Abstract
An eleven-box model of the ocean-atmosphere subsystem of the global carbon cycle is developed to study the potential contribution of continental rock weathering and oceanic sedimentation to variations of atmospheric CO2 pressure over glacial-interglacial timescales. The model is capable of reproducing the distribution of total dissolved inorganic carbon, total alkalinity, phosphate, δ13C, and Δ14C between the various ocean basins today, as well as the partial pressure of atmospheric CO2. A simple sedimentation scheme at 20 different depth levels drives carbonate deposition and dissolution as a function of the depths of carbonate and aragonite lysoclines in each ocean basins considered (Atlantic, Antarctic and Indo-Pacific). The coral-reef erosion-deposition cycle is also taken into account. Furthermore, a simple cycle of oceanic strontium isotopes has been added to this model to take advantage of the 87Sr/86Sr data recently published by Dia et al. (1992) for the last 300,000 years. These data emphasize the importance of weathering of continental silicate rocks at glacial-interglacial timescales. They are used to construct several scenarios of changes of continental weathering over the last glacial cycles. They suggest that the flux of alkalinity delivered to the ocean from continental silicate weathering may have been substantially larger during glacial times than today. We show that such variations of continental weathering may explain at least in part the observed changes of the partial pressure of atmospheric CO2 between glacial and interglacial periods.
Access this chapter
Tax calculation will be finalised at checkout
Purchases are for personal use only
Preview
Unable to display preview. Download preview PDF.
References
Barnola JM, Raynaud D, Korotkevich YS, Lorius C (1987) Vostok ice core provides 160,000 year record of atmospheric CO2. Nature 329: 408–414
Berger WH, Keir RS (1984) Glacial-Holocene changes in atmospheric CO2 and the deep-sea record. In: Hansen JE, Takahashi T (eds) Climate Processing and Climate Sensitivity. American Geophysical Union, Washington DC, (Geophysical Monograph Series, vol 29, p 337)
Berger WH, Killingley JS (1982) The Worthington effect and the origin of the Younger Dryas. J Mar Res 40:27–38
Berner RA, Lasaga AC, Garrels RM (1983) The carbonate-silicate geochemical cycle and its effect on the atmospheric carbon dioxide over the past 100 million years. Am J Sci 283:641–683
Berner RA, Rye DM (1992) Calculation of the Phanerozoic strontium isotope record of the oceans from a carbon cycle model. Am J Sci 292:136–148
Bolin B, Björkström A, Holmen K, Moore B (1983) The simultaneous use of tracers for ocean circulation studies. Tellus 35B:206–236
Brass GW (1976) The variation of the marine 87Sr/86Sr ratio during Phanerozoic time: interpretation using a flux model. Geochim Cosmochim Acta 40: 721–730
Broecker WS (1982) Ocean chemistry during glacial time. Geochim Cosmochim Acta 46:1689–1705
Broecker WS (1992) The Glacial World According to Wally. Lamont-Doherty Geological Observatory of Columbia University, Palisades NY
Broecker WS, Peng TH (1986) Carbon cycle, 1985: Glacial to interglacial changes in the operation of the global carbon cycle. Radiocarbon 28:309–327
Broecker WS, Peng TH (1989) The cause of the glacial to interglacial atmospheric CO2 change: a polar alkalinity hypothesis. Global Biogeochemical Cycles 3:215–239
Broecker WS, Takahashi T (1978) The relationship between lysocline depth and in situ carbonate ion concentration. Deep-Sea Res 25:65–95
Burke WH, Denison RE, Hetherington EA, Koepnick RB, Nelson HF, Otto JB (1980) Variation of seawater 87Sr/86Sr throughout Phanerozoic time. Geology 10:516–519
Dia AN, Cohen AS, O’Nions RK, Shackleton NJ (1992) Seawater Sr isotope variation over the past 300 kyr and influence of global climate cycles. Nature 356:786–788
Edmond JM (1992) Himalayan tectonics, weathering processes and the strontium isotope record in marine limestones. Science 258:1594–1597
Farrell JW and Prell WL (1989) Climatic change and CaCO3 preservation: an 800,000 year bathymetrie reconstruction from the central equatorial Pacific Ocean. Paleoceanography 4: 447–466
François LM, Walker JCG (1992) Modelling the Phanerozoic carbon cycle and climate: constraints from the 87Sr/86Sr isotopic ratio of seawater. Am J Sci 292:81–135
François LM, Walker JCG, Opdyke BN (1993) The history of global weathering and the chemical evolution of the ocean-atmosphere system. In: Takahashi E, Jeanloz R, Rubie DC (eds) Chemical Evolution of the Earth and Planets, American Geophysical Union, Washington DC (Geophysical Monograph Series, vol 74, IUGG Series, vol 14)
Froelich PN, Blanc V, Mortlock RA, Chillrud SL, Dunstan W, Udomkit A, Peng TH (1992) River fluxes of dissolved silica to the ocean were higher during glacials: Ge/Si in diatoms, rivers and oceans. Paleoceanography 7:739–767
Holland HD (1984) The Chemical Evolution of the Atmosphere and Oceans. Princeton University Press, Princeton NJ
Keir RS (1980) The dissolution kinetics of biogenic calcium carbonates in seawater. Geochim Cosmochim Acta 44:241–252
Keir RS (1988) On the Late Pleistocene ocean geochemistry and circulation. Paleoceanography 3:413–445
Keir RS, Berger WH (1983) Atmospheric CO2 content in the last 120,000 years: the phosphate-extraction model. J Geophys Res 88:6027–6038
Kinsey D, Hopley D (1991) The significance of coral-reef s as global carbon sinks — Response to greenhouse. Palaeogeog Palaeocl Palaeoecol 89:1–15
Knox F, McElroy MB (1984) Changes in atmospheric CO2: influence of the marine biota at high latitude, J Geophys Res 89:4629–4637
Koepnick RB, Denison RE, Dahl DA (1988) The Cenozoic seawater 87Sr86Sr curve: Data review and implications for correlation of marine strata. Paleoceanography 3:743–756
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 327:477–482
Lasaga AC, Berner RA, Garrels RM (1985) An improved geochemical model of atmospheric CO2 fluctuations over the past 100 million years. In: Sundquist ET, Broecker WS (eds) The Carbon Cycle and Atmospheric CO2: Natural Variations Archean to Present. American Geophysical Union, Washington DC (Geophysical Monograph Series vol 32, p 397–411)
Maier-Reimer E, Mikolajewicz U (1991) The Hamburg Large Scale Geostrophic Ocean General Circulation Model (Cycle 1). Technical Report No 2. Deutsches Klimarechenzentrum, Hamburg
Martin JH (1990) Glacial-interglacial CO2 change: the iron hypothesis. Paleoceanography 5:1–13
Meybeck M (1987) Global chemical weathering of surficial rocks estimated from river dissolved loads. Am J Sci 287:401–428
Opdyke BN, Walker JCG (1992a) Return of the coral-reef hypothesis: Basin to shelf partitioning of CaCO3 and its effect on atmospheric CO2. Geology 20:733–736
Opdyke BN, Walker JCG (1992b) Glacial to interglacial, basin to shelf partitioning of CaCO3 and its effect on atmospheric CO2. In: Sarnthein M, Thiede J, Zahn R (eds) Fourth International Conference on Paleoceanography ICP IV, Short- and Long-Term Global Change: Records and Modelling 21–25 Sept 1992. GEOMAR, Kiel (GEOMAR REPORT 15)
Peterman ZE, Hedge CE, Tourtelot HA (1970) Isotopic composition of strontium in seawater throughout Phanerozoic time. Geochim Cosmochim Acta 34:105–120
Raymo ME (1991) Geochemical evidence supporting T.C. Chamberlin’s theory of glaciation. Geology 19:344–347
Raymo ME, Ruddiman WF, Froelich PN (1988) Influence of late Cenozoic mountain building on ocean geochemical cycles. Geology 16:649–653
Sarmiento JL, Toggweiler JR (1984) A new model for the role of the oceans in determining atmospheric pCO2. Nature 308:621–624
Veizer J, Compston W (1974) 87Sr/86Sr composition of seawater during the Phanerozoic. Geochim Cosmochim Acta 38:1461–1484
Wadleigh MA, Veizer J, Brooks W (1985) Strontium and its isotopes in Canadian rivers: fluxes and global implications. Geochim Cosmochim Acta 49:1727–1736
Walker JCG (1977) Evolution of the atmosphere. MacMillan, New York
Walker JCG, Opdyke BN (submitted) The influence of variable rates of shelf carbonate deposition on atmospheric carbon dioxide and pelagic sediments. Paleoceanography
Walker JCG, Hays PB, Kasting JF (1981) A negative feedback mechanism for the long-term stabilization of Earth’s surface temperature. J Geophys Res 86:9776–9782
Author information
Authors and Affiliations
Editor information
Editors and Affiliations
Rights and permissions
Copyright information
© 1994 Springer-Verlag Berlin Heidelberg
About this paper
Cite this paper
Munhoven, G., François, L.M. (1994). Glacial-Interglacial Changes in Continental Weathering: Possible Implications for Atmospheric CO2 . In: Zahn, R., Pedersen, T.F., Kaminski, M.A., 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. https://doi.org/10.1007/978-3-642-78737-9_3
Download citation
DOI: https://doi.org/10.1007/978-3-642-78737-9_3
Publisher Name: Springer, Berlin, Heidelberg
Print ISBN: 978-3-642-78739-3
Online ISBN: 978-3-642-78737-9
eBook Packages: Springer Book Archive