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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.
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15
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10544227999
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18O results into good agreement (Fig. 4A).
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18O results into good agreement (Fig. 4A).
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16
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0028254914
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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).
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Hughes, M.K.1
Diaz, H.F.2
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0028190420
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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).
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0028254914
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Routledge, London
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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).
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Jones, P.D.2
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10544244864
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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.
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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)].
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(1965)
Symposium on Marine Geochemistry Occas. Publ. 3
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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)].
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10544227584
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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).
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10544230887
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57
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10544225205
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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.
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