메뉴 건너뛰기




Volumn 274, Issue 5292, 1996, Pages 1504-1508

The little ice age and medieval warm period in the Sargasso Sea

Author keywords

[No Author keywords available]

Indexed keywords

CARBON 14; SODIUM CHLORIDE;

EID: 0029659429     PISSN: 00368075     EISSN: None     Source Type: Journal    
DOI: 10.1126/science.274.5292.1504     Document Type: Article
Times cited : (410)

References (57)
  • 1
    • 10544226021 scopus 로고
    • N. G. Pisias, Quat. Res. 10, 66 (1978); A. Juillet-Leclerc and H. Schrader, Nature 329, 146 (1987); J. P. Kennett and B. L. Ingram, ibid. 377, 510 (1995); K. A. Hughen, J. T. Overpeck, L. C. Peterson, S. Trumbore, ibid. 380, 51 (1996).
    • (1978) Quat. Res. , vol.10 , pp. 66
    • Pisias, N.G.1
  • 2
    • 0023524565 scopus 로고
    • N. G. Pisias, Quat. Res. 10, 66 (1978); A. Juillet-Leclerc and H. Schrader, Nature 329, 146 (1987); J. P. Kennett and B. L. Ingram, ibid. 377, 510 (1995); K. A. Hughen, J. T. Overpeck, L. C. Peterson, S. Trumbore, ibid. 380, 51 (1996).
    • (1987) Nature , vol.329 , pp. 146
    • Juillet-Leclerc, A.1    Schrader, H.2
  • 3
    • 0029509059 scopus 로고
    • N. G. Pisias, Quat. Res. 10, 66 (1978); A. Juillet-Leclerc and H. Schrader, Nature 329, 146 (1987); J. P. Kennett and B. L. Ingram, ibid. 377, 510 (1995); K. A. Hughen, J. T. Overpeck, L. C. Peterson, S. Trumbore, ibid. 380, 51 (1996).
    • (1995) Nature , vol.377 , pp. 510
    • Kennett, J.P.1    Ingram, B.L.2
  • 4
    • 0029668978 scopus 로고    scopus 로고
    • N. G. Pisias, Quat. Res. 10, 66 (1978); A. Juillet-Leclerc and H. Schrader, Nature 329, 146 (1987); J. P. Kennett and B. L. Ingram, ibid. 377, 510 (1995); K. A. Hughen, J. T. Overpeck, L. C. Peterson, S. Trumbore, ibid. 380, 51 (1996).
    • (1996) Nature , vol.380 , pp. 51
    • Hughen, K.A.1    Overpeck, J.T.2    Peterson, L.C.3    Trumbore, S.4
  • 5
    • 0022823460 scopus 로고
    • P. D. Jones, T. M. L. Wigley, P. B. Wright, Nature 322, 430 (1986); B. D. Santer et al., Clin. Dynam. 12, 77 (1995); B. D. Santer et al., Nature 382, 39 (1996).
    • (1986) Nature , vol.322 , pp. 430
    • Jones, P.D.1    Wigley, T.M.L.2    Wright, P.B.3
  • 6
    • 0029530918 scopus 로고
    • P. D. Jones, T. M. L. Wigley, P. B. Wright, Nature 322, 430 (1986); B. D. Santer et al., Clin. Dynam. 12, 77 (1995); B. D. Santer et al., Nature 382, 39 (1996).
    • (1995) Clin. Dynam. , vol.12 , pp. 77
    • Santer, B.D.1
  • 7
    • 0029663322 scopus 로고    scopus 로고
    • P. D. Jones, T. M. L. Wigley, P. B. Wright, Nature 322, 430 (1986); B. D. Santer et al., Clin. Dynam. 12, 77 (1995); B. D. Santer et al., Nature 382, 39 (1996).
    • (1996) Nature , vol.382 , pp. 39
    • Santer, B.D.1
  • 8
    • 0019367070 scopus 로고
    • E. P. Laine and C. D. Hollister, Mar. Geol. 39, 277 (1981); W. J. McCartney and M. S. McCartney, Rev. Geophys. 31, 29 (1993).
    • (1981) Mar. Geol. , vol.39 , pp. 277
    • Laine, E.P.1    Hollister, C.D.2
  • 11
    • 0024484685 scopus 로고
    • M. P. Bacon and J. N. Rosholt, Geochim. Cosmochim. Acta 46, 651 (1982); D. O. Suman and M. P. Bacon, Deep-Sea Res. 36, 869 (1989).
    • (1989) Deep-Sea Res. , vol.36 , pp. 869
    • Suman, D.O.1    Bacon, M.P.2
  • 13
    • 10544244014 scopus 로고
    • _, Deep-Sea Res. 36, 845 (1989).
    • (1989) Deep-Sea Res. , vol.36 , pp. 845
  • 14
    • 10544247634 scopus 로고    scopus 로고
    • BC-004 was recovered from 33°41.6'N, 57°36.7'W by CSS Hudson at 4418 m on the undulating plateau of the northeast Bermuda Rise, within 1000 m ot KNR31 GPC-5 (6) and EN120 GGC1 (17). The box core was subcored using plastic pipe with a diameter of 11.4 cm.
    • BC-004 was recovered from 33°41.6'N, 57°36.7'W by CSS Hudson at 4418 m on the undulating plateau of the northeast Bermuda Rise, within 1000 m ot KNR31 GPC-5 (6) and EN120 GGC1 (17). The box core was subcored using plastic pipe with a diameter of 11.4 cm.
  • 15
    • 10544227999 scopus 로고    scopus 로고
    • 18O results into good agreement (Fig. 4A).
    • 18O results into good agreement (Fig. 4A).
  • 16
    • 0028254914 scopus 로고
    • In this report these names are used informally to denote cooling several hundred years ago, and warming about 1000 years ago. Although there is general agreement that there was cooling and glacial expansion in many regions during the LIA interval, and warming during the MWP interval, it is by no means certain that specific events or even these intervals were synchronous and worldwide. Contrast, for example, M. K. Hughes and H. F. Diaz, Clim. Change 26, 109 (1994) with J. M. Grove and R. Switsur, ibid. 26, 143 (1994). See also R. S. Bradley and P. D. Jones, Climate Since A.D. 1500 (Routledge, London, 1995).
    • (1994) Clim. Change , vol.26 , pp. 109
    • Hughes, M.K.1    Diaz, H.F.2
  • 17
    • 0028190420 scopus 로고
    • In this report these names are used informally to denote cooling several hundred years ago, and warming about 1000 years ago. Although there is general agreement that there was cooling and glacial expansion in many regions during the LIA interval, and warming during the MWP interval, it is by no means certain that specific events or even these intervals were synchronous and worldwide. Contrast, for example, M. K. Hughes and H. F. Diaz, Clim. Change 26, 109 (1994) with J. M. Grove and R. Switsur, ibid. 26, 143 (1994). See also R. S. Bradley and P. D. Jones, Climate Since A.D. 1500 (Routledge, London, 1995).
    • (1994) Clim. Change , vol.26 , pp. 143
    • Grove, J.M.1    Switsur, R.2
  • 18
    • 0028254914 scopus 로고
    • Routledge, London
    • In this report these names are used informally to denote cooling several hundred years ago, and warming about 1000 years ago. Although there is general agreement that there was cooling and glacial expansion in many regions during the LIA interval, and warming during the MWP interval, it is by no means certain that specific events or even these intervals were synchronous and worldwide. Contrast, for example, M. K. Hughes and H. F. Diaz, Clim. Change 26, 109 (1994) with J. M. Grove and R. Switsur, ibid. 26, 143 (1994). See also R. S. Bradley and P. D. Jones, Climate Since A.D. 1500 (Routledge, London, 1995).
    • (1995) Climate since A.D. 1500
    • Bradley, R.S.1    Jones, P.D.2
  • 20
    • 0021599868 scopus 로고
    • Brief events of intense deep current activity and sediment resuspension known as abyssal storms have been observed off Nova Scotia by C. D. Hollister and I. N. McCave [Nature 309, 220 (1994)].
    • (1994) Nature , vol.309 , pp. 220
    • Hollister, C.D.1    McCave, I.N.2
  • 24
    • 0027789167 scopus 로고
    • H. C. Hass, Mar. Geol. 111, 361 (1993); D. J. W. Piper, M. Feetham, J. Goulden, paper presented at the Fifth International Conference on Paleoceanography, Halifax, Nova Scotia, 10 to 14 October 1995, p. 58.
    • (1993) Mar. Geol. , vol.111 , pp. 361
    • Hass, H.C.1
  • 27
    • 0029529638 scopus 로고
    • E. A. Boyle and P. D. Rosener, Palaeogéogr. Palaeoclimatol. Palaececol. 89, 113 (1990); D. W. Oppo and S. J. Lehman, Paleoceanography 10, 901 (1995).
    • (1995) Paleoceanography , vol.10 , pp. 901
    • Oppo, D.W.1    Lehman, S.J.2
  • 32
    • 0001133281 scopus 로고
    • L. D. Talley and M. E. Raymer, J. Mar. Res. 40 (suppl.), 757 (1982); W. J. Jenkins, ibid., p. 265.
    • (1982) J. Mar. Res. , vol.40 , Issue.SUPPL. , pp. 757
    • Talley, L.D.1    Raymer, M.E.2
  • 33
    • 10544221481 scopus 로고    scopus 로고
    • L. D. Talley and M. E. Raymer, J. Mar. Res. 40 (suppl.), 757 (1982); W. J. Jenkins, ibid., p. 265.
    • J. Mar. Res. , pp. 265
    • Jenkins, W.J.1
  • 35
    • 10544244864 scopus 로고    scopus 로고
    • 18O values, the influences of temperature and salinity changes in the Sargasso Sea surface are additive, whereas they tend to cancel each other at other locations
    • 18O values, the influences of temperature and salinity changes in the Sargasso Sea surface are additive, whereas they tend to cancel each other at other locations.
  • 36
    • 0001528193 scopus 로고
    • D. R. Cayan, J. Clin. 5, 354 (1992); Y. Kushnir, ibid. 7, 141 (1994).
    • (1992) J. Clin. , vol.5 , pp. 354
    • Cayan, D.R.1
  • 37
    • 0028262614 scopus 로고
    • D. R. Cayan, J. Clin. 5, 354 (1992); Y. Kushnir, ibid. 7, 141 (1994).
    • (1994) J. Clin. , vol.7 , pp. 141
    • Kushnir, Y.1
  • 39
    • 85088083480 scopus 로고
    • Narragansett Marine Laboratory, Naragansett, RI
    • 18O relationship [H. Craig and L. I. Gordon, Symposium on Marine Geochemistry (Occas. Publ. 3, Narragansett Marine Laboratory, Naragansett, RI, 1965)], and Shackleton's paleotemperature equation [N. J. Shackleton, CNRS Colloq. 219, 203 (1974)].
    • (1965) Symposium on Marine Geochemistry Occas. Publ. 3
    • Craig, H.1    Gordon, L.I.2
  • 40
    • 0000752576 scopus 로고
    • 18O relationship [H. Craig and L. I. Gordon, Symposium on Marine Geochemistry (Occas. Publ. 3, Narragansett Marine Laboratory, Naragansett, RI, 1965)], and Shackleton's paleotemperature equation [N. J. Shackleton, CNRS Colloq. 219, 203 (1974)].
    • (1974) CNRS Colloq. , vol.219 , pp. 203
    • Shackleton, N.J.1
  • 42
    • 10544227584 scopus 로고    scopus 로고
    • 18O results most likely reflect sedimentary processes such as bioturbation. All data are archived at the NOAA/NGDC World Data Center-A for Paleoclimatology (paleo@mail.ngdc.noaa.gov)
    • 18O results most likely reflect sedimentary processes such as bioturbation. All data are archived at the NOAA/NGDC World Data Center-A for Paleoclimatology (paleo@mail.ngdc.noaa.gov).
  • 44
    • 10544230887 scopus 로고
    • Kiel
    • J. Patzold and G. Wefer, paper presented at the Fourth International Conference on Paleoceanography, Kiel, p. 224 (1992); R. B. Dunbar and J. E. Cole, Coral Records of Ocean-Atmosphere Variability (University Corporation for Atmospheric Research, Boulder, CO, 1993).
    • (1992) Fourth International Conference on Paleoceanography , pp. 224
    • Patzold, J.1    Wefer, G.2
  • 45
    • 0003453639 scopus 로고
    • University Corporation for Atmospheric Research, Boulder, CO
    • J. Patzold and G. Wefer, paper presented at the Fourth International Conference on Paleoceanography, Kiel, p. 224 (1992); R. B. Dunbar and J. E. Cole, Coral Records of Ocean-Atmosphere Variability (University Corporation for Atmospheric Research, Boulder, CO, 1993).
    • (1993) Coral Records of Ocean-Atmosphere Variability
    • Dunbar, R.B.1    Cole, J.E.2
  • 48
    • 0012002094 scopus 로고
    • M. R. Talbot and G. Delibrias, ibid 268, 722 (1977); Earth Planet. Sci. Lett. 47, 336 (1980).
    • (1977) Nature , vol.268 , pp. 722
    • Talbot, M.R.1    Delibrias, G.2
  • 49
    • 0019187292 scopus 로고
    • M. R. Talbot and G. Delibrias, ibid 268, 722 (1977); Earth Planet. Sci. Lett. 47, 336 (1980).
    • (1980) Earth Planet. Sci. Lett. , vol.47 , pp. 336
  • 50
    • 0025624861 scopus 로고
    • K. R. Briffa et al., Nature 346, 434 (1990); Clin. Dynam. 7, 111 (1992).
    • (1990) Nature , vol.346 , pp. 434
    • Briffa, K.R.1
  • 51
    • 0026478038 scopus 로고
    • K. R. Briffa et al., Nature 346, 434 (1990); Clin. Dynam. 7, 111 (1992).
    • (1992) Clin. Dynam. , vol.7 , pp. 111
  • 57
    • 10544225205 scopus 로고    scopus 로고
    • I thank C. E. Franks and E. Roosen for technical assistance; R. Bradley, E. Druffel, and R. Dunbar for comments on the manuscript; M. McCartney, T. Joyce, W. Schmitz, E. Boyle, S. Lehman, and W. Jenkins for discussions; and I. Hardy, K. Moran, and the Bedford Institute of Oceanography for help in acquiring and archiving BC-004. This work was funded by the NOAA Atlantic Climate Change Program
    • I thank C. E. Franks and E. Roosen for technical assistance; R. Bradley, E. Druffel, and R. Dunbar for comments on the manuscript; M. McCartney, T. Joyce, W. Schmitz, E. Boyle, S. Lehman, and W. Jenkins for discussions; and I. Hardy, K. Moran, and the Bedford Institute of Oceanography for help in acquiring and archiving BC-004. This work was funded by the NOAA Atlantic Climate Change Program.


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.