The DOI matches its DataCite record; 1 of the 1 references it cites were found in a registry or an index.
Pleistocene and Holocene Flora of New England as a Framework for Interpreting Aspects of Plant Rarity
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(Uploaded by Plazi from the Biodiversity Heritage Library) No abstract provided.
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Mosses associated with calcareous soil or bedrock predominate in the late-glacial record of New York-New England, even when the fossils were recovered from areas of acidic bedrock and soil.
“Mosses associated with calcareous soil or bedrock predominate in the late-glacial record of New York-New England (Miller, 1987a(Miller, , b, 1989)), even when the fossils were recovered from areas of acidic bedrock and soil.”
From Late-Quaternary history of the alpine flora of the New Hampshire White Mountains (2002) · cites this paper as Miller, 1989
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Citations
Cites
Late Glacial and Early Holocene Landscapes in Northern New England and Adjacent Areas of Canada
Davis, R. B., & Jacobson, G. L. (1985) · Quaternary Research · doi:10.1016/0033-5894(85)90040-7 · Cited by 162
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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
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Metadata
- Authors
- Miller, N. G.
- Venue
- New England Botanical Club [etc.]
- Publisher
- New England Botanical Club [etc.]
- Published
- 1989
- References
- 1
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