scholarly journals Squareflower, Paronychia erecta

EDIS ◽  
2018 ◽  
Vol 2018 (5) ◽  
Author(s):  
Debbie Miller ◽  
Mack Thetford ◽  
Chris Verlinde ◽  
Gabriel Campbell ◽  
Ashlynn Smith

Squareflower is found in beach dunes, coastal grasslands, and scrub. This plant is an endemic restricted to the coastal Panhandle of Florida, counties west of the Big Bend region, and west to Louisiana. The square outline of the inflorescence is unique and makes squareflower a desirable plant for coastal landscapes.https://edis.ifas.ufl.edu/sg179 This publication is derived from information in SGEB-75/SG156, Dune Restoration and Enhancement for the Florida Panhandle, by Debbie Miller, Mack Thetford, Christina Verlinde, Gabriel Campbell, and Ashlynn Smith. https://edis.ifas.ufl.edu/sg156.

EDIS ◽  
2018 ◽  
Vol 2018 (5) ◽  
Author(s):  
Debbie Miller ◽  
Mack Thetford ◽  
Chris Verlinde ◽  
Gabriel Campbell ◽  
Ashlynn Smith

Coastal groundcherry occurs on beach dunes, coastal grasslands, coastal scrub, and disturbed areas. This plantis found throughout coastal counties on the west coast of Florida—except for the Big Bend region and the extreme southeasternmost counties—and more broadly west to Louisiana. Threatened and endangered beach mice and many other animals rely on this plant as a food source. Plants can be longed-lived and form relatively thick tuberous roots. Coastal groundcherry can hybridize with other Physalis species, particularly with P. viscosa, and has long frustrated plant taxonomists because of the inherent variation within the genus (Sullivan 1985).https://edis.ifas.ufl.edu/sg180 This publication is derived from information in SGEB-75/SG156, Dune Restoration and Enhancement for the Florida Panhandle, by Debbie Miller, Mack Thetford, Christina Verlinde, Gabriel Campbell, and Ashlynn Smith. https://edis.ifas.ufl.edu/sg156.


EDIS ◽  
2018 ◽  
Vol 2018 (5) ◽  
Author(s):  
Debbie Miller ◽  
Mack Thetford ◽  
Chris Verlinde ◽  
Gabriel Campbell ◽  
Ashlynn Smith

Seacoast marshelder is an important plant for dune restoration, stabilization, and formation because of itsability to trap sand. It grows on foredunes and forms low, rounded dunes as sand accumulates (Craig 1991). As the aboveground portions of the plant become buried by sand, rooting is stimulated in stem tissue (Craig 1975). This gives the appearance that the plant is rhizomatous when in fact it is the sand burial resulting in the presence of below-ground stems. This plant occurs throughout coastal Florida (except for the Big Bend coast) and in coastal southeastern states west to Texas and northeast to Virginia.https://edis.ifas.ufl.edu/sg174 This publication is derived from information in SGEB-75/SG156, Dune Restoration and Enhancement for the Florida Panhandle, by Debbie Miller, Mack Thetford, Christina Verlinde, Gabriel Campbell, and Ashlynn Smith. https://edis.ifas.ufl.edu/sg156.


EDIS ◽  
2018 ◽  
Vol 2018 (5) ◽  
Author(s):  
Debbie Miller ◽  
Mack Thetford ◽  
Chris Verlinde ◽  
Gabriel Campbell ◽  
Ashlynn Smith

Bitter panicgrass is important in dune stabilization and building and often grows intermixed with sea oats onforedunes. It is also found spread throughout back dunes, interdunal swales, and coastal grasslands. This plantoccurs throughout coastal Florida, except for the Big Bend coast, west to New Mexico, and along coastal northeast states to Massachusetts. A significant proportion of bitter panicgrass reproduction is by vegetative spread; its seeds are often sterile.https://edis.ifas.ufl.edu/sg178 This publication is derived from information in SGEB-75/SG156, Dune Restoration and Enhancement for the Florida Panhandle, by Debbie Miller, Mack Thetford, Christina Verlinde, Gabriel Campbell, and Ashlynn Smith. https://edis.ifas.ufl.edu/sg156.


2011 ◽  
Vol 70 (4) ◽  
pp. 573-576
Author(s):  
Frederick B. Stangl Jr ◽  
Dana R. Mills ◽  
Michael W. Haiduk
Keyword(s):  
Big Bend ◽  

1997 ◽  
Vol 17 (11) ◽  
pp. 1297-1319 ◽  
Author(s):  
GEORGES L WEATHERLY ◽  
DAVID THISTLE
Keyword(s):  
Big Bend ◽  

2020 ◽  
Vol 103 (12) ◽  
pp. 1471-1480
Author(s):  
Seiji Miyazono ◽  
Allison A. Pease ◽  
Sarah Fritts ◽  
Timothy B. Grabowski

2014 ◽  
Vol 13 ◽  
pp. 101-102
Author(s):  
Katherine E. Cummings ◽  
Michal Kowalewski ◽  
Savanna Barry ◽  
Thomas K. Frazer

1944 ◽  
Vol 76 (1) ◽  
pp. 11-18 ◽  
Author(s):  
E. R. Tinkham

This is one of a series of papers on the insect life of the Big Bend Region of Trans-Pecos, Texas, in which the author plans to present a fairly complete picture of the insect and animal life of that little known region. The area is composed of Presidio and Jeff Davis Counties, the former mainly Lower Sonoran in its faunal affinities, the latter principally Upper Sonoran and partly Transitional. Each county has its own mountain system; Presidio County the Chinati Mountains and Jeff Davis County the Davis Range. The Chinatis are desert mountains; the Davis are forested with oaks and pines.


1936 ◽  
Vol 1 (3) ◽  
pp. 215-219 ◽  
Author(s):  
E. F. Wood

Trait manifestations for the Hopewellian, or according to the more recently accepted terminology, the Central Basin cultural phase, have for several years been known to exist in eastern Wisconsin, but the occurrence of this phase with a residentiary cultural group in the eastern part of the state has had no positive indication until recently when a typical Central Basin mound burial was discovered in the Big Bend region of Waukesha County.The burial was partially unearthed by Mr. Henry J. Peterson while grading a portion of his land fronting on the south bank of Fox River in the N.W. ¼ of the N.W. ¼ of Section 25, Vernon Township. Mr. Peterson immediately notified the Milwaukee Public Museum of his find and kindly invited members of the staff to investigate the site. Mr. Peterson should here be commended for his foresight which made possible the gathering and preservation of data which otherwise might have been lost forever.


2017 ◽  
Vol 67 (4) ◽  
pp. 547-565 ◽  
Author(s):  
Dee Ann Cooper ◽  
Roger W. Cooper ◽  
James B. Stevens ◽  
M.S. Stevens ◽  
William A. Cobban ◽  
...  

Abstract The upper lower Cenomanian through middle Santonian (Upper Cretaceous) of the Boquillas Formation in the Big Bend Region of Trans-Pecos Texas consists of a marine carbonate succession deposited at the southern end of the Western Interior Seaway. The Boquillas Formation, subdivided into the lower, c. 78 m thick limestone-shale Ernst Member, and the upper, c. 132 m thick limestone/chalk/marl San Vicente Member, was deposited in a shallow shelf open marine environment at the junction between the Western Interior Seaway and the western margins of the Tethys Basin. Biogeographically, the area was closely tied with the southern Western Interior Seaway. The richly fossiliferous upper Turonian, Coniacian and lower Santonian parts of the Boquillas Formation are particularly promising for multistratigraphic studies.


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