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Postglacial vegetational changes along an elevational gradient in the Adirondack Mountains (New York) : a study of plant macrofossils

Jackson, Stephen T., Biological Survey (N.Y.)·1989·Bulletin
DOI 10.5962/bhl.title.135549
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  • Macrofossil evidence from the Adirondack Mountains and the White Mountains shows raised elevational limits for white pine (300 m), hemlock (300 m, Adirondacks; 200 m, White Mountains), and yellow birch (150 m, Adirondacks), interpreted as an increase in temperature of 1°C or more from about 9000 to at least 4000 yBP.

    “Macrofossil evidence from the Adirondack Mountains (Jackson, 1989;Whitehead and Jackson, 1990) and the White Mountains (Spear et al., 1994) shows raised elevational limits for white pine (300 m), hemlock (300 m, Adirondacks; 200 m, White Mountains), and yellow birch (Betula alleghaniensis Britt.)(150 m, Adirondacks), which is interpreted as an increase in temperature of 1°C or more from about 9000”

    From Late-Quaternary history of the alpine flora of the New Hampshire White Mountains (2002) · cites this paper as Jackson, 1989

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Research works printed but not linked: 51

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Metadata

Authors
Jackson, S. T., & (N.Y.), B. S.
ORCID
Jackson, Stephen T.
Venue
Bulletin
Publisher
University of the State of New York, State Education Dept., New York State Museum, Biological Survey
Published
1989
ISSN
0278-3355
DOI
10.5962/bhl.title.135549
Cited by
24
References
2

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