Habitat Separation by the Amphipods Pontoporeia Affinis and P. femorata near Prudhoe Bay, Alaska

Oikos ◽  
1982 ◽  
Vol 39 (1) ◽  
pp. 77 ◽  
Author(s):  
M. Busdosh ◽  
Donald M. LaVigne ◽  
Gordon A. Robilliard
2007 ◽  
Author(s):  
Jennifer Yvonne Julian ◽  
Kirk Charles Forcade ◽  
Taylor L. West ◽  
Kevin yeager ◽  
Robert Lee Mielke ◽  
...  

Author(s):  
Annie Jonsson

AbstractMost animal species have a complex life cycle (CLC) with metamorphosis. It is thus of interest to examine possible benefits of such life histories. The prevailing view is that CLC represents an adaptation for genetic decoupling of juvenile and adult traits, thereby allowing life stages to respond independently to different selective forces. Here I propose an additional potential advantage of CLCs that is, decreased variance in population growth rate due to habitat separation of life stages. Habitat separation of pre- and post-metamorphic stages means that the stages will experience different regimes of environmental variability. This is in contrast to species with simple life cycles (SLC) whose life stages often occupy one and the same habitat. The correlation in the fluctuations of the vital rates of life stages is therefore likely to be weaker in complex than in simple life cycles. By a theoretical framework using an analytical approach, I have (1) derived the relative advantage, in terms of long-run growth rate, of CLC over SLC phenotypes for a broad spectrum of life histories, and (2) explored which life histories that benefit most by a CLC, that is avoid correlation in vital rates between life stages. The direction and magnitude of gain depended on life history type and fluctuating vital rate. One implication of our study is that species with CLCs should, on average, be more robust to increased environmental variability caused by global warming than species with SLCs.


1985 ◽  
Vol 37 (06) ◽  
pp. 1010-1018 ◽  
Author(s):  
T.N. Tyler ◽  
R.R. Metzger ◽  
L.R. Twyford
Keyword(s):  

2009 ◽  
Vol 12 (01) ◽  
pp. 25-32 ◽  
Author(s):  
Manmath Panda ◽  
James G. Ambrose ◽  
Gilbert Beuhler ◽  
Patrick L. McGguire
Keyword(s):  

2007 ◽  
Author(s):  
Jennifer Yvonne Julian ◽  
Janet Sack ◽  
Joel E. Johns
Keyword(s):  

1977 ◽  
Vol 19 (81) ◽  
pp. 533-546 ◽  
Author(s):  
W. F. Weeks ◽  
A. Kovacs ◽  
S. J. Mock ◽  
W. B. Tucker ◽  
W. D. Hibler ◽  
...  

Abstract During March-May 1976, a combination of laser and radar ranging systems was used to study the motion of both the fast ice and the pack ice near Narwhal and Cross Islands, two barrier islands located 16 and 21 km offshore in the vicinity of Prudhoe Bay, Alaska. Laser measurements of targets on the fast ice near Narwhal Island indicate small net displacements of approximately 1 m over the period of study (71 d) with short-term displacements of up to 40 cm occurring over 3 d periods. The main motion was outward normal to the coast and was believed to be the result of thermal expansion of the ice. The radar records of fast-ice sites farther offshore show a systematic increase in the standard deviation of the displacements as measured parallel to the coast, reaching a value of ±6.6 m at 31 km. The farthest fast-ice sites show short-term displacements of up to 12 m. There are also trends in the records that are believed to be the result of the general warming of the fast ice with time. Radar targets located on the pack ice showed large short-term displacements (up to 2.7 km) but negligible net ice drift along the coast. There was no significant correlation between the movement of the pack and the local wind, suggesting that coastal ice prediction models can only succeed if handled as part of a regional model which incorporates stress transfer through the pack. The apparent fast-ice-pack-ice boundary in the study area was located in 30-35 m of water.


1985 ◽  
Author(s):  
H.H. Haldorsen ◽  
C.A. Rego ◽  
D.M. Change ◽  
H.J. Mayson ◽  
D.M. Creveling

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