Deep-sea carbonates: Reading the carbon-isotope signal
Tóm tắt
Từ khóa
Tài liệu tham khảo
Adam, C. G., Benson, R. H., Kidd, R. B., Ryan, W. B. F. &Wright, R. C. (1977): The Messinian salinity crisis and evidence of late Miocene eustatic changes in the world ocean. - Nature,269, 383–386.
Arthur, M. A. (1982): The carbon cycle — controls on atmospheric CO2 and climate in the geologic past. - In:Berger, W. H. &:Crowell, D. C. (eds.): Climate in Earth History. - National Academy Press, Washington, D.C., 55–67.
-,Anderson, T. F.,Kaplan, I. R.,Veizer, J. &Land, L. S. (1983): Stable isotopes in sedimentary geology. - SEPM Short Coure No. 10, Dallas, 1983.
Bainbridge, A. E. (ed.) (1981): GEOSECS Atlantic Expedition. Volume 1 Hydrographic Data. - National Science Foundation, Washington, D.C., 121 pp.
Barron, E. J &Washington, W. M. (1985): Warm Cretaceous climates: high atmospheric CO2 as a plausible mechanism. -In:Sundquist, E. T. &Broecker, W. S. (eds.), The Carbon Cycle and Atmospheric CO2: Natural Variations Archaen to Present. - Amer. Geophys. Union, Geophys. Monograph32, 546–553.
Barron, J. A. &Keller G. (1982): Widespread Miocene deep sea hiatuses: coincidence with periods of global cooling. - Geology,10: 577–581.
-,Keller, G. &Dunn, D. A. (1985): A multiple microfossil biochronology for the Miocene. - In:Kennett, J. P. (ed.), The Miocene Ocean: Paleoceanography and Biogeography. - Mem. Geol. Soc. Am.,163, 21–36.
Bender, M. L. &Graham, D. W. (1981): On late Miocene abyssal hydrography. - Micropaleontology,6, 451–464.
Bender, L. &Keigwin, L. D., Jr. (1979): Speculations about the upper Miocene change in abyssal Pacific dissolved bicarbonate δ13C. - Earth Planet. Sci. Lett.,45, 383–393.
— (1977): Carbon dioxide excursions and the deep sea record: aspects of the problem. - In:N. R. Andersen &A. Malahoff (eds.), The Fate of Fossil Fuel CO2 in the Oceans, Plenum Press, New York, 505–542.
- &Keir, R. S. (1984): Glacial-Holocene changes in atmospheric CO2 and the deep sea record. - In: J. E.Hansen & T.Takahashi (eds.), Climate Processes and Climate Sensitivity, Amer. Geophys. Union Geophys. Monograph29, 337–351.
- &Vincent, E. (1981): Chemostratigraphy and biostratigraphic correlation: excercises in systemic stratigraphy. Proc. 26th Internat. Geol. Congress, Geology of Oceans Symposium (Paris, 1980) - Spec. Publ. Oceanologica Acta, 115–127.
—,Killingley, J. S. &Vincent, E. (1978): Stable isotopes in deep-sea carbonates: Box Core ERDC-92, west equatorial Pacific. - Oceanologica Acta, 1, 203–216.
-,Be, A. W. H. &Vincent, E. (eds.) (1981): Oxygen and carbon isotopes in foraminifera. - Palaeogeogr., Palaeoclimatol., Palaeoecol.,33, 1–277 (special issue).
—,Killingley, J. S., Metzler, C. V. &Vincent, E. (1985): Two-step deglaciation:14C-dated high resolution δ18O records from the tropical Atlantic Ocean. - Quaternary Research,23, 258–271.
Berggren, W. A. &Haq, B. U. (1976): The Andalusian Stage (Late Miocene): biostratigraphy, biochronology and paleoecology. - Palaeogeogr., Palaeoclimatol., Palaeoecol.,20, 67–129.
-,Kent, D. V. &Van Couvering, J. A. (in press): Neogene geochronology and chronostratigraphy. In:Snelling, N. J., ed., Geochronology and the geological record. - Geological Society of London Special Paper.
Berner, R. A. &Raiswell, R. (1983): Burial of organic carbon and pyrite sulfur m sediments over Phanerozoic time: a new theory. - Geochim. Cosmochim. Acta,47, 855–862.
—,Lasaga, A. C. &Garrels, R. M. (1983): The carbonate-silicate geochemical cycle and its effect on atmospheric carbon dioxide over the past 100 million years. - Amer. Jour. Sci.,283, 641–683.
Berner, W., Oeschger, H. &Stauffer, B. (1980): Information on the CO2 cycle from ice core studies: Radiocarbon,22, 227–235.
Boersma, A. &Shackleton, N. (1977): Tertiary oxygen and carbon isotope stratigraphy, Site 357 (Mid-latitude South Atlantic). - Init. Repts. DSDP,39, 911–924.
Boyle, E. A. &Keigwin, L. D. (1982): Deep circulation of the North Atlantic over the last 200,000 years: geochemical evidence. - Science,218, 784–787.
Bramlette, M. N. (1946): Monterey Formation of California and orgin of its siliceous rocks. U.S. Geol. Surv. Prof. Pap.212, 1–57.
Broecker, W. S. (1973): Factors controlling CO2 content in the oceans and atmosphere. - In: G. M.Woodwell & E. V.Pecan (eds.), Carbon and the Biosphere, AEC Symposium,30, 32–50.
- (1974): Chemical oceanography. - Hartcourt Brace Jovanovich, New York.
— &Peng, T. H. (1982): Tracers in the Sea. - Eldigio Press, Palisades, New York, 690 pp.
—,Spencer, D. W. &Craig, H. (eds.) (1982): GEO-SECS Pacific Expedition, Volume 3, Hydrographic Data. - National Science Foundation, Washington, D.C., 137 pp.
—,Peteet, D. &Rind, D. (1985): Does the ocean-atmosphere system have more than one stable mode of operation? - Nature,315, 21–26.
Calvert, S. E. (1966): Origin of diatom-rich, varved sediments from the Gulf of California. - Jour. Geol.,74, (5), Part 1, 546–565.
Corliss, B. H. (1985): Microhabitats of benthic foraminifera within deep-sea sediment. - Nature,314, 435–438.
Curry, W. B. &Lohmann, G. P. (1982): Carbon isotopic changes in benthic foraminifera from the western South Atlantic: reconstruction of glacial abyssal circulation patterns. - Quat. Res.,18, 218–235.
—, (1983): Reduced advection into Atlantic Ocean deep eastern basins during last glacial maximum.- Nature,306, 577–580.
Delmas, R. J., Ascencio, J. M. &Legrand, M. (1980): Polar ice evidence that atmospheric CO2 20,000 years BP was 50% of present. - Nature,284, 155–157.
Duplessy, J. C., Chenouard, L. &Vila, F. (1975): Weyl's theory of glaciation supported by isotopic study of Norwegian Cove Kll. - Science,188, 1208–1209.
—,Moyes, J. &Pujol, C. (1980): Deep water formation in the North Atlantic during the last ice age. - Nature,286, 479–482.
Fischer, A. G. &Arthur, M. A. (1977): Secular variations in the pelagic realm. - Soc. Econ. Paleontol. Mineral. Spec. Publ.25, 19–50.
Ganssen, G. (1983): Dokumentation von küstennahem Auftrieb anhand stabiler Isotope in rezenten Foraminiferen vor Nordwest-Afrika. - Meteor. Forsch.-Ergebnisse, C.37, 1–46.
Ganssen, G. &Sarnthein, M. (1983): Stable-isotope composition of foraminifers: the surface and bottom water record of coastal upwelling. - In:Suess, E. &Thiede, J. (eds.), Coastal Upwelling, Part A, 99–121, Plenum Press, New York.
Grossman, E. L. (1984): Carbon isotopic fractionation in live benthic foraminifera — comparison with inorganic precipitate studies. - Geochim. Cosmochim. Acta,48, 1505–1512.
Haq, B. R., Worsley, T. R., Burckle, L. H., Douglas, R. G., Keigwin, L. D., Jr.,Opdyke, N. D., Savins, S. M., Sommer, M. A. (1980): Late Miocene marine carbon-isotope shift and synchroneity of some phytoplanktonic biostratigraphic events. - Geology,8, 427–431.
Holser, W. T. (1984): Gradual and abrupt shifts in ocean chemistry during Phanerozoic time. - In:Holland, H. &Trendall (eds.), Patterns of Change in Earth Evolution, 123–143, Berlin (Dahlem Konferenzen, Springer-Verlag).
Jansen, E. &Erlenkeuser, H. (1985): Ocean circulation in the Norwegian Sea during the last deglaciation; isotopic evidence. - Palaeogeog., Palaeoclimatol., Palaeoecol.,49, 189–206.
Keigwin, L. D., Jr. (1979): Late Cenozoic stable isotope stratigraphy and paleoceanography of DSDP Sites from the east equatorial and north central Pacific Ocean. - Earth Planet. Sci. Letts.45, 361–382.
— &Shackleton, N. J. (1980): Uppermost Miocene carbon isotope stratigraphy of a piston core in the equatorial Pacific. - Nature,284, 613–614.
Killingley, J. S. (1983): Effects of diagenetic recrystallization on18O/16O values of deep-sea sediments.- Nature,301, 594–597.
Kroopnick, P. M. (1985): The distribution of13C of ∑CO2 in the world oceans. - Deep-Sea Res.,32 (1), 57–84.
—,Margolis, S. V. &Wong, C. S. (1977): δ13C variations in marine carbonate sediments as indicators of the CO2 balance between the atmosphere and oceans. - In:Andersen, N. R. &Malahoff, A. (eds.), The Fate of Fossil Fuel CO2 in the Oceans, 295–321, Plenum Press, New York.
Loutit, T. S. &Keigwin, L. D., Jr (1982): Stable isotopic evidence for latest Miocene sea level fall in the Mediterranean region. - Nature,300, 163–166.
—,Kennett, J. P. &Savin, S. M. (1983): Miocene equatorial and southwest Pacific paleoceanography from stable isotope evidence. - Marine Micropaleontology,8, 215–233.
McCorkle, D. C., Emerson, S. R., andQuay, P. D. (1985): Stable carbon isotopes in marine pore waters. - Earth Planet. Sci. Letters,74, 13–26.
Miller, K. G. &Fairbanks, R. G. (1983): Evidence for Oligocene-Middle Miocene abyssal circulation changes in the western North Atlantic. - Nature,306, 250–253.
- &Fairbanks, R. G. (1985): Oligocene-Miocene global carbon and abyssal circulation changes. - In:Sundquist, E. &Broecker, W. (eds.), The Carbon Cycle and Atmospheric CO2: Natural variations Archaean to present, Amer. Geophys. Union Geophys. Monograph,32, 469– 486.
— &Thomas, E. (1985): Late Eocene to Oligocene benthic foraminiferal isotopic record, Site 574 equatorial Pacific. - Init. Rpts. DSDP,85, 771–777.
Neftel, A., Oeschger, H., Schwander, J., Stauffer, B. &Zumbrunn, R. (1982): Ice core sample measurements give atmospheric CO2 content during the past 40,000 years. - Nature,295, 220–223.
Oeschger, H.,Beer, J.,Siegenthaler, U.,Stauffer, B.,Dansgaard, W.Si Langway, C. C. (1984): Late glacial climate history from ice cores. - In: J.Hansen & T.Takahashi (eds.), Climate Processes and Climate sensitivity, Amer. Geophys. Union, Geophys, Monograph29, 299–306.
Redfield, A. C., Ketchum, B. H. &Richards, F. A. (1963): The influence of organisms on the low position of sea water.-In:Hill, M. N. (ed.), The Low Position of Sea Water Comparative and Descriptive Oceanography, The Sea, 2, Wiley and Sons, New York, 26–77.
Reimers, R. E., Kalhorn, S., Emerson, S. R. &Nealson, K. H. (1984): Oxygen consumption rates in pelagic sediments from the Central Pacific: first estimates from microelectrode profiles. - Geochim. Cosmochim. Acta,48, 903–910.
Riedel, W. R. &Saito, T. (eds.) (1979): Marine Plankton and Sediments. - Micropaleontology, Special Pub. No. 3, Micropaleontology Press, New York, 159 pp.
Savin, S. M. &Douglas, R. G. (1973): Stable isotope and magnesium geochemistry of Recent planktonic Foraminifera from the South Pacific. - Geol. Soc. Am. Bull.,84, 2327–2342.
—, — &Stehli, F. G. (1975): Tertiary marine paleotemperatures. - Geol. Soc. Am. Bull.,86, 1499–1510.
—, —,Keller, G., Killingley, J. S., Shaughnessy, J. L., Sommer, M. A., Vincent, E. &Woodruff, F. (1981): Miocene benthic foraminiferal isotope records: a synthesis. - Mar. Micropaleontol.,6, 423–450.
Scholle, P. A. &Arthur, M. A. (1980): Carbon isotopic fluctuations in pelagic limestones: potential stratigraphic and petroleum exploration tool. - Amer. Assoc. Petrol. Geol. Bull.,64, 65–87.
Shackleton, N. (1977): Carbon-13 in Uvigerina: tropical rainforest history and the equatorial Pacific carbonate dissolution cycles. - In:N. R. Andersen &A. Malahoff (eds.) The Fate of Fossil Fuel CO2 in the Oceans:- Plenum Press, New York, 401–427.
— &Kennett, J. P. (1975): Paleotemperature history of the Cenozoic and initiation of Antarctic glaciation: oxygen and carbon isotope analyses in DSDP Sites 277, 279 and 281. - Init. Repts. DSDP29, 743–755.
—,Hall, M. A., Line &Shuxi, C. (1983a): Carbon isotope data in core V19-30 confirm reduced carbon dioxide concentration in the ice age atmosphere. - Nature,306, 319–322.
—,Imbrie, J. &Hall, M. A. (1983b): Oxygen and carbon isotope record of east Pacific core V19-30: Implications for formation of deep water in the Pleistocene North Atlantic. - Earth Planet. Sci. Lett.,65, 233–244.
—,Hall, M. A. &Boersma, A. (1984): Oxygen and carbon isotope data from Leg 74 foraminifera. - Init. Repts. DSDP,74, 599–612.
Tappan, H. (1968): Primary production, isotopes, extinctions and the atmosphere: Palaeogeog., Palaeoclim., Palaeoec,4, 187–210.
Vail, P. R. &Hardenbol, J. (1979): Sea level changes during the Tertiary: - Oceanus,22, 71–79.
Van Andel, T. H.,Heath, G. R. &Moore, T. C., JR. (1975): Cenozoic history and paleoceanography of the central equatorial Pacific.-Mem. Geol. Soc. Am.,143.
Vergnaud-Grazzini, C. &Rabussier-Lointier, D. (1980): Essai de corrélation stratigraphique par le moyen des isotopes de l'oxygène et du carbone. - Bull. Soc. Geól. France, (7)22, 719–730.
Vincent, E. &Berger, W. H. (1985): Carbon dioxide and polar cooling in the Miocene: the Monterey Hypothesis. - In:Sundquist, E. T. &Broecker, W. S. (eds.), The Carbon Cycle and Atmospheric CO2; Natural Variations Archean to Present. Am. Geophys. Union, Geophys. Monograph32, 455–468.
— &Killingley, J. S. (1985): Oxygen and carbon isotope record for the Early and Middle Miocene in the Central Equatorial Pacific (DSDP Leg 85) and paleoceanographic implications. - In: Init. Repts. DSDP,85, 749–769.
—, — (1980): The Magnetic Epoch-6 carbon shift: a change in the ocean's13C/12C ratio 6.2 million years ago. - Mar. Micropaleontol.,5, 185–203.
—, — (1981a): Stable isotope composition of benthic foraminifera from the equatorial Pacific. - Nature,289, 639–643.
—, — (1981b): Stable isotopes in benthic foraminifera from Ontong-Java-Plateau. Box Cores ERDC 112 and 123. - Palaeogeogr., Palaeoclimatol., Palaeoecol.,33, 221–230.
-, -& - (1985): Miocene oxygen and carbon isotope stratigraphy of the tropical Indian Ocean. - In:Kennett, J. (ed.), The Miocene Ocean: Paleoceanography and Biogeography, Mem. Geol. Soc. Am.,163, 103–130.
Weyl, P. K. (1968): The role of the oceans in climatic change: a theory of the ice ages. - Met. Monogr.8 (30), 37–62.
Woodruff, F. &Savin, S. M. (1985): σ13C values of Miocene Pacific benthic foraminifera: correlations with sea level and productivity. - Geology,13, 119–122.