메뉴 건너뛰기




Volumn 5, Issue 8, 2004, Pages

Crystallinity of foraminifera shells: A proxy to reconstruct past bottom water CO3= changes?

Author keywords

Bottom water CO3; Calcite crystallinity; Carbonate dissolution; Foraminifers

Indexed keywords


EID: 20744435181     PISSN: 15252027     EISSN: 15252027     Source Type: Journal    
DOI: 10.1029/2003GC000668     Document Type: Article
Times cited : (30)

References (39)
  • 1
    • 0037034770 scopus 로고    scopus 로고
    • Glacial-interglacial stability of ocean pH inferred from foraminifer dissolution rates
    • Anderson, D. M., and D. Archer (2002), Glacial-interglacial stability of ocean pH inferred from foraminifer dissolution rates, Nature, 416, 70-73.
    • (2002) Nature , vol.416 , pp. 70-73
    • Anderson, D.M.1    Archer, D.2
  • 2
    • 0029730825 scopus 로고    scopus 로고
    • An atlas of the distribution of calcium carbonate in sediments of the deep sea
    • Archer, D. E. (1996), An atlas of the distribution of calcium carbonate in sediments of the deep sea, Global. Biogeochem. Cycles, 10, 159-174.
    • (1996) Global. Biogeochem. Cycles , vol.10 , pp. 159-174
    • Archer, D.E.1
  • 4
    • 0036139994 scopus 로고    scopus 로고
    • A new, mechanistic model for organic carbon fluxes in the ocean based on the quantitative association of POC with ballast minerals
    • Armstrong, R. A., C. Lee, J. I. Hedges, S. Honjo, and S. G. Wakeham (2002), A new, mechanistic model for organic carbon fluxes in the ocean based on the quantitative association of POC with ballast minerals, Deep Sea Res., Part II, 49, 219-236.
    • (2002) Deep Sea Res., Part II , vol.49 , pp. 219-236
    • Armstrong, R.A.1    Lee, C.2    Hedges, J.I.3    Honjo, S.4    Wakeham, S.G.5
  • 7
    • 37049250562 scopus 로고
    • Carbonate compensation depth: Relation to carbonate solubility in ocean waters
    • Ben Yaakov, S., E. Ruth, and I. R. Kaplan (1974), Carbonate compensation depth: Relation to carbonate solubility in ocean waters, Science, 184, 982-984.
    • (1974) Science , vol.184 , pp. 982-984
    • Ben Yaakov, S.1    Ruth, E.2    Kaplan, I.R.3
  • 8
    • 0001802810 scopus 로고
    • Planktonic foraminifera: Selective solution and paleoclimatic interpretation
    • Berger, W. H. (1968), Planktonic foraminifera: Selective solution and paleoclimatic interpretation, Deep Sea Res. Oceanogr. Abstr., 15, 31-43.
    • (1968) Deep Sea Res. Oceanogr. Abstr. , vol.15 , pp. 31-43
    • Berger, W.H.1
  • 9
    • 0001331322 scopus 로고
    • Planktonic foraminifera: Selective solution and the lysocline
    • Berger, W. H. (1970), Planktonic foraminifera: Selective solution and the lysocline, Mar. Geol., 8, 111-138.
    • (1970) Mar. Geol. , vol.8 , pp. 111-138
    • Berger, W.H.1
  • 10
    • 1642376171 scopus 로고    scopus 로고
    • Impact of the ocean carbonate chemistry on living foraminiferal shell weight: Comment on "carbonate ion concentration in glacial-age deep waters of the Caribbean Sea"
    • doi:10.1029/2002GC000388, by W. S. Broecker and E. Clark
    • Bijma, J.,B.Honisch, and R. E. Zeebe (2002), Impact of the ocean carbonate chemistry on living foraminiferal shell weight: Comment on ''Carbonate ion concentration in glacial-age deep waters of the Caribbean Sea'' by W. S. Broecker and E. Clark, Geochem. Geophys. Geosyst., 3(11), 1064, doi:10.1029/2002GC000388.
    • (2002) Geochem. Geophys. Geosyst. , vol.3 , Issue.11 , pp. 1064
    • Bijma J.B.Honisch1    Zeebe, R.E.2
  • 11
    • 0019188395 scopus 로고
    • Variations isotopiques (oxygene et carbone) et crystallographiques chez des espèces actuelles de foraminifères planctoniques en fonction de la profondeur de dépôt
    • Bonneau,M.C., F. Mélières, and C. Vergnaud-Grazzini (1980), Variations isotopiques (oxygene et carbone) et crystallographiques chez des espèces actuelles de foraminifères planctoniques en fonction de la profondeur de dépôt, Bull. Soc. Geol. Fr., 22(5), 791-793.
    • (1980) Bull. Soc. Geol. Fr. , vol.22 , Issue.5 , pp. 791-793
    • Bonneau, M.C.1    Mélières, F.2    Vergnaud-Grazzini, C.3
  • 12
    • 0023699802 scopus 로고
    • 2 cycles
    • 2 cycles, Nature, 331, 55-56.
    • (1988) Nature , vol.331 , pp. 55-56
    • Boyle, E.A.1
  • 13
    • 0033374414 scopus 로고    scopus 로고
    • 3 size distribution: A paleocarbonate ion proxy?
    • 3 size distribution: A paleocarbonate ion proxy?, Paleoceanography, 14(5), 596-604.
    • (1999) Paleoceanography , vol.14 , Issue.5 , pp. 596-604
    • Broecker, W.S.1    Clark, E.2
  • 14
    • 0035824430 scopus 로고    scopus 로고
    • Glacial-to-Holocene redistribution of carbonate ion in the deep sea
    • Broecker, W. S., and E. Clark (2001a), Glacial-to-Holocene redistribution of carbonate ion in the deep sea, Science, 294, 2152-2155.
    • (2001) Science , vol.294 , pp. 2152-2155
    • Broecker, W.S.1    Clark, E.2
  • 15
    • 0034753188 scopus 로고    scopus 로고
    • An evaluation of Lohmann's foraminifera weight dissolution index
    • Broecker, W. S., and E. Clark (2001b), An evaluation of Lohmann's foraminifera weight dissolution index, Paleoceanography, 16, 531-534.
    • (2001) Paleoceanography , vol.16 , pp. 531-534
    • Broecker, W.S.1    Clark, E.2
  • 18
    • 0024870077 scopus 로고
    • Thecauseoftheglacial to interglacial atmospheric CO2 change: A polar alkalinity hypothesis
    • Broecker, W. S., andT. H. Peng(1989), Thecauseoftheglacial to interglacial atmospheric CO2 change: A polar alkalinity hypothesis, Global Biogeochem. Cycles, 3(3), 215-239.
    • (1989) Global Biogeochem. Cycles , vol.3 , Issue.3 , pp. 215-239
    • Broecker, W.S.1    Peng, T.H.2
  • 19
    • 0017923002 scopus 로고
    • The relationship between lysocline depth and in situ carbonate ion concentration
    • Broecker, W. S., and T. Takahashi (1978), The relationship between lysocline depth and in situ carbonate ion concentration, Deep Sea Res., 25, 65-95.
    • (1978) Deep Sea Res. , vol.25 , pp. 65-95
    • Broecker, W.S.1    Takahashi, T.2
  • 21
    • 0019390081 scopus 로고
    • Carbon fluxes at the sediment-water interface of the deep sea: Calcium carbonate preservation
    • Emerson, S., and M. Bender (1981), Carbon fluxes at the sediment-water interface of the deep sea: Calcium carbonate preservation, J. Mar. Res., 39, 139-162.
    • (1981) J. Mar. Res. , vol.39 , pp. 139-162
    • Emerson, S.1    Bender, M.2
  • 22
    • 0038373575 scopus 로고    scopus 로고
    • Factors controlling the flux of organic carbon to the bat hypelagic zone of the ocean
    • doi:10.1029/2001GB001722
    • Francois, R., S. Honjo, R. Krishfield, and S. Manganini (2002), Factors controlling the flux of organic carbon to the bat hypelagic zone of the ocean, Global Biogeochem. Cycles, 16(4), 1087, doi:10.1029/2001GB001722.
    • (2002) Global Biogeochem. Cycles , vol.16 , Issue.4 , pp. 1087
    • Francois, R.1    Honjo, S.2    Krishfield, R.3    Manganini, S.4
  • 23
    • 0001542370 scopus 로고
    • The solubility of calcite in the oceans
    • Ingle, S. E. (1975), The solubility of calcite in the oceans, Mar. Chem, 3, 301-319.
    • (1975) Mar. Chem. , vol.3 , pp. 301-319
    • Ingle, S.E.1
  • 24
    • 0018917499 scopus 로고
    • The dissolution kinetics of biogenic calcium carbonates in seawater
    • Keir, R. S. (1980), The dissolution kinetics of biogenic calcium carbonates in seawater, Geochim. Cosmochim. Acta, 44, 241-252.
    • (1980) Geochim. Cosmochim. Acta , vol.44 , pp. 241-252
    • Keir, R.S.1
  • 25
    • 0013415120 scopus 로고    scopus 로고
    • Association of sinking organic matter with various types of mineral ballast in the deep sea: Implications for the rain ratio
    • doi:10.1029/2001GB001765
    • Klaas, C., and D. E. Archer (2002), Association of sinking organic matter with various types of mineral ballast in the deep sea: Implications for the rain ratio, Global Biogeochem. Cycles, 16(4), 1116, doi:10.1029/2001GB001765.
    • (2002) Global Biogeochem. Cycles , vol.16 , Issue.4 , pp. 1116
    • Klaas, C.1    Archer, D.E.2
  • 28
    • 0029527365 scopus 로고
    • A model for variation in the chemistry of planktonic foraminifera due to secondary calcification and selective dissolution
    • Lohmann, G. P. (1995), A model for variation in the chemistry of planktonic foraminifera due to secondary calcification and selective dissolution, Paleoceanography, 10, 445-457.
    • (1995) Paleoceanography , vol.10 , pp. 445-457
    • Lohmann, G.P.1
  • 29
    • 4244124277 scopus 로고
    • Porte-échantillon tournant pour analyse par diffractométrie X
    • Mélières, F. (1973), Porte-échantillon tournant pour analyse par diffractométrie X, Bull. Soc. Fr. Mineral. Cristallogr., 96, 75-79.
    • (1973) Bull. Soc. Fr. Mineral. Cristallogr. , vol.96 , pp. 75-79
    • Mélières, F.1
  • 30
    • 0001439777 scopus 로고
    • X-ray mineralogy studies, Leg 41, Deep Sea Drilling Project, Eastern North Atlantic Ocean
    • Mélières, F. (1978), X-ray mineralogy studies, Leg 41, Deep Sea Drilling Project, Eastern North Atlantic Ocean, Initial Rep. Deep Sea Drill. Proj., 41, 1065-1086.
    • (1978) Initial Rep. Deep Sea Drill. Proj. , vol.41 , pp. 1065-1086
    • Mélières, F.1
  • 31
    • 33746004836 scopus 로고
    • The thermodynamics of the carbonate system in seawater
    • Millero, F. J. (1979), The thermodynamics of the carbonate system in seawater, Geochim. Cosmochim. Acta, 43, 1651-1661.
    • (1979) Geochim. Cosmochim. Acta , vol.43 , pp. 1651-1661
    • Millero, F.J.1
  • 32
    • 0020970301 scopus 로고
    • The solubility of calcite and aragonite in seawater at various salinities, temperatures and one atmosphere total pressure
    • Mucci, A. (1983), The solubility of calcite and aragonite in seawater at various salinities, temperatures and one atmosphere total pressure, Am. J. Sci., 283, 780-799.
    • (1983) Am. J. Sci. , vol.283 , pp. 780-799
    • Mucci, A.1
  • 33
    • 1642353318 scopus 로고    scopus 로고
    • An end to the "rain ratio" reign?
    • doi:10.1029/ 2003GC000512
    • Ridgwell, A. J. (2003), An end to the ''rain ratio'' reign?, Geochem. Geophys. Geosyst., 4(6), 1051, doi:10.1029/ 2003GC000512.
    • (2003) Geochem. Geophys. Geosyst. , vol.4 , Issue.6 , pp. 1051
    • Ridgwell, A.J.1
  • 34
    • 0028976168 scopus 로고
    • Evidence for a higher pH in the glacial ocean from boron isotopes in foraminifera
    • Sanyal, A., N. G. Hemming, G. N. Hanson, and W. S. Broecker (1995), Evidence for a higher pH in the glacial ocean from boron isotopes in foraminifera, Nature, 373, 234-236.
    • (1995) Nature , vol.373 , pp. 234-236
    • Sanyal, A.1    Hemming, N.G.2    Hanson, G.N.3    Broecker, W.S.4
  • 35
    • 0019138872 scopus 로고
    • 3 in seawater at 2°C based upon in-situ sampled pore water composition
    • 3 in seawater at 2°C based upon in-situ sampled pore water composition, Mar. Chem., 9, 223-235.
    • (1980) Mar. Chem. , vol.9 , pp. 223-235
    • Sayles, F.L.1
  • 36
    • 0007657572 scopus 로고
    • Precision of GEOSECS shipboard data
    • Natl. Sci. Found., Washington, D. C., edited by W. S. Broecker, D. W. Spencer, and H. Craig
    • Takahashi, T. (1982), Precision of GEOSECS shipboard data, in GEOSECS Pacific Expedition, vol.3, Hydrographic Data, edited by W. S. Broecker, D. W. Spencer, and H. Craig, pp. 5-10, Natl. Sci. Found., Washington, D. C.
    • (1982) GEOSECS Pacific Expedition, Vol. 3, Hydrographic Data , pp. 5-10
    • Takahashi, T.1
  • 37
    • 0013625843 scopus 로고
    • 2 concentration data
    • edited by R. F. Weiss et al., U.S. Govt. Print. Off., Washington, D. C
    • Takahashi, T. (1983), Precision and accuracy ofthe GEOSECS Indian Ocean alkalinity and total CO2 concentration data, in GEOSECS Indian Ocean Expedition, vol.5, Hydrographic Data, 1977-1978, edited by R. F. Weiss et al., pp. 5-7, U.S. Govt. Print. Off., Washington, D. C.
    • (1983) GEOSECS Indian Ocean Expedition, vol.5, Hydrographic Data 1977-1978 , pp. 5-7
    • Takahashi, T.1
  • 38
    • 0022213456 scopus 로고
    • Redfield ratio based on chemical data from isopycnal surfaces
    • Takahashi, T., W. S. Broecker, and S. Langer (1985), Redfield ratio based on chemical data from isopycnal surfaces, J. Geophys. Res., 90, 6907-6924.
    • (1985) J. Geophys. Res. , vol.90 , pp. 6907-6924
    • Takahashi, T.1    Broecker, W.S.2    Langer, S.3


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.