Skip to main content

Carbon Sequestration in Marine Systems

  • Conference paper
Carbon Sequestration in the Biosphere

Part of the book series: NATO ASI Series ((ASII,volume 33))

Abstract

Biological processes in the oceans that affect the partitioning of CO2 between the atmosphere and oceans under different conditions of global climate and sea level are briefly described. For the oceans, the present net uptake due to organic productivity is small and any alteration of this balanced condition is likely to be very gradual. By contrast, the coastal zone, which tends to be a net source of CO2 to the atmosphere due to the oxidation of organic matter transported from the land, exhibits several potential mechanisms for the sequestration of anthropogenic CO2 involving ecological and geochemical processes. However, this region is being significantly altered by humans as a result of modifications to catchment systems and the land-ocean interface and, indirectly, to climate and sea level. A qualitative analysis suggests that the capacity of the coastal zone to store organic carbon will become weaker as ecosystems are disturbed and as organic material is mobilised and oxidised within catchment sytems and coastal environments. In both the open ocean and shelf seas changes to the carbonate system could also affect levels of atmospheric CO2 but the rate at which these might occur and their net effect are uncertain.

This is a preview of subscription content, log in via an institution to check access.

Access this chapter

Chapter
USD 29.95
Price excludes VAT (USA)
  • Available as PDF
  • Read on any device
  • Instant download
  • Own it forever
eBook
USD 84.99
Price excludes VAT (USA)
  • Available as EPUB and PDF
  • Read on any device
  • Instant download
  • Own it forever
Softcover Book
USD 109.99
Price excludes VAT (USA)
  • Compact, lightweight edition
  • Dispatched in 3 to 5 business days
  • Free shipping worldwide - see info

Tax calculation will be finalised at checkout

Purchases are for personal use only

Institutional subscriptions

Preview

Unable to display preview. Download preview PDF.

Unable to display preview. Download preview PDF.

References

  • Archer D; Maier-Reimer E (1994) Effect of deep-sea sedimentary calcite preservation on atmospheric CO2 concentration. Nature 367:260–263.

    Article  CAS  Google Scholar 

  • Atkinson MJ; Smith SV (1983) C:N:P ratios of benthic marine plants. Iimnol Oceanogr 28:568–574.

    Article  CAS  Google Scholar 

  • Bakun A (1990) Global climate change and intensification of coastal upwelling. Science 247:198–201.

    Article  CAS  Google Scholar 

  • Bauer JE; Williams PM; Druffel ERM (1992) 14C activity of dissolved organic carbon fractions in the north-central Pacific and Sargasso Sea. Nature 357:667–670.

    Article  CAS  Google Scholar 

  • Berner RA (1989) Biogeochemical cycles of carbon and sulfur and their effect on tmospheric oxygen over Phanerozoic time. Palaeogeogr Palaeoclimatol Palaeoecol 75:97–122.

    Article  Google Scholar 

  • Billen G; Lancelot C; Meybeck M (1991) N, P and Si retention along the aquatic continuum from land to ocean. In Mantoura RFC, Martin J-M, Wollast R (eds) Ocean margin processes in global change. John Wiley & Sons Chichester, pp 19–44.

    Google Scholar 

  • Boyle EA (1990) Quaternary deepwater paleoceanography. Science 249:863–870.

    Article  CAS  Google Scholar 

  • Broecker WS (1991) The great ocean conveyor. Oceanography 4: 70–89.

    Google Scholar 

  • Broecker WS; Peng T-H (1993) What caused the glacial to interglacial CO2 change? In Heimann M (ed) The global carbon cycle. NATO ASI Ser I Vol. 15, Springer-Verlag Berlin Heidelberg, pp 95–115.

    Google Scholar 

  • Calvert SE; Karlin RE; Toolin LJ; Donahue DJ; Southon JR; Vogel JS (1991) Low organic carbon accumulation rates in Black Sea sediments. Nature 350:692–695.

    Article  CAS  Google Scholar 

  • Canfield DE (1993) Organic matter oxidation in marine sediments. In Wollast R, Mackenzie FT, Chou L (eds) Interactions of C, N, P and S biogeochemical cycles and global change. NATO ASI Ser I Vol 4 Springer-Verlag Berlin Heidelberg, pp 333–363.

    Chapter  Google Scholar 

  • Carlton JT; Geller JB (1993) Ecological roulette: The global transport of nonindigenous marine organisms. Science 261:78–82.

    Article  Google Scholar 

  • Christensen JP (1994) Carbon export from continental shelves, denitrification and atmospheric carbon dioxide. Contin Shelf Res 14:547–576.

    Article  Google Scholar 

  • Depetris PJ; Kempe S (1990) The impact of the El Ni_o 1982 event on the Paran_ River, its discharge and carbon transport. Palaeogeogr Palaeoclimatol Palaeoecol 89:239–244.

    Article  Google Scholar 

  • Downing JP; Meybeck M; Orr JC; Twilley RR; Scharpenseel H-W (1993) Land and water interface zones. Water Air & Soil Poll 70:123–137.

    Article  CAS  Google Scholar 

  • Falkowski PG; Biscaye PE; Sancetta C (1994) The lateral flux of biogenic particles from the eastern North Atlantic continental margin to the North Atlantic Ocean. Deep-Sea Res II 41:583–601.

    Article  CAS  Google Scholar 

  • Flannery BP; Kheshgi HS; Hoffert MI; Lapenis AG (1993) Assessing the effectiveness of marine CO2 disposal. Energy Convers Mgmt 34:983–989.

    Article  CAS  Google Scholar 

  • Frankignoulle M; Canon C; Gattuso J-P (1994) Marine calcification as a source of carbon dioxide: Positive feedback of increasing atmospheric CO2. Limnol Oceanogr 39:458–462.

    Article  CAS  Google Scholar 

  • Gattuso J-P; Pichin M; Delesalle B; Frankignoulle M (1993) Community metabolism and air-sea CO2 fluxes in a coral reef ecosystem (Moorea, French Polynesia). Mar Ecol Prog Ser 96: 259–267.

    Article  Google Scholar 

  • Glasby GP (1988) Entropy, pollution and environmental degradation. Ambio 17:330–335.

    Google Scholar 

  • Gorsline DS (1992) The geological setting of Santa Monica and San Pedro Basins, California continental borderland. Prog Oceanogr 30:1–36.

    Article  Google Scholar 

  • Henrichs SM; Reeburgh WS (1987) Anaerobic mineralization of marine sediment organic matter: Rates and the role of anaerobic processes in the oceanic carbon economy. Geomicrob J 5:191–237.

    Article  CAS  Google Scholar 

  • Holligan PM; Fernández E; Aiken J; Balch WM; Boyd P; Burkill PH; Finch M; Groom SB; Malin G; Muller K; Purdie DA; Robinson C; Trees CC; Turner SM; van der Wal P (1993) A biogeochemical study of the coccolithophore, Emilicmia huxleyi, in the North Atlantic. Global Biogeochem Cycles 7:879–900.

    Article  CAS  Google Scholar 

  • Howard WR; Prell WL (1994) Late quaternary CaCO3 production and preservation in the Southern Ocean: implications for oceanic and atmospheric carbon cycling. Paleoceanography 9:453–482.

    Article  Google Scholar 

  • International Geosphere-Biosphere Programme (1993) Land-Ocean Interactions in the Coastal Zone (LOICZ). Science plan. IGBP Report No. 255, 50pp.

    Google Scholar 

  • Kempe S (1984) Sinks of the anthropogenically enhanced carbon cycle in surface fresh waters. J Geophys Res 89:4657–4676.

    Article  CAS  Google Scholar 

  • Kempe S (1988) Estuaries — their natural and anthropogenic changes. In Rosswall T, Woodmansee RG, Risser PG (eds) Scales and global change. SCOPE Report 35, John Wiley & Sons Chichester, pp 251–285.

    Google Scholar 

  • Kempe S; Pegler K (1991) Sinks and sources of CO2 in coastal seas: the North Sea. Tellus 43B:224–235.

    CAS  Google Scholar 

  • Kheshgi HS; Flannery BP; Hoffert MI (1991) Marine biota effects on the compositional structure of the world oceans. J Geophys Res 96:4957–4969.

    Article  Google Scholar 

  • Kurz KD; Maier-Reimer E (1993) Iron fertilization of the Austral Ocean-The Hamburg model assessment. Global Biogeochem Cycles 7:229–244.

    Article  CAS  Google Scholar 

  • Leuenberger M; Siegenthaler U; Langway CC (1992) Carbon isotopic composition of atmospheric CO2 during the last ice age from an Antarctic ice core. Nature 357:488–490.

    Article  CAS  Google Scholar 

  • Longhurst AR (1991) The role of the marine biosphere in the global carbon cycle. Limnol Oceanogr 36:1507–1526.

    Article  CAS  Google Scholar 

  • Mayer LM (1994a) Surface area control of organic carbon accumulation in continental shelf sediments. Geochim Cosmochim Acta 58:1271–1284.

    Article  CAS  Google Scholar 

  • Mayer LM (1994b) Relationship between mineral surfaces and organic carbon concentrations in soils and sediments. Chem Geology 114:347–363.

    Article  CAS  Google Scholar 

  • McConnaughey TA (1994) Calcification, photosynthesis, and the global carbon cycle. Bull Inst oceanogr Monaco No. Spec 13:137–161.

    Google Scholar 

  • Meybeck M (1993) C, N, P, and S in rivers: from sources to global inputs. In Wollast R, Mackenzie FT, Chou L (eds) Interactions of C, N, P and S biogeochemical cycles and global change. NATO ASI Ser I Vol. 4 Springer-Verlag Berlin Heidelberg, pp 163–193.

    Chapter  Google Scholar 

  • Milliman JD (1993) Production and accumulation of calcium carbonate in the ocean: budget of a nonsteady state. Global Biogeochem Cycles 7:927–957.

    Article  CAS  Google Scholar 

  • Milliman JD; Syvitski PM (1992) Geomorphic/tectonic control of sediment discharge to the ocean: The importance of small mountainous rivers. J Geol 100:525–544.

    Article  Google Scholar 

  • Morris JT; Kjerfve B; Dean JM (1990) Dependence of estuarine productivity on anomalies in mean sea-level. Limnol Oceanogr 35:926–930.

    Article  Google Scholar 

  • Opdyke BN; Walker JCG (1992) Return of the coral reef hypothesis: Basin to shelf partitioning of CaCO3 and its effect on atmospheric CO2. Geology 20:733–736.

    Article  CAS  Google Scholar 

  • Orr JC; Sarmiento JL (1992) Potential of marine macroalgae as a sink for CO2: constraints from a 3-D General circulation model of the global ocean. Water Air & Soil Poll 64:405–421.

    Article  CAS  Google Scholar 

  • Paillard D; Ghil M; Le Treut H (1993) Dissolved organic matter and the glacial-interglacial pCO2 problem. Global Biogeochem Cycles 7:901–914.

    Article  CAS  Google Scholar 

  • Peltier WR; Tushingham AM (1989) Global sea level rise and the greenhouse effect: Might they be connected? Science 244:806–810.

    Article  CAS  Google Scholar 

  • Peterson BJ; Melillo JM (1985) The potential storage of carbon caused by eutrophication of the biosphere. Tellus 37B: 117–127.

    Article  CAS  Google Scholar 

  • Raven JA (1994) Carbon fixation and carbon availability in marine phytoplankton. Photosynth Res 39:259–273.

    Article  CAS  Google Scholar 

  • Reimers CE; Jahnke RA; McCorkle DC (1992) Carbon fluxes and burial rates over the continental slope and rise off central California with implications for the global carbon cycle. Global Biogeochem Cycles 6:199–224.

    Article  CAS  Google Scholar 

  • Ritschard RL (1992) Marine algae as a CO2 sink. Water Air & Soil Poll 64:289–303.

    Article  CAS  Google Scholar 

  • Sabine CL; Mackenzie FT (1990) Oceanic sinks for anthropogenic CO2. Int J Energy Envir Econ 21:119–127.

    Google Scholar 

  • Sahaglan DL; Schwartz FW; Jacobs DK (1994) Direct anthropogenic contributions to sea level rise in the twentieth century. Nature 367:54–57.

    Article  Google Scholar 

  • Sarmiento JL; Bender M (1994) Carbon biogeochemistry and climate change. Photosynth Res 39:209–234.

    Article  CAS  Google Scholar 

  • Sarmiento JL; Siegenthaler U (1992) New production and the global carbon cycle. In Falkowski PG, Woodhead AD (eds) Primary productivity and biogeochemical cycles in the sea. Plenum Press New York, pp. 317–332.

    Google Scholar 

  • Shaffer G (1993) Effects of the marine carbon biota on global carbon cycling. In Heimann M (ed) The global carbon cycle. NATO ASI Ser I Vol 15, Springer-Verlag Berlin Heidelberg, pp 431–455.

    Google Scholar 

  • Siegenthaler U; Sarmiento JL (1993) Atmospheric carbon dioxide and the ocean. Nature 365:119–125.

    Article  CAS  Google Scholar 

  • Sirocko F; Ittekot V (1992) Organic carbon accumulation rates in the Holocene and glacial Arabian Sea: implications for O2-consumption in the deep-sea and atmospheric CO2 variations. Clim Dyn 7:167–172.

    Article  Google Scholar 

  • Smetacek V; Bathmann U; Nöthig E-M; Schareg R (1991) Coastal eutrophication: causes and consequences. In Mantoura RFC, Martin J-M, Wollast R (eds) Ocean margin processes in global change. John Wiley & Sons Chichester, pp. 251–279.

    Google Scholar 

  • Smith RC; Prezelin BB; Baker KS; Bidigare RR; Boucher NP; Coley T; Karentz D; Maclntyre S; Matlick HA; Menzies D; Ondrusek M; Wan Z; Waters KJ (1992) Ozone depletion: Ultraviolet radiation and phytoplankton biology in Antarctic waters. Science 255:952–959.

    Article  CAS  Google Scholar 

  • Smith SV (1981) Marine macrophytes as a global carbon sink. Science 211:838–840.

    Article  CAS  Google Scholar 

  • Smith SV; Buddemeier RW (1992) Global change and coral reef systems. Annu Rev Ecol Syst 23:89–118.

    Article  Google Scholar 

  • Smith SV; Hollibaugh JT (1993) Coastal metabolism and the oceanic carbon balance. Rev Geophys 31(1):75–89.

    Article  Google Scholar 

  • Sundquist ET (1993) The global carbon dioxide budget. Science 259:934–941.

    CAS  Google Scholar 

  • Thingstad TF (1993) Microbial processes and the biological carbon pump. In Evans GT, Fasham MJR (eds) Towards a model of ocean biogeochemical processes. Springer-Verlag Berlin Heidelberg, pp 193–208.

    Chapter  Google Scholar 

  • Twilley RR; Chen RH; Hargis T (1992) Carbon sinks in mangroves and their implications to carbon budget of tropical coastal ecosystems. Water Air & Soil Poll 64:265–288.

    Article  CAS  Google Scholar 

  • Walsh JJ (1991) Importance of continental margins in the marine biogeochemical cycling of carbon and nitrogen. Nature 350:53–55.

    Article  CAS  Google Scholar 

  • Watson AJ; Law CS; Van Scoy KA; Millero FJ; Yao W; Friederich GE; Liddicoat MI; Wanninkhof RH; Barber RT; Coale KH (1994) Minimal effect of iron fertilization on sea-surface carbon dioxide concentrations. Nature 371:143–145.

    Article  CAS  Google Scholar 

  • Wong CS; Matear R (1993) The storage of anthropogenic CO2 in the ocean. Energy Convers Mgmt 34:873–880.

    Article  CAS  Google Scholar 

  • Woods J; Barkmann W (1993) The plankton multiplier — positive feedback in the greenhouse. J Plankton Res 15:1053–1074.

    Article  Google Scholar 

Download references

Author information

Authors and Affiliations

Authors

Editor information

Editors and Affiliations

Rights and permissions

Reprints and permissions

Copyright information

© 1995 Springer-Verlag Berlin Heidelberg

About this paper

Cite this paper

Holligan, P.M. (1995). Carbon Sequestration in Marine Systems. In: Beran, M.A. (eds) Carbon Sequestration in the Biosphere. NATO ASI Series, vol 33. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-79943-3_4

Download citation

  • DOI: https://doi.org/10.1007/978-3-642-79943-3_4

  • Publisher Name: Springer, Berlin, Heidelberg

  • Print ISBN: 978-3-642-79945-7

  • Online ISBN: 978-3-642-79943-3

  • eBook Packages: Springer Book Archive

Publish with us

Policies and ethics