scholarly journals Vascular plant extinction in the continental United States and Canada

Author(s):  
Wesley M. Knapp ◽  
Anne Frances ◽  
Reed Noss ◽  
Robert F. C. Naczi ◽  
Alan Weakley ◽  
...  
2012 ◽  
Vol 110 (8) ◽  
pp. 1623-1629 ◽  
Author(s):  
Chengke Bai ◽  
William S. Alverson ◽  
Aaron Follansbee ◽  
Donald M. Waller

Science ◽  
1963 ◽  
Vol 142 (3598) ◽  
pp. 1483-1484 ◽  
Author(s):  
W. H. Wagner ◽  
A. J. Sharp

2019 ◽  
Vol 13 (1) ◽  
pp. 319-348
Author(s):  
Kevin D. Philley

The state of Mississippi is one of the least botanically explored areas in the eastern United States. A floristic survey of Choctaw County, Mississippi, was conducted from November 2009 through November 2017 in order to document the vascular flora and describe its plant communities. The county is located in the central portion of the state within the North Central Plateau physiographic region, an area dominated by dissected uplands with acidic to circumneutral sandy-clay soils. Three major river basins occur in the county, including the Big Black River, Noxubee River, and Pearl River. A total of 950 vascular plant species (958 taxa including varieties, subspecies, and recognized hybrids) was recorded. Three-hundred thirteen of these taxa were new county records. Twenty-eight species of special concern as designated by the Mississippi Natural Heritage Program were documented. Approximately 15 percent of the flora is considered non-native to the United States. Eight primary plant communities are also described.


2017 ◽  
Vol 11 (1) ◽  
pp. 117-120
Author(s):  
Kathryn Mauz

Botanist Cyrus G. Pringle collected plants in the western United States and northwestern Mexico between 1881 and 1884, and distributed his specimens as ‘Flora of the Pacific Slope’. The majority of the vascular plant type collections resulting from that work have been discussed elsewhere. This note addresses type status for five additional names that were previously overlooked in Pringle’s catalogue for Arizona and California.


Author(s):  
John M. Wehrung ◽  
Richard J. Harniman

Water tables in aquifer regions of the southwest United States are dropping off at a rate which is greater than can be replaced by natural means. It is estimated that by 1985 wells will run dry in this region unless adequate artificial recharging can be accomplished. Recharging with surface water is limited by the plugging of permeable rock formations underground by clay particles and organic debris.A controlled study was initiated in which sand grains were used as the rock formation and water with known clay concentrations as the recharge media. The plugging mechanism was investigated by direct observation in the SEM of frozen hydrated sand samples from selected depths.


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