Clues to Ocean History: a Brief Overview of Proxies
49
Mangerud I, Lie SE, Fumes H, Kristiansen JL, Loemo L
(1984) A Younger Dryas ash bed in western Norway,
and ist possible correlations with tephra in cores
from the Norwegian Sea and the North Atlantic. Quat
Res21: 85-104
Mangini A, Lomitschka M, Eichstaedter R, Frank N,
Vogler S, Bonani G, Hajdas I, Piitzold J (1998) Coral
provides way to age deepwater. Nature 392: 347-348
Marcantonio F et al. (1995) A comparative study of accumulation rates derived by He and Th isotope analysis of marine sediments. Earth Planet Sci Lett 133:
549-555
Marcantonio F, Anderson RF, Stute M, Kumar N,
Schlosser P, Mix A (1996) Extra-terrestrial 'He as a
tracer of marine sediment transport and accumulation. Nature 383: 705-707
Martin IH, Fitzwater SE (1988) Iron deficiency limits
phytoplankton growth in the north-east Pacific
subarctic. Nature 331: 341-343
Martinson DG, Pisias NG, Hays JD, Imbrie I, Moore TC,
Shackleton NI (1987) Age dating and the orbital
theory of the ice ages: development of a high-resolution 0 to 300,000-year chronostratigraphy. Quat Res
27: 1-29.
Mashiotta TA, LeaDW, Spero HJ (1997) Experimental
determination of cadmium uptake in shells of the
planktonic foraminifera Orbulina universa and
Globigerina bulloides: implications for surface water paleoreconstructions. Geochim Cosmochim Acta
61: 4053-4065
Mashiotta TA, LeaDW, Spero HJ (subm) Using planktic
Mg paleothermometry to determine glacial-interglacial changes in seawater 1)180. Earth Planet Sci Lett
Maslin MA, Haug GH, Sarnthein M, Tiedemann R,
Erlenkeuser H, Stax R (1995) Northwest Pacific site
882: the initiation of northern hemisphere galciation.
In: Rea DK, Basov lA, Scholl DW, Allan IF (eds),
Proc ODP Sci Results 145, College Station, TX,
pp315-332
McCorkle DC, Keigwin LD, Corliss BH, Emerson SR
(1990) The influence of microhabitats on the carbon
isotopic composition of deep-sea benthic
foraminifera. Paleoceanography 5: 161-185
McCorkle DC, Martin PA, Lea DW, Klinkhammer GP
(1995) Evidence of a dissolution effect on benthic
foraminiferal shell chemistry -1)13C-, Cd/Ca, Ba/Ca,
and Sr/Ca results from the Ontong Java Plateau.
Paleoceanography 10: 699-714
McCrea 1M (1950) On the isotopic chemistry of carbonates and a paleotemperature scale. I Chern Phys 18:
849-857
McElroy MB (1983) Marine biological controls on atmospheric CO 2 and climate. Nature 302: 328-329
Meyers PA (1994) Preservation of elemental and isotopic source identification of sedimentary organic
matter. Chern Geo1114: 289-302
Miller KG, Lohmann GP (1982) Environmental distribution of recent benthic foraminifera on the northeast
united states continental slope. Geol Soc Amer Bull
93:200-206
Mitsuguchi T, Matsumoto E, Abe 0, Uchida T, Isdale
PJ (1996) Mg/Ca thermometry in coral skeletons.
Science 274: 961-963
Mix AC (l989a) Influence of productivity variations on
long - term atmospheric COr Nature 337: 541-544
Mix AC (1989b) Pleistocene paleoproductivity: Evidence
from organic carbon and foraminiferal species. In:
Berger WH, Smetacek VS, Wefer G (eds) Productivity of the Ocean: Present and Past. J Wiley & Sons,
New York, pp 313-340
Montoya JP (1994) Nitrogen isotope fractionation in the
modem ocean: implications for the sedimentary
record. In: Zahn R, Pedersen TF, Kaminski MA,
Labeyrie L (eds) Carbon Cycling in the Glacial Ocean:
Constaints on the Ocean's Role in Global Change.
NATO ASI Series, Vol 17, Springer, Berlin Heidelberg
New YOIk, pp 259-279
Montoya JP, Horrigan SG, McCarthy 11 (1991) Rapid,
storm-induced changes in the natural abundance of
15N in a planktonic ecosystem. Geochim Cosmochim
Acta 55: 3627-3638
Moore WS, Dymond J (1988) Correlation of 2lO Pb removal with organic carbon fluxes in the Pacific
Ocean. Nature 331: 339-341
Morley 11 (1979) A transfer function for estimating
paleoceanographic conditions based on deep-sea
surface sediment distribution of radiolarian assemblages in the South Atlantic. Quat Res 12: 381-395
Mortlock RA, Charles CD, Froelich PN, Zibello MA,
Salzman I, Hayes JD, Burckle LH (1991) Evidence for
lower productivity in the Antarctic Ocean during the
last glaciation. Nature 351: 220-223
Mulitza S, Diirkoop A, Hale W, Wefer G, Niebler HS
(1997) Planktonic foraminifera as recorders of past
surface-water stratification. Geology 25: 335-338
Miiller P J (1977) C/N ratios in Pacific deep-sea
sediments: effects of inorganic ammonium and organic nitrogen compounds sorbed by clays.
Geochim CosmochimActa41: 765-776
MUller PI, Suess E (1977) Interaction of organic compounds with calcium carbonate. 1. Amino acid composition of sorbed layers. Geochim Cosmochim Acta
41:941-949
Miiller PJ, Suess E (1979) Productivity, sedimentation
49
Mangerud I, Lie SE, Fumes H, Kristiansen JL, Loemo L
(1984) A Younger Dryas ash bed in western Norway,
and ist possible correlations with tephra in cores
from the Norwegian Sea and the North Atlantic. Quat
Res21: 85-104
Mangini A, Lomitschka M, Eichstaedter R, Frank N,
Vogler S, Bonani G, Hajdas I, Piitzold J (1998) Coral
provides way to age deepwater. Nature 392: 347-348
Marcantonio F et al. (1995) A comparative study of accumulation rates derived by He and Th isotope analysis of marine sediments. Earth Planet Sci Lett 133:
549-555
Marcantonio F, Anderson RF, Stute M, Kumar N,
Schlosser P, Mix A (1996) Extra-terrestrial 'He as a
tracer of marine sediment transport and accumulation. Nature 383: 705-707
Martin IH, Fitzwater SE (1988) Iron deficiency limits
phytoplankton growth in the north-east Pacific
subarctic. Nature 331: 341-343
Martinson DG, Pisias NG, Hays JD, Imbrie I, Moore TC,
Shackleton NI (1987) Age dating and the orbital
theory of the ice ages: development of a high-resolution 0 to 300,000-year chronostratigraphy. Quat Res
27: 1-29.
Mashiotta TA, LeaDW, Spero HJ (1997) Experimental
determination of cadmium uptake in shells of the
planktonic foraminifera Orbulina universa and
Globigerina bulloides: implications for surface water paleoreconstructions. Geochim Cosmochim Acta
61: 4053-4065
Mashiotta TA, LeaDW, Spero HJ (subm) Using planktic
Mg paleothermometry to determine glacial-interglacial changes in seawater 1)180. Earth Planet Sci Lett
Maslin MA, Haug GH, Sarnthein M, Tiedemann R,
Erlenkeuser H, Stax R (1995) Northwest Pacific site
882: the initiation of northern hemisphere galciation.
In: Rea DK, Basov lA, Scholl DW, Allan IF (eds),
Proc ODP Sci Results 145, College Station, TX,
pp315-332
McCorkle DC, Keigwin LD, Corliss BH, Emerson SR
(1990) The influence of microhabitats on the carbon
isotopic composition of deep-sea benthic
foraminifera. Paleoceanography 5: 161-185
McCorkle DC, Martin PA, Lea DW, Klinkhammer GP
(1995) Evidence of a dissolution effect on benthic
foraminiferal shell chemistry -1)13C-, Cd/Ca, Ba/Ca,
and Sr/Ca results from the Ontong Java Plateau.
Paleoceanography 10: 699-714
McCrea 1M (1950) On the isotopic chemistry of carbonates and a paleotemperature scale. I Chern Phys 18:
849-857
McElroy MB (1983) Marine biological controls on atmospheric CO 2 and climate. Nature 302: 328-329
Meyers PA (1994) Preservation of elemental and isotopic source identification of sedimentary organic
matter. Chern Geo1114: 289-302
Miller KG, Lohmann GP (1982) Environmental distribution of recent benthic foraminifera on the northeast
united states continental slope. Geol Soc Amer Bull
93:200-206
Mitsuguchi T, Matsumoto E, Abe 0, Uchida T, Isdale
PJ (1996) Mg/Ca thermometry in coral skeletons.
Science 274: 961-963
Mix AC (l989a) Influence of productivity variations on
long - term atmospheric COr Nature 337: 541-544
Mix AC (1989b) Pleistocene paleoproductivity: Evidence
from organic carbon and foraminiferal species. In:
Berger WH, Smetacek VS, Wefer G (eds) Productivity of the Ocean: Present and Past. J Wiley & Sons,
New York, pp 313-340
Montoya JP (1994) Nitrogen isotope fractionation in the
modem ocean: implications for the sedimentary
record. In: Zahn R, Pedersen TF, Kaminski MA,
Labeyrie L (eds) Carbon Cycling in the Glacial Ocean:
Constaints on the Ocean's Role in Global Change.
NATO ASI Series, Vol 17, Springer, Berlin Heidelberg
New YOIk, pp 259-279
Montoya JP, Horrigan SG, McCarthy 11 (1991) Rapid,
storm-induced changes in the natural abundance of
15N in a planktonic ecosystem. Geochim Cosmochim
Acta 55: 3627-3638
Moore WS, Dymond J (1988) Correlation of 2lO Pb removal with organic carbon fluxes in the Pacific
Ocean. Nature 331: 339-341
Morley 11 (1979) A transfer function for estimating
paleoceanographic conditions based on deep-sea
surface sediment distribution of radiolarian assemblages in the South Atlantic. Quat Res 12: 381-395
Mortlock RA, Charles CD, Froelich PN, Zibello MA,
Salzman I, Hayes JD, Burckle LH (1991) Evidence for
lower productivity in the Antarctic Ocean during the
last glaciation. Nature 351: 220-223
Mulitza S, Diirkoop A, Hale W, Wefer G, Niebler HS
(1997) Planktonic foraminifera as recorders of past
surface-water stratification. Geology 25: 335-338
Miiller P J (1977) C/N ratios in Pacific deep-sea
sediments: effects of inorganic ammonium and organic nitrogen compounds sorbed by clays.
Geochim CosmochimActa41: 765-776
MUller PI, Suess E (1977) Interaction of organic compounds with calcium carbonate. 1. Amino acid composition of sorbed layers. Geochim Cosmochim Acta
41:941-949
Miiller PJ, Suess E (1979) Productivity, sedimentation