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Holocene Vegetational History of the Kootenai River Valley, Montana

Published online by Cambridge University Press:  20 January 2017

Richard N. Mack ,
N. W. Rutter  and
S. Valastro
Richard N. Mack
Affiliation:
Department of Botany, Washington State University, Pullman, Washington 99164 USA
N. W. Rutter
Affiliation:
Department of Geology, University of Alberta, Edmonton, Alberta T6G 2E1, Canada
S. Valastro
Affiliation:
Radiocarbon Laboratory, Balcones Research Center, 10100 Burnet Road, Austin, Texas 78758 USA
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Abstract

Pollen records in the Kootenai and Fisher River drainages in western Montana reveal a fivezone sequence of Holocene vegetation change. Deposition of Glacier Peak Ash-Layer G (ca. 10,540 ± 660 yr B.P.) in the lowermost sediments (clay intermixed with pebbles) at Tepee Lake gives a minimum date for the initiation of sedimentation. Initial vegetation on the newly deglaciated terrain was dominated by Pinus (probably white bark pine) with small amounts of Gramineae, Picea and Abies, reflecting a relatively cool, moist macroclimate. Two vegetation units appear to contribute to Pollen Zone II (ca. 11,000–7100 yr B.P.): arboreal communities with pines, along with Pseudotsuga or Larix, or both, and treeless vegetation dominated by Artemisia. Pollen Zone II represents an overall warmer macroclimate than occurred upon ice withdrawal. After ca. 7100 yr B.P. (Pollen Zone III) diploxylon pines became a major pollen contributor near both Tepee Lake and McKillop Creek Pond, indicating an expansion of xerophytic forest (P. contorta and P. ponderosa) along with an increase in the prominence of Pseudotsuga menziesii or Larix occidentalis, or both. Artemisia briefly expanded coverage near Tepee Lake concomitant with the Mazama ashfall ca. 6700 yr B.P. A short-term climatic trend with more available water began after ca. 4000 yr B.P. as Abies (probably A. grandis) along with Picea engelmannii became a more regular component of the forest surrounding both sites. Emergence of the modern macroclimate is indicated primarily with the first regular appearance of Tsuga heterophylla in the pollen record by ca. 2700 yr B.P., synchronous with the development of western hemlock forest within the same latitudes in northern Idaho and northeastern Washington.

Type
Original Articles
Information
Quaternary Research , Volume 20 , Issue 2 , September 1983 , pp. 177 - 193
Copyright
University of Washington

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