1962
DOI: 10.1086/626809
|View full text |Cite
|
Sign up to set email alerts
|

Pleistocene Ice Volumes and Sea-Level Lowering

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1
1
1
1

Citation Types

0
38
0
2

Year Published

1966
1966
2020
2020

Publication Types

Select...
5
3
2

Relationship

0
10

Authors

Journals

citations
Cited by 118 publications
(40 citation statements)
references
References 12 publications
0
38
0
2
Order By: Relevance
“…The depth of · its outer edge varies between 80 and 140 meters, spanning the world average of 132 meters (Shepard, 1963, p. 257) and lying close to the estimate of 159 meters for the maximum lowering of sea level during Pleistocene glaciations (Donn, Farrand, and Ewing, 1962). Most of the area of the shelf is well below present wave base, which is about 20 meters, as estimated from the position at which waves begin to refract and transmit energy to the sea bottom.…”
Section: ?L"' Gktlumentioning
confidence: 55%
“…The depth of · its outer edge varies between 80 and 140 meters, spanning the world average of 132 meters (Shepard, 1963, p. 257) and lying close to the estimate of 159 meters for the maximum lowering of sea level during Pleistocene glaciations (Donn, Farrand, and Ewing, 1962). Most of the area of the shelf is well below present wave base, which is about 20 meters, as estimated from the position at which waves begin to refract and transmit energy to the sea bottom.…”
Section: ?L"' Gktlumentioning
confidence: 55%
“…During ice ages when global temperatures were 5 o C (9 o F) lower than today, much of the ocean's water was tied up in glaciers and sea level was often over one hundred meters (three hundred feet) lower than today (Donn et al, 1962;Kennett, 1982;Oldale, 1985). On the other hand, during the last interglacial period (100,000 years ago) when temperatures were about 1 o C (2 o F) warmer, sea level was approximately 6 meters (20 feet) higher than today (Mercer, 1970).…”
Section: Climate and Sea Levelmentioning
confidence: 99%
“…The greatest unionid diversity is found in ancient rivers with dynamic hydrogeological histories (Lydeard & Mayden, 1995;Neves et al, 1997). Many of these rivers have undergone reorganization during the cyclic glacial advances and retreats of the Pliocene and Pleistocene (e.g., Donn et al, 1962;Melhorn & Kempton, 1991) or experienced episodic tilt-block tectonics (e.g., Cox, 1994) during the Pleistocene and Early Holocene. These geologic events have profound evolutionary effects by restricting gene flow, causing allopatric speciation through vicariance, or creating opportunities for rapid radiations and secondary contact zones between onceisolated populations through stream-capture events (Roe et al, 2001;Kozak et al, 2006).…”
mentioning
confidence: 99%