226
Wolffetal.
Imbrie J, Kipp NG (1971) A new micropaleontological
method for quantitative paleoclimatology: application to a Late Pleistocene Caribbean core. In:
Turekian KK (ed) Late Cenocoic glacial ages. Yale
University Press, New Haven, pp 71-181
Imbrie J, van Donk J, Kipp NG (1973) Paleoclimatic investigation of a late Pleistocene Caribean deep-sea
core: Comparison of isotopic and faunal methods.
Quat Res 3: 10-38
Imbrie J, McIntyre A, Mix A (1989) Oceanic response to
orbital forcing in the late Quaternary: Observational
and experimental strategies. In: Berger A (ed) Climate
and Geo- Sciences. Kluwer Academic, Dordrecht,
pp 121-164
Jouzel J, Koster RD, Suozzo RJ, Russell GL (1994) Stable water isotope behaviour during the last glacial
maximum: A general circulation model analysis. J
Geophy Res 99: 25791-25801
Kallel N, PaterneM, Labeyrie L, Duplessy J, ArnoldM
(1997) Temperature and salinity records of the
Tyrrhenian Sea during the last 18,000 years.
Pa1aeogeogr Pa1aeoclimatol Pa1aeoecol135: 97-108
Keigwin LD (1996) The Little Ice Age and Medieval
Warm period in the Sargasso Sea. Science 274:
1504-1508
Kipp N G (1976) New transfer function for estimating past
sea-surface conditions from sea-bed distribution of
planktonic foraminiferal assemblages in the North
Atlantic. In: Cline RM, Hays JD (eds) Investigation
of late Quaternary Paleoceanography and
Paleoclimatology. Geol Soc Amer Mem, pp 3-41
Labeyrie LD, Duplessy JC, Blanc PL (1987) Variations in
mode of formation and temperature of oceanic deep
waters over the past 125,000 years. Nature 327:
477482
Lautenschlager M, Mikolajewicz U, Maier-Reimer E,
Heinze C (1992) Application of ocean models for the
interpretation of AGCM experiments on the climate
of the last glacial maximum. Paleoceanography 7:
769-782
Le J (1993) Paleotemperature estimation methods: Sensitivity test on two western equatorial Pacific cores.
Quat Sci Rev 11: 801-820
Levitus S (1982) Climatological Atlas of the World Ocean.
NOAA Professional Paper 13: 1-173
Levitus S, Boyer TP (1994) World Ocean Atlas 1994,
Volume 4: Temperature, pp 1-117
Levitus S, Burgett R, Boyer TP (1994) World Ocean Atlas
1994, Volume 3: Salinity,pp 1-99
Lorenz S, Grieger B, Helbig P, Herterich K (1996) Investigating the sensitivity of the Atmospheric General
Circulation Model ECHAM 3 to paleoclimatic
boundary conditions. Geol Rundsch 85: 513-524.
Maslin MA, Shackleton NJ, Pflaumann U (1995) Surface
water temperature, salinity, and density changes in
the northeast Atlantic during the last 45,000 years:
Heinrich events, deep water formation, and climatic
rebounds. Paleoceanography 10: 527-544
Melles M (1991) Paliiozeanographie im Spiitquartiir am
Kontinentalrand des sud lichen Weddellmeeres,
Antarktis. Ber Polarforsch Bremerhaven 81, pp 1-190
Merlivat L, Jouze1 J (1979) Global climatic interpretation
of the deuterium-oxygen-18 relationship for precipitation. J Geophys Res 84: 5029-5033
Mix AC (1987) The oxygen-isotope record of glaciation.
In: Ruddiman WF, Wright HEJ (eds) North America
and adjacent oceans during the last deglaciation.
Geol Soc Amer, Boulder, Colorado,pp 111-135
Mix AC, Ruddiman WF (1985) Structure and timing of
the last deglaciation: Oxygen isotope evidence. Quat
Sci Rev 4: 59-108
Mulitza S (1994) Spiitquartiire Variationen der
oberfliichennahen Hydrographie im westlichen
iiquatorialen Atlantik. Ber Fachber Geowiss Univ
Bremen 57,pp 1-97
Mulitza S, WolffT, Piitzold J, Hale W, Wefer G (1998)
Temperature sensitivity of planktonic foraminifera
and its influence on the oxygen isotope record. Mar
Micropa!eontol33 :223-240
Muller PJ, Schneider R, Ruhland G (1994) Late Quaternary PCO, 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
New York,pp 343-366
N aidu PD (1993) Distribution patterns of recent planktonic foraminifera in surface sediments of the western continental margin ofIndia. Mar Geol 110:
403418
Niebler HS (1995) Reconstruction of palaeo-environmental parameters using stable isotopes and faunal assemblages of planktonic foraminifera in the South
Atlantic Ocean. Ber Polarforsch Bremerhaven 167,
ppl-198
Overpeck JT, Webb III T, Prentice, IC (1985) Quantitative interpretation offossil pollen spectra: Dissimilarity coefficients and the method of modern analogs.
Quat Res 23: 87-108
Wolffetal.
Imbrie J, Kipp NG (1971) A new micropaleontological
method for quantitative paleoclimatology: application to a Late Pleistocene Caribbean core. In:
Turekian KK (ed) Late Cenocoic glacial ages. Yale
University Press, New Haven, pp 71-181
Imbrie J, van Donk J, Kipp NG (1973) Paleoclimatic investigation of a late Pleistocene Caribean deep-sea
core: Comparison of isotopic and faunal methods.
Quat Res 3: 10-38
Imbrie J, McIntyre A, Mix A (1989) Oceanic response to
orbital forcing in the late Quaternary: Observational
and experimental strategies. In: Berger A (ed) Climate
and Geo- Sciences. Kluwer Academic, Dordrecht,
pp 121-164
Jouzel J, Koster RD, Suozzo RJ, Russell GL (1994) Stable water isotope behaviour during the last glacial
maximum: A general circulation model analysis. J
Geophy Res 99: 25791-25801
Kallel N, PaterneM, Labeyrie L, Duplessy J, ArnoldM
(1997) Temperature and salinity records of the
Tyrrhenian Sea during the last 18,000 years.
Pa1aeogeogr Pa1aeoclimatol Pa1aeoecol135: 97-108
Keigwin LD (1996) The Little Ice Age and Medieval
Warm period in the Sargasso Sea. Science 274:
1504-1508
Kipp N G (1976) New transfer function for estimating past
sea-surface conditions from sea-bed distribution of
planktonic foraminiferal assemblages in the North
Atlantic. In: Cline RM, Hays JD (eds) Investigation
of late Quaternary Paleoceanography and
Paleoclimatology. Geol Soc Amer Mem, pp 3-41
Labeyrie LD, Duplessy JC, Blanc PL (1987) Variations in
mode of formation and temperature of oceanic deep
waters over the past 125,000 years. Nature 327:
477482
Lautenschlager M, Mikolajewicz U, Maier-Reimer E,
Heinze C (1992) Application of ocean models for the
interpretation of AGCM experiments on the climate
of the last glacial maximum. Paleoceanography 7:
769-782
Le J (1993) Paleotemperature estimation methods: Sensitivity test on two western equatorial Pacific cores.
Quat Sci Rev 11: 801-820
Levitus S (1982) Climatological Atlas of the World Ocean.
NOAA Professional Paper 13: 1-173
Levitus S, Boyer TP (1994) World Ocean Atlas 1994,
Volume 4: Temperature, pp 1-117
Levitus S, Burgett R, Boyer TP (1994) World Ocean Atlas
1994, Volume 3: Salinity,pp 1-99
Lorenz S, Grieger B, Helbig P, Herterich K (1996) Investigating the sensitivity of the Atmospheric General
Circulation Model ECHAM 3 to paleoclimatic
boundary conditions. Geol Rundsch 85: 513-524.
Maslin MA, Shackleton NJ, Pflaumann U (1995) Surface
water temperature, salinity, and density changes in
the northeast Atlantic during the last 45,000 years:
Heinrich events, deep water formation, and climatic
rebounds. Paleoceanography 10: 527-544
Melles M (1991) Paliiozeanographie im Spiitquartiir am
Kontinentalrand des sud lichen Weddellmeeres,
Antarktis. Ber Polarforsch Bremerhaven 81, pp 1-190
Merlivat L, Jouze1 J (1979) Global climatic interpretation
of the deuterium-oxygen-18 relationship for precipitation. J Geophys Res 84: 5029-5033
Mix AC (1987) The oxygen-isotope record of glaciation.
In: Ruddiman WF, Wright HEJ (eds) North America
and adjacent oceans during the last deglaciation.
Geol Soc Amer, Boulder, Colorado,pp 111-135
Mix AC, Ruddiman WF (1985) Structure and timing of
the last deglaciation: Oxygen isotope evidence. Quat
Sci Rev 4: 59-108
Mulitza S (1994) Spiitquartiire Variationen der
oberfliichennahen Hydrographie im westlichen
iiquatorialen Atlantik. Ber Fachber Geowiss Univ
Bremen 57,pp 1-97
Mulitza S, WolffT, Piitzold J, Hale W, Wefer G (1998)
Temperature sensitivity of planktonic foraminifera
and its influence on the oxygen isotope record. Mar
Micropa!eontol33 :223-240
Muller PJ, Schneider R, Ruhland G (1994) Late Quaternary PCO, 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
New York,pp 343-366
N aidu PD (1993) Distribution patterns of recent planktonic foraminifera in surface sediments of the western continental margin ofIndia. Mar Geol 110:
403418
Niebler HS (1995) Reconstruction of palaeo-environmental parameters using stable isotopes and faunal assemblages of planktonic foraminifera in the South
Atlantic Ocean. Ber Polarforsch Bremerhaven 167,
ppl-198
Overpeck JT, Webb III T, Prentice, IC (1985) Quantitative interpretation offossil pollen spectra: Dissimilarity coefficients and the method of modern analogs.
Quat Res 23: 87-108