Alkenone 1)l3C as a Proxy for Past PCO, in Surface Waters
487
Miiller PI, Kirst G, Ruhland G, von Storch I, Rosell-Mele
A (1998) Calibration of the alkenone paleotemperature index Uk' 37 based on core-tops from the
eastern South Atlantic and the global ocean (60 0 N60 0 S), Geochim Cosmochim 62: 1757-1772
Murray JW, Johnson E, Garside C (1995) AU,S, JGOFS
Process Study in the equatorial Pacific (EqPac):
Introduction, Deep-Sea Res II 42: 275-293
Nimer NA, MerrettMJ (1996) The developmentofa CO,concentrating mechanism in Erniliania huxleyi, New
Phytol 133: 383-389
Nimer NA, MerretMJ, Brownlee C (1996) Inorganic carbon transport in relation to culture age and inorganic
carbon concentration in a high-calcifying strain of
Erniliania huxleyi (Prymnesiophyceae), J Phycol32:
813-818
Nimer NA, Iglesias-Rodriguez MD, Merrett MJ (1997)
Bicarbonate utilization by marine phytoplankton
species, J Phycol33: 625-631
Paasche E (1964) A tracer study of the inorganic carbon
uptake during coccolith formation and photosynthesis in the coccolithophorid Coccolithus huxleyi,
Physiol Plant (Suppl) 3: 1-82
Paillard D, Ghil M, Le Treut H (1993) Dissolved organic
matter and the glacial-interglacial pCO, problem,
Global Biogeochem Cycles 7: 901-914
Pancost RD, Freeman KH, Wakeham SG, Robertson CY
(1997) Controls on carbon isotope fractionation by
diatoms in the Peru upwelling region, Geochim
CosmochimActa61: 4983-4991
Pedersen TF, Nielsen B, Pickering M (1991) Timing of
Late Quaternary productivity pulses in the Panama
Basin and implications for atmospheric CO"
Paleoceanography 6: 657-677
Popp BN, Takigiku R, Hayes 1M, Louda JW, Baker EW
(1989) The post-paleozoic chronology and mechanism of l3e depletion in primary marine organic matter, Amer J Sci 289: 436-454
Popp BN, Parekh P, Tilbrook B, Bidagare RR, Laws EA
(1997) Organic carbon /i l3 C variations in sedimentary
rocks as chemostratigraphic and paleoenvironmental
tools, Palaeogeogr Palaeoclimat Palaeoecol 132:
119-132
Popp BN, Kenig F, Wakeham SG, Laws EA, Bidigare RR
(1998a) Does growth rate effect ketone unsaturation
and intracellular carbon isotopic variability in
Erniliania huxleyi? Paleoceanography 13: 35-41
Popp BN, Laws EA, Bidigare RR, Dore JE, Hanson KL,
Wakeham SG (1998b) Effect of phytoplankton cell
geometry on carbon isotopic fractionation, Geochim
Cosmochim Acta 62: 69-77
Rau GH (1994) Variations in sedimentary organic 1)l3C
as a proxy for past changes in ocean and atmospheric
CO, concentrations, In: ZahnR, et aL (eds) Carbon
Cycling in the Glacial Ocean: Constraints on the
Ocean's Role in Global Change, NATO ASI Series I
17, Springer, Berlin Heidelberg New York, pp 307-321
Rau GH, Sweeney RE, DesMarais DJ (1989) Latitudinal
variations in plankton 1)\3C: Implications for CO, and
productivity in past oceans. Deep-Sea Res 341:
516-518
Rau GH, Froehlich PN, Takahashi T, DesMarais DJ (1991)
Does sedimentary organic 1)l3C record variation in
Quaternary ocean [CO,(aq)]? Paleoceanography 6:
335-347
Rau GH, Takahashi T, DesMarais DJ, Repta DJ, Martin
JH (1992) The relationship between 1)l3C of organic
matter and [CO,(aq)] in ocean surface water:
Data from a JGOFS site in the northeast Atlantic
Ocean and a model. Geochim Cosmochim Acta 56:
1413-1419
Rau GH, Riehesell U, Wolf-Gladrow D (1996) A model of
photosynthetic l3C fractionation by marine phytoplankton based on diffusive molecular CO, uptake.
Mar Ecol Prog Ser 133: 275-285
Rau GH, Riebesell U, Wolf-Gladrow D (1997) CO,,,, -dependent photosynthetic l3C fractionation in the
ocean: A model versus measurements. Global
Biogeochem Cycles 11: 267-278
RaveloAC, Fairbanks RG, Philander SGH (1990) Reconstructing tropical Atlantic hydrography using
planktonic foraminifera and an ocean model.
Paleoceanography 5: 409-431
Raven JA, Johnston AM (1991) Mechanisms of inorganic-carbon acquisition in marine phytoplankton
and their implications for the use of other resources,
LimnolOceanogr36: 1701-1714
Raymo ME, Horowitz M (1996) Organic carbon paleopeo, and marine-ice core correlations and chronology. Geophys Res Lett 23: 367-370
Robertson JE, Watson AJ, Langdon e, Ling RD, Wood
JW (1993) Diurinal variation in surface pCO, and 0,
at 60 0 N, 200W in the Nort Atlantic. Deep Sea Res II
40:409-422
Sabine CL, Wallace DWR, Millero FJ (1997) Survey of
CO, in the oceans reveals clues about global carbon
cycle. Eos, Transactions, American Geophysical
Union 78(5): SO-55
Sarmiento IS, Toggweiler JR (1984) A new model for the
role of the oceans in determining atmospheric pCO,.
Nature 308: 621-624
487
Miiller PI, Kirst G, Ruhland G, von Storch I, Rosell-Mele
A (1998) Calibration of the alkenone paleotemperature index Uk' 37 based on core-tops from the
eastern South Atlantic and the global ocean (60 0 N60 0 S), Geochim Cosmochim 62: 1757-1772
Murray JW, Johnson E, Garside C (1995) AU,S, JGOFS
Process Study in the equatorial Pacific (EqPac):
Introduction, Deep-Sea Res II 42: 275-293
Nimer NA, MerrettMJ (1996) The developmentofa CO,concentrating mechanism in Erniliania huxleyi, New
Phytol 133: 383-389
Nimer NA, MerretMJ, Brownlee C (1996) Inorganic carbon transport in relation to culture age and inorganic
carbon concentration in a high-calcifying strain of
Erniliania huxleyi (Prymnesiophyceae), J Phycol32:
813-818
Nimer NA, Iglesias-Rodriguez MD, Merrett MJ (1997)
Bicarbonate utilization by marine phytoplankton
species, J Phycol33: 625-631
Paasche E (1964) A tracer study of the inorganic carbon
uptake during coccolith formation and photosynthesis in the coccolithophorid Coccolithus huxleyi,
Physiol Plant (Suppl) 3: 1-82
Paillard D, Ghil M, Le Treut H (1993) Dissolved organic
matter and the glacial-interglacial pCO, problem,
Global Biogeochem Cycles 7: 901-914
Pancost RD, Freeman KH, Wakeham SG, Robertson CY
(1997) Controls on carbon isotope fractionation by
diatoms in the Peru upwelling region, Geochim
CosmochimActa61: 4983-4991
Pedersen TF, Nielsen B, Pickering M (1991) Timing of
Late Quaternary productivity pulses in the Panama
Basin and implications for atmospheric CO"
Paleoceanography 6: 657-677
Popp BN, Takigiku R, Hayes 1M, Louda JW, Baker EW
(1989) The post-paleozoic chronology and mechanism of l3e depletion in primary marine organic matter, Amer J Sci 289: 436-454
Popp BN, Parekh P, Tilbrook B, Bidagare RR, Laws EA
(1997) Organic carbon /i l3 C variations in sedimentary
rocks as chemostratigraphic and paleoenvironmental
tools, Palaeogeogr Palaeoclimat Palaeoecol 132:
119-132
Popp BN, Kenig F, Wakeham SG, Laws EA, Bidigare RR
(1998a) Does growth rate effect ketone unsaturation
and intracellular carbon isotopic variability in
Erniliania huxleyi? Paleoceanography 13: 35-41
Popp BN, Laws EA, Bidigare RR, Dore JE, Hanson KL,
Wakeham SG (1998b) Effect of phytoplankton cell
geometry on carbon isotopic fractionation, Geochim
Cosmochim Acta 62: 69-77
Rau GH (1994) Variations in sedimentary organic 1)l3C
as a proxy for past changes in ocean and atmospheric
CO, concentrations, In: ZahnR, et aL (eds) Carbon
Cycling in the Glacial Ocean: Constraints on the
Ocean's Role in Global Change, NATO ASI Series I
17, Springer, Berlin Heidelberg New York, pp 307-321
Rau GH, Sweeney RE, DesMarais DJ (1989) Latitudinal
variations in plankton 1)\3C: Implications for CO, and
productivity in past oceans. Deep-Sea Res 341:
516-518
Rau GH, Froehlich PN, Takahashi T, DesMarais DJ (1991)
Does sedimentary organic 1)l3C record variation in
Quaternary ocean [CO,(aq)]? Paleoceanography 6:
335-347
Rau GH, Takahashi T, DesMarais DJ, Repta DJ, Martin
JH (1992) The relationship between 1)l3C of organic
matter and [CO,(aq)] in ocean surface water:
Data from a JGOFS site in the northeast Atlantic
Ocean and a model. Geochim Cosmochim Acta 56:
1413-1419
Rau GH, Riehesell U, Wolf-Gladrow D (1996) A model of
photosynthetic l3C fractionation by marine phytoplankton based on diffusive molecular CO, uptake.
Mar Ecol Prog Ser 133: 275-285
Rau GH, Riebesell U, Wolf-Gladrow D (1997) CO,,,, -dependent photosynthetic l3C fractionation in the
ocean: A model versus measurements. Global
Biogeochem Cycles 11: 267-278
RaveloAC, Fairbanks RG, Philander SGH (1990) Reconstructing tropical Atlantic hydrography using
planktonic foraminifera and an ocean model.
Paleoceanography 5: 409-431
Raven JA, Johnston AM (1991) Mechanisms of inorganic-carbon acquisition in marine phytoplankton
and their implications for the use of other resources,
LimnolOceanogr36: 1701-1714
Raymo ME, Horowitz M (1996) Organic carbon paleopeo, and marine-ice core correlations and chronology. Geophys Res Lett 23: 367-370
Robertson JE, Watson AJ, Langdon e, Ling RD, Wood
JW (1993) Diurinal variation in surface pCO, and 0,
at 60 0 N, 200W in the Nort Atlantic. Deep Sea Res II
40:409-422
Sabine CL, Wallace DWR, Millero FJ (1997) Survey of
CO, in the oceans reveals clues about global carbon
cycle. Eos, Transactions, American Geophysical
Union 78(5): SO-55
Sarmiento IS, Toggweiler JR (1984) A new model for the
role of the oceans in determining atmospheric pCO,.
Nature 308: 621-624