Presettlement Pinus taeda in the Mississippi Valley Alluvial Plain of the Monroe County, Arkansas area

  • Authors: Bragg, Don C.
  • Publication Year: 2005
  • Publication Series: Miscellaneous Publication
  • Source: Journal of the Arkansas Academy of Science, Vol. 59: 187-195

Abstract

Loblolly pine (Pinus taeda) is the most dominant conifer in the southeastern United States (Baker and Langdon, 1990). However, loblolly pine was conspicuously absent from virtually the entire Mississippi Valley Alluvial Plain during presettlement times. A map (Fig. 1) of the native distribution of loblolly from Baker and Langdon (1990) identifies 2 exceptions to this gap-a narrow strip of land (Macon Ridge) in northeastern Louisiana corresponding to Quaternary-period braided stream terraces left by the ancestral Arkansas River and a small pocket of braided stream terraces from the ancestral Missouri and Mississippi rivers in Arkansas (Saucier, 1974). Unlike Macon Ridge (a noticeably elevated landform), the Arkansas terraces are flat to very gently rolling plains subject to frequent, long-term and large-scale inundation (at least before modern drainage and flood control projects).

  • Citation: Bragg, Don C. 2005. Presettlement Pinus taeda in the Mississippi Valley Alluvial Plain of the Monroe County, Arkansas area. Journal of the Arkansas Academy of Science, Vol. 59: 187-195
  • Posted Date: October 30, 2006
  • Modified Date: July 23, 2007
  • Requesting Print Publications

    Publication requests are subject to availability. Fiscal responsibility limits the hardcopies of publications we produce and distribute. Electronic versions of publications may be downloaded, distributed and printed.

    Please make any requests at pubrequest@fs.fed.us.

    Publication Notes

    • This article was written and prepared by U.S. Government employees on official time, and is therefore in the public domain.
    • Our online publications are scanned and captured using Adobe Acrobat. During the capture process some typographical errors may occur. Please contact the SRS webmaster if you notice any errors which make this publication unusable.
    • To view this article, download the latest version of Adobe Acrobat Reader.