-
2
-
-
0028184130
-
-
P. Mayewski et al., Science 263, 1747 (1994).
-
(1994)
Science
, vol.263
, pp. 1747
-
-
Mayewski, P.1
-
3
-
-
0028982137
-
-
A. T. Kotilainen and N. J. Shackleton, Nature 377, 323 (1995); E. C. Grimm, G. L. Jacobson Jr., W. A. Watts, B. C. S. Hansen, K. A. Maasch, Science 261, 198 (1993).
-
(1995)
Nature
, vol.377
, pp. 323
-
-
Kotilainen, A.T.1
Shackleton, N.J.2
-
4
-
-
0027842945
-
-
A. T. Kotilainen and N. J. Shackleton, Nature 377, 323 (1995); E. C. Grimm, G. L. Jacobson Jr., W. A. Watts, B. C. S. Hansen, K. A. Maasch, Science 261, 198 (1993).
-
(1993)
Science
, vol.261
, pp. 198
-
-
Grimm, E.C.1
Jacobson Jr., G.L.2
Watts, W.A.3
Hansen, B.C.S.4
Maasch, K.A.5
-
6
-
-
84979434446
-
-
A. McIntyre et al., Paleoceanography 4, 19 (1989); A. McIntyre et al., Program for the Fifth International Conference on Paleoceanography (Halifax, Nova Scotia, 1995), p. 54.
-
(1989)
Paleoceanography
, vol.4
, pp. 19
-
-
McIntyre, A.1
-
9
-
-
2142785916
-
-
C. P. Summerhayes et al., Eds. Wiley, New York
-
G. Reverdin, in Upwelling in the Ocean: Modern Processes and Ancient Records, C. P. Summerhayes et al., Eds. (Wiley, New York, 1995), pp. 125-148.
-
(1995)
Upwelling in the Ocean: Modern Processes and Ancient Records
, pp. 125-148
-
-
Reverdin, G.1
-
15
-
-
0028810066
-
-
T. Fronval et al., Nature 374, 443 (1995).
-
(1995)
Nature
, vol.374
, pp. 443
-
-
Fronval, T.1
-
19
-
-
0003885674
-
-
Holden-Day, Oakland, CA
-
Test of symmetry of a random variable Y about a point c. If we assume that Y has a frequency function p, then symmetry about c is p(Y + c) = p(Y - c). P. J. Bickel and K. A. Doksum, Mathematical Statistics (Holden-Day, Oakland, CA, 1977).
-
(1977)
Mathematical Statistics
-
-
Bickel, P.J.1
Doksum, K.A.2
-
20
-
-
12644265323
-
-
note
-
Calendric chronology of cores RC2402 and RC2408 yields eight peak-to-peak intervals having a range of 8.1 to 9.0 ky, with a mean of 8.43 ky.
-
-
-
-
24
-
-
12644318757
-
-
note
-
14C chronology ranges from ±30 to ±420 for dated samples, but for interpolated values we consider that these estimates could be larger as a result of variation in sedimentation rate. However, in RC2408, F. profunda maxima were either directly AMS-dated or have dates closely allied with them. Calendric conversion yields 2σ errors ranging from ±35 to ±450. We found that the extreme case for the oldest peak-to-peak interval for conversion (15), using a minus error for the younger peak and a plus error for the older peak, is 8.75 ky. The estimate of the oldest interval for conversion (76) is 9.3 ky.
-
-
-
-
25
-
-
0024929479
-
-
A. Berger, Quat. Int. 2, 1 (1989); P. I. Pestiaux et al., Clim. Change 12, 9 (1988).
-
(1989)
Quat. Int.
, vol.2
, pp. 1
-
-
Berger, A.1
-
26
-
-
0002648487
-
-
A. Berger, Quat. Int. 2, 1 (1989); P. I. Pestiaux et al., Clim. Change 12, 9 (1988).
-
(1988)
Clim. Change
, vol.12
, pp. 9
-
-
Pestiaux, P.I.1
-
35
-
-
0030456027
-
-
S. P. Harrison et al., Quat. Res. 45, 138 (1996); S. O. Dahl and A. Nesje, Holocene 3, 269 (1993). Increased precipitation is inferred from changes in vegetation and lake levels and glacial accretion on the continents adjacent to the subpolar North Atlantic after 5 ka.
-
(1996)
Quat. Res.
, vol.45
, pp. 138
-
-
Harrison, S.P.1
-
36
-
-
0030456027
-
-
S. P. Harrison et al., Quat. Res. 45, 138 (1996); S. O. Dahl and A. Nesje, Holocene 3, 269 (1993). Increased precipitation is inferred from changes in vegetation and lake levels and glacial accretion on the continents adjacent to the subpolar North Atlantic after 5 ka.
-
(1993)
Holocene
, vol.3
, pp. 269
-
-
Dahl, S.O.1
Nesje, A.2
-
37
-
-
12644263353
-
-
note
-
We thank M. Yarusinski for assistance. Supported by NSF [MG&G grant OCE93-13821 (95%)], and NSF OCE801015 AMS/National Ocean Sciences Accelerator Mass Spectrometry Facility. This is Lamont-Doherty Earth Observatory contribution 5579.
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