of vertical nutrient redistribution on surface ocean /il3C. Global Biogeochem
Cycles 5: 351-358
Kitazato H (1994) Foraminiferal microhabitats in four
marine environments around Japan. Mar
Micropaleontol24: 29-41
Klovan JE, Imbrie J (1971) An algorhythm an FORTRAN
IV program for large scale Q-mode factor analysis. J
Int Assoc Math Geol3: 61-77
Klump J, Hebbeln D, Wefer G (subm) The impact of sediment provenance on barium-based productivity estimates. Geochim Cosmochim Acta
Kroon D, Ganssen G (1988) The planktic /il3C record,
upwelling and climate. In: Brummer GJA, Kroon D
(eds) Planktonic Foraminifera as Tracers of OceanClimate History. Free University Press, Amsterdam,
pp335-346
Kroon D, Ganssen G (1989) Northern indian ocean
upwelling cells and the stable isotope composition
ofliving planktonic foraminifers. Deep-Sea Res 36:
1219-1236
Kroopnick P (1980) The distribution of l3 C in the Atlantic Ocean. Earth Planet Sci Lett 49: 469-484
Kroopnick P (1985) The distribution of l3C oO;C0 2 in
the worlds ocean. Deep-Sea Res 32: 57-84
Kumar N, Anderson RF, Mortlock RA, Froelich PN,
47
vegetation belts. "Meteor" Forsch Ergebn C 40:
87-135
Howard WR, Prell WL (1992) Late Quaternary surface
circulation of the southern indian ocean and its relationship to orbital variations. Paleoceanography
7:79-117
Hutchins DA, Bruland KW (1998) Iron-limited diatom
growth and Si:N uptake ratios in a coastal upwelling
regime. Nature 393: 561-564
Hutson WH (1977) Transfer functions underno-analog
conditions: Experiments with Indian Ocean planktonic foraminifera. Quat Res 8: 355-367
Hutson WH (1980) The Agulhas current during the late
Pleistocene: analysis of modem faunal analogs.
Science 207: 64-66
Imbrie J, Kipp NG (1971) A new micropaleontological
method for quantitative paleolimatology: Application to a Late Pleistocene Carribian core. In: Turekian
K (ed) The Late Cenozoic Glacial Ages. Yale Univ
Press, New Haven, Conn, pp 71-181
Imbrie J, Hays ID, 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 marine /i"0 record.
In: Berger A, Imbrie J, Hays J, Kukla G, Saltzman B
(eds) Milankovitch and climate, Part I. D. Reidel,
Dordrecht, pp 269-305
JahnkeRA, Craven DB, GaillardJ-F (1994) The influence
of organic matter diagenesis on CaCO, dissolution
at the deep-sea floor. Geochim Cosmochim Acta 58:
2799-2809
Jansen JHF, vanIperenIM (1991) A 220,000-yearclimatic
record for the East Equatorial Atlantic ocean and
Equatorial Africa: Evidence from diatom and opal
phytoliths in the Zaire (Congo) deep-sea fan.
Paleoceanography 6: 573-591
Jansen JHF, Anderliesten C, Houston CM, de Jong
AFM, van derBorg K, van Iperen IM (1989) Aridity
in tropical Africa during the last 225,000 years, a
record of phytoliths/freshwater diatoms from the
Zaire (Congo) deep-sea fan (northeast Angola
Basin). Radiocarbon 31: 557-569
Jasper JP, Hayes IM (1990) A carbon isotope record of
C0 2 1eveis during the Late Quaternary. Nature 347:
462464
Jasper JP, Hayes JM (1994) Reconstruction of
paleoceanic pC0 2 1eveis from carbon isotopic compositions of sedimentary biogenic components. In:
Zahn R, Pedersen TF, Kaminski M, Labeyrie L (eds)
Carbon Cycling in the Glacial Ocean: Constraints on
the Oceans' Role in Global Change. NATO ASI Series, Elsevier, pp 323-341
Jasper JP, Hayes IM, Mix AC, Prahl FG (1994) Photosynthetic fractionation of l3C and concentrations of
dissolved CO 2 in the central equatorial pacific during the last 255,000 years. Paleoceanography 9:
781-798
Johnson TC, Hamilton EL, Berger WH (1977) Physical
properties of calcareous ooze: control by dissolution at depth. Mar Geo124: 259-277
Jouzel J, Barkov NI, Bamola IM, Bender M, Chappellaz
J, Genthon C, Kotlyakov VM, Lipenkov V, Lorius C,
Petit JR, Raynaud D, Raisbeck G, Ritz C, Sowers T,
Stievenard M, Yiou F, Yiou P (1993) Extending the
Vostok ice-core record of palaeoclimate to the penultimate glacial period. Nature 364: 407-412
Kakihana H, Kotaka M, Satoh S, Nomura M, Okamota
M (1977) Fundamental studies on the ion-exchange
separation of boron isotopes. Bull Chern Soc Jpn 50:
158-163
Kalberer M, FischerG, Piitzold J, Donner B, Segl M, Wefer
G (1993) Seasonal sedimentation and stable isotope
record of pteropods off Cap Blanc. Mar Geol 113:
305-320
Karl D, Letelier R, Tupas L, Dore J, Christian J, Hebel D
(1997) The role of nitrogen fIXation in biogeochemical
cycling in the subtropical North Pacific Ocean. Nature388: 533-538
Keir RS (1991) The effect of vertical nutrient redistribution on surface ocean /il3C. Global Biogeochem
Cycles 5: 351-358
Kitazato H (1994) Foraminiferal microhabitats in four
marine environments around Japan. Mar
Micropaleontol24: 29-41
Klovan JE, Imbrie J (1971) An algorhythm an FORTRAN
IV program for large scale Q-mode factor analysis. J
Int Assoc Math Geol3: 61-77
Klump J, Hebbeln D, Wefer G (subm) The impact of sediment provenance on barium-based productivity estimates. Geochim Cosmochim Acta
Kroon D, Ganssen G (1988) The planktic /il3C record,
upwelling and climate. In: Brummer GJA, Kroon D
(eds) Planktonic Foraminifera as Tracers of OceanClimate History. Free University Press, Amsterdam,
pp335-346
Kroon D, Ganssen G (1989) Northern indian ocean
upwelling cells and the stable isotope composition
ofliving planktonic foraminifers. Deep-Sea Res 36:
1219-1236
Kroopnick P (1980) The distribution of l3 C in the Atlantic Ocean. Earth Planet Sci Lett 49: 469-484
Kroopnick P (1985) The distribution of l3C oO;C0 2 in
the worlds ocean. Deep-Sea Res 32: 57-84
Kumar N, Anderson RF, Mortlock RA, Froelich PN,