1954
DOI: 10.2307/1931109
|View full text |Cite
|
Sign up to set email alerts
|

Some Lower Mississippi Valley Flood Plain Biotic Communities: Their age and Elevation

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1
1
1
1

Citation Types

1
46
0

Year Published

1985
1985
2016
2016

Publication Types

Select...
5
4

Relationship

0
9

Authors

Journals

citations
Cited by 81 publications
(49 citation statements)
references
References 8 publications
1
46
0
Order By: Relevance
“…Shelford, 1954;Barnes, 1978;Menges and Waller, 1983; Hupp and Osterkamp, 1985; Lyon and Sagers, 1998). Elevation affects the frequency and duration of inundation and may influence the likelihood of bed load movement, the latter depending additionally on particle size and shape.…”
Section: Geomorphological Controls On Vegetation Compositionmentioning
confidence: 99%
“…Shelford, 1954;Barnes, 1978;Menges and Waller, 1983; Hupp and Osterkamp, 1985; Lyon and Sagers, 1998). Elevation affects the frequency and duration of inundation and may influence the likelihood of bed load movement, the latter depending additionally on particle size and shape.…”
Section: Geomorphological Controls On Vegetation Compositionmentioning
confidence: 99%
“…The capacity of A. maritima to thrive in severe environments would make it extremely well suited for primary forest succession (Ugolini 1968;Chapin et al 1994) but less competitive during secondary succession, when soil nutrients or soil moisture are less prohibitive of other species (Connell and Slatyer 1977). The present rarity of A. maritima might best be explained by its specialized and narrow realized niche and by the absence of opportunities to serve its role in primary forest succession within its range over the last 10,000 yr. During the late Pleistocene Epoch, successive episodes of glacial progression and recession and numerous episodes of widespread sediment deposition and subsequent erosion, especially in the Mississippi River drainage basin (Esling and Halberg 1985;Hajic 1985;Lively and Alexander 1985), would have provided extensive and continuous opportunities for colonization of A. maritima on wet, disturbed sites in full sunlight (Shelford 1954;Ugolini 1968;Bedinger 1978;Chapin et al 1994). With the retreat of the last great glacier (the Wisconsin ice sheet), the resumption of drainage of the Great Lakes via the St. Lawrence River, and the opening of the outlet channel for Glacial Lake Agassiz to the northeast about 10,000 yr ago, the Mississippi River basin and many other watersheds of central and eastern North America have experienced a long period of relative stability (Delcourt and Delcourt 1993;Saucier 1994).…”
Section: Ecologymentioning
confidence: 99%
“…Sediment deposition usually increases the terrestrialization rate not only through increasing aggradation, but also through eutrophication, as suspended sediment is usually nutrient-rich (Shelford 1954, Peck and Smart 1986, Bhowmik and Adams 1989, Sparks et al 1990). Plants do not succeed if they are unable to tolerate these submersion periods (primarily helophytes and hydrophytes with low reserves and growth rates; van der Valk and Bliss 1971, Hamel and Bhe Âreur 1982, Brock et al 1987, Sparks et al 1990, van den Brink et al 1995.…”
Section: The Erosional±depositional Environment and Equilibriummentioning
confidence: 99%