The DOI matches its Crossref record.
A previously unrecognized late-glacial cold event in eastern North America
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Each is checked against this paper’s own text: does it say what the citing paper says it does?
The change from organic to inorganic sediments characteristic of the Younger Dryas in Nova Scotia and New Brunswick is not found at the White Mountain sites.
“The change from organic to inorganic sediments characteristic of the Younger Dryas in Nova Scotia and New Brunswick (Mott et al. 1986, Levesque et al. 1993) is not found at our White Mountain sites.”
From Late Quaternary History of Low‐ and Mid‐Elevation Vegetation in the White Mountains of New Hampshire (1994) · cites this paper as Levesque et al. 1993
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Cites
No references could be resolved yet.
Research works printed but not linked: 19
- Berger, W. H. Palaeogeogr. Palaeoclimatol. Palaeoecol. 89, 219–237 (1990). · DOI
- Broecker, W. S. Quat Res. 38, 135–138 (1992). · DOI
- Eicher, U. Mitt. Naturforsch. Ges. Bern 37, 65–80 (1980).
- Eicher, U. & Siegenthaler, U. Boreas 5, 109–117 (1976). · DOI
- Lotter, A., Ammann, B. & Sturm, M. Clim. Dyn. 6, 233–239 (1992). · DOI
- Siegenthaler, U., Eicher, U., Oeschger, H. & Dansgaard, W. Ann. Glaciol. 5, 149–152 (1984). · DOI
- Oeschger, H. et al. Geophys. Monogr. 29 (eds Hansen, J. E. & Takahashi. T.) 299–306 (AGU, Washington, DC, 1984).
- Johnsen, S. J. et al. Nature 359, 311–313 (1992). · DOI
- Riezebos, P. A. & Slotboom, R. T. Boreas 13, 347–353 (1984). · DOI
- Iversen, J. Danm. geol. Unders. 7, 345–445 (1973).
- Paus, A. Boreas 17, 113–139 (1988). · DOI
- Paus, A. J. Quat. Sci. 4, 223–242 (1989) · DOI
- Broecker, W. S. et al. Paleoceanography 3, 1–19 (1988). · DOI
- Lehman, S. J. & Keigwin, L. D. Nature 356, 757–762 (1992). · DOI
- Mott, R. J., Grant, D. R., Stea, R. & Occhietti, S. Nature 323, 247–250 (1986). · DOI · Paper page
- Stea, R. R. & Mott, R. J. Boreas 18, 169–187 (1989). · DOI
- Mayle, F. E., Levesque, A. J. & Cwynar, L. C. Quat. Res. (in the press).
- Wilson, S. E., Walker, I. R., Mott, R. J. & Smol, J. P. Clim. Dyn. (in the press).
- Bogaard, P. & Schmincke, H.-U. Geol. Soc. Am. Bull. 96, 1554–1571 (1985). · DOI
Cited by
Sorted by citations
EVIDENCE FOR THE CLOSE CLIMATIC CONTROL OF NEW ENGLAND VEGETATION HISTORY
Shuman, B., Newby, P., Huang, Y., & Webb, T. (2004) · Ecology · doi:10.1890/02-0286 · Cited by 161
Late Quaternary History of Low‐ and Mid‐Elevation Vegetation in the White Mountains of New Hampshire
Spear, R. W., Davis, M. B., & Shane, L. C. K. (1994) · Ecological Monographs · doi:10.2307/2937056 · Cited by 125
Natural Hybrids and Gene Flow between Upland and Lowland Switchgrass
Zhang, Y., Zalapa, J., Jakubowski, A. R., Price, D. L., Acharya, A., Wei, Y., Brummer, E. C., Kaeppler, S. M., & Casler, M. D. (2011) · Crop Science · doi:10.2135/cropsci2011.02.0104 · Cited by 77
Late-Quaternary history of the alpine flora of the New Hampshire White Mountains
Miller, N. G., & Spear, R. W. (2002) · Géographie physique et Quaternaire · doi:10.7202/004854ar · Cited by 31
A late-glacial transition from Picea glauca to Picea mariana in southern New England
Lindbladh, M., Oswald, W. W., Foster, D. R., Faison, E. K., Hou, J., & Huang, Y. (2007) · Quaternary Research · doi:10.1016/j.yqres.2007.01.010 · Cited by 23
Metadata
- Authors
- Levesque, A. J., Mayle, F. E., Walker, I. R., & Cwynar, L. C.
- Venue
- Nature
- Published
- 1993-02
- Volume
- 361
- Issue
- 6413
- Pages
- 623-626
- ISSN
- 0028-0836
- 1476-4687
- Cited by
- 163
- References
- 0
- Language
- en
- Update notices
- correction (1993-05-13)
- Licence
- www.springer.com/tdm (tdm)
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Registry, retraction, Cites and statistics results are computed, not judged, with one exception: a printed reference that no index lists is read once by a model before it counts as a citation error. Claims are extracted by a model and kept only when their quote appears verbatim in the text; each cited source is then checked, with a model’s help, for whether it says what the claim relies on. Those verdicts can be wrong — read the claim’s quote and the cited source before relying on one.
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