scholarly journals Sediment Layers Pinpoint Periods of Climatic Change

Eos ◽  
2020 ◽  
Vol 101 ◽  
Author(s):  
Katherine Kornei

Researchers studying sediment cores from the Gulf of Alaska have pinpointed when the Cordilleran Ice Sheet, now extinct, disgorged icebergs into the Pacific Ocean.

Science ◽  
2020 ◽  
Vol 370 (6517) ◽  
pp. 716-720 ◽  
Author(s):  
Maureen H. Walczak ◽  
Alan C. Mix ◽  
Ellen A. Cowan ◽  
Stewart Fallon ◽  
L. Keith Fifield ◽  
...  

New radiocarbon and sedimentological results from the Gulf of Alaska document recurrent millennial-scale episodes of reorganized Pacific Ocean ventilation synchronous with rapid Cordilleran Ice Sheet discharge, indicating close coupling of ice-ocean dynamics spanning the past 42,000 years. Ventilation of the intermediate-depth North Pacific tracks strength of the Asian monsoon, supporting a role for moisture and heat transport from low latitudes in North Pacific paleoclimate. Changes in carbon-14 age of intermediate waters are in phase with peaks in Cordilleran ice-rafted debris delivery, and both consistently precede ice discharge events from the Laurentide Ice Sheet, known as Heinrich events. This timing precludes an Atlantic trigger for Cordilleran Ice Sheet retreat and instead implicates the Pacific as an early part of a cascade of dynamic climate events with global impact.


1980 ◽  
Vol 13 (3) ◽  
pp. 303-321 ◽  
Author(s):  
Robert M. Thorson

AbstractDuring the Vashon Stade of the Fraser Glaciation, about 15,000–13,000 yr B.P., a lobe of the Cordilleran Ice Sheet occupied the Puget lowland of western Washington. At its maximum extent about 14,000 yr ago, the ice sheet extended across the Puget lowland between the Cascade Range and Olympic Mountains and terminated about 80 km south of Seattle. Meltwater streams drained southwest to the Pacific Ocean and built broad outwash trains south of the ice margin. Reconstructed longitudinal profiles for the Puget lobe at its maximum extent are similar to the modern profile of Malaspina Glacier, Alaska, suggesting that the ice sheet may have been in a near-equilibrium state at the glacial maximum. Progressive northward retreat from the terminal zone was accompanied by the development of ice-marginal streams and proglacial lakes that drained southward during initial retreat, but northward during late Vashon time. Relatively rapid retreat of the Juan de Fuca lobe may have contributed to partial stagnation of the northwestern part of the Puget lobe. Final destruction of the Puget lobe occurred when the ice retreated north of Admiralty Inlet. The sea entered the Puget lowland at this time, allowing the deposition of glacial-marine sediments which now occur as high as 50 m altitude. These deposits, together with ice-marginal meltwater channels presumed to have formed above sea level during deglaciation, suggest that a significant amount of postglacial isostatic and(or) tectonic deformation has occurred in the Puget lowland since deglaciation.


Geology ◽  
2018 ◽  
Vol 46 (4) ◽  
pp. 307-310 ◽  
Author(s):  
Juliane Müller ◽  
Oscar Romero ◽  
Ellen A. Cowan ◽  
Erin L. McClymont ◽  
Matthias Forwick ◽  
...  

1969 ◽  
Vol 26 (7) ◽  
pp. 1955-1956 ◽  
Author(s):  
E. A. Best ◽  
Peter J. Eldridge

During August 1967, 12 specimens of Sebastodes rubrivinctus were collected from the Pacific Ocean off Amchitka Island, Alaska. This is a westward extension of their known range from the Gulf of Alaska.


1998 ◽  
Vol 15 (2) ◽  
pp. 67-83 ◽  
Author(s):  
Stephen P. Barnes ◽  
Samuel D. Bradbrook ◽  
Barry A. Cragg ◽  
Julian R. Marchesi ◽  
Andrew J. Weightman ◽  
...  

Zootaxa ◽  
2017 ◽  
Vol 4312 (2) ◽  
pp. 394 ◽  
Author(s):  
HELMUT LEHNERT ◽  
ROBERT P. STONE

A new species of Trichogypsiidae is described and compared to its congeners. Trichogypsia alaskensis n. sp. represents the fifth species of the family and with this record all three genera of the family are now represented in the North Pacific Ocean. Calcarea are rare in the Gulf of Alaska but with this new record the number of confirmed species rises from two to three. The new species has larger diactines of a broader size range and with a different pattern of spination than all congeners. 


2001 ◽  
Vol 28 (19) ◽  
pp. 3721-3724
Author(s):  
Cathy Stephens

Sign in / Sign up

Export Citation Format

Share Document