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Sources of Carbon to Deep-Sea Corals

Published online by Cambridge University Press:  18 July 2016

Sheila Griffin  and
Ellen R M Druffel
Sheila Griffin
Affiliation:
Department of Chemistry Woods Hole Oceanographic Institution Woods Hole, Massachusetts 02543
Ellen R M Druffel
Affiliation:
Department of Chemistry Woods Hole Oceanographic Institution Woods Hole, Massachusetts 02543
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Abstract

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Radiocarbon measurements in deep-sea corals from the Little Bahama Bank were used to determine the source of carbon to the skeletal matrices. Specimens of Lophelia, Gerardia, Paragorgia johnsoni and Corallium noibe were sectioned according to visible growth rings and/or stem diameter. We determined that the source of carbon to the corals accreting organic matter was primarily from surface-derived sources. Those corals that accrete a calcerous skeleton were found to obtain their carbon solely from dissolved inorganic carbon (DIC) in sea water from the depth at which the corals grew. These results, in conjunction with growth-rate studies using short-lived radioisotopes, support the use of deep-sea corals to reconstruct time histories of transient and non-transient tracers at depth in the oceans.

Type
II. Carbon Cycle in the Environment
Information
Radiocarbon , Volume 31 , Issue 3: June 20-25, 1988 Dubrovnik, Yugoslavia , 1989 , pp. 533 - 543
Copyright
Copyright © The American Journal of Science 

References

Broecker, W S, Gerard, R, Ewing, M and Heezen, B C, 1960, Natural radiocarbon in the Atlantic Ocean: Jour Research, v 65, p 2903–2931.Google Scholar
Druffel, E R M, 1982, Banded corals: changes in oceanic carbon-14 during the Little Ice Age: Science, v 218, p 13–19.Google Scholar
Druffel, E R M and King, L (ms), Corals as recorders of chemical properties in the deep sea: Ms in preparation.Google Scholar
Druffel, E R M and Linick, T W, 1978, Radiocarbon in annual coral rings from Florida: Geophys Research Letters, v 5, p 913–916.Google Scholar
Duncan, P M, 1877, On the rapidity of growth and variability of some Madreporaria on an Atlantic cable with remarks upon the rate of accumulation of foraminiferal deposits: Ann Mag Nat Hist, ser 4, v 20, p 361–365.Google Scholar
Emerson, S C, Stump, C, Grootes, P, Stuiver, M, Farwell, G and Schmidt, F, 1987, Estimates of degradable organic carbon in deep-sea surface sediments from 14C concentrations: Nature, v 329, p 51–53.Google Scholar
Goreau, T F and Goreau, N I, 1960, The physiology of skeleton formation in corals, IV, On isotopic equilibrium exchanges of calcium between corallium and environment in living and deep reef-building corals: Biol Bull Marine Biol Lab, Woods Hole, v 119, p 416–427.CrossRefGoogle Scholar
Griffin, S and Druffel, E R M, 1985, Woods Hole Oceanographic Institution Radiocarbon Laboratory: Sample treatment and gas preparation: Radiocarbon, v 27, no. 1, p 43–51.CrossRefGoogle Scholar
Grigg, R W, 1974, Distribution and abundance of precious corals in Hawaii, in Cameron, A M, ed, Internatl coral reef symposium, 2nd, Proc: Brisbane, Australia, v 2, p 235–240.Google Scholar
Kroopnik, P M, 1985, The distribution of 13C of ΣCO2 in the world oceans: Deep-sea Research, v 32, no. 1, p 57–84.CrossRefGoogle Scholar
Mikkelsen, N, Erlenkeuser, E, Killingley, J S and Berger, W H, 1982, Norwegian corals: radiocarbon and stable isotopes in Lophelia pertusa : Boreas, v 11, p 163–171.CrossRefGoogle Scholar
Mullins, H T, Newton, C R, Heath, K and Vanburen, H M, 1981, Modern deep-water coral mounds north of Little Bahama Bank: Criteria for recognition of deep-water biotherms in the rock record: Jour Sed Petrol, v 51, no. 3, p 999–1013.Google Scholar
Neumann, A C, Kofold, J W and Keller, G H, 1977, Lithoherms in the Straits of Florida: Geology, v 5, p 4–10.Google Scholar
Newton, C R, Mullins, H T, Garduski, A F, Hine, A C and Dix, G R, 1987, Coral mounds on the West Florida Slope: Unanswered questions regarding the development of deep-water banks: Soc Economic Paleontologists & Mineralogists, Research Repts, p 359–367.Google Scholar
Pourtales, L F, 1868, Contributions to the Gulf Stream at great depths: Bull Mus Comp Zool, Harvard, v 1, p 103–142.Google Scholar
Pratje, O, 1924, Korallenbänke in tiefen und kühlen Wässer: Centralbl f Min Geol, p 410–415.Google Scholar
Schuhmacher, H and Zibrowius, H, 1985, What is hermatypic? A redefinition of ecological groups in corals and other organisms: Coral Reefs, v 4, p 1–9.Google Scholar
Sikes, E (ms), 1984, Bioerosion of deep carbonates by macro-endoliths: Masters's thesis, Univ North Carolina, 120 p.Google Scholar
Squires, D F, 1964, Fossil coral thickets in Wairarapa, New Zealand: Jour Paleontol, v 38, no. 5, p 904–915.Google Scholar
Stuiver, M and Ostlund, H G, 1980, GEOSECS Atlantic radiocarbon: Radiocarbon, v 22, no. 1, p 1–24.Google Scholar
Stuiver, M and Polach, H A, 1977, Discussion: Reporting of 14C data: Radiocarbon, v 19, no. 3, p 355–363.CrossRefGoogle Scholar
Teichert, C, 1958, Cold and deep-water coral banks: Bull Am Assoc Petrol Geol, v 42, no. 5, p 1064–1082.Google Scholar
Vaughan, T W and Wells, J G, 1943, Revision of the suborders, families and genera of the Schleractinia: Geol Soc America Spec Paper, v 144, p 1–363.Google Scholar
Wells, J G, 1956, Scleractinia. Treatise on invertebrate paleontology, Part F, Coelenterata, in Moore, R C, ed, Geol Soc America, Univ Kansas, p 328–444.Google Scholar
Williams, P M and Druffel, E R M, 1987, Radiocarbon in dissolved organic matter in the Central North Pacific Ocean: Nature, v 330, no. 6145, p 246–248.Google Scholar