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Geology topics

Kristen L. Cook

Publications and source records attributed to Kristen L. Cook.

2 recordsLinked to original sources

Establishing conservation benchmarks for threatened Bull Trout using spawner-recruitment relationships

Understanding the relationship between breeding adults and juvenile recruitment is fundamental to conserving at-risk species. Knowing whether recruitment is depensatory or compensatory at low adult abundances can aid in developing conservation strategies and recovery goals. However, this relationship requires long-term monitoring of two life stages, which can be costly and uncommon, especially for non-commercially harvested fish species, such as Bull Trout ( Salvelinus confluentus ). Listed as threatened in the United States and Canada, Bull Trout have declined throughout their range due to anthropogenic disturbances. Although spawner–recruitment relationships can create realistic recovery goals, this relationship is poorly characterized for Bull Trout. We used redd counts and juvenile densities from 11 Bull Trout populations to (1) establish spawner-recruitment dynamics, (2) assess environmental influences on productivity, and (3) derive recovery benchmarks. Bull Trout exhibited high recruitment productivity at low adult abundances and clear recruitment limitations at high abundances. Recruitment productivity varied across populations but was not associated with environmental covariates. We highlight strong compensatory capacity at low adult abundances, indicating possible recovery if limiting factors beyond spawning and rearing habitats are addressed.

Montana↗

A rockslide-generated tsunami in a Greenland fjord rang Earth for 9 days

Climate change is increasingly predisposing polar regions to large landslides. Tsunamigenic landslides have occurred recently in Greenland (Kalaallit Nunaat), but none have been reported from the eastern fjords. In September 2023, we detected the start of a 9-day-long, global 10.88-millihertz (92-second) monochromatic very-long-period (VLP) seismic signal, originating from East Greenland. In this study, we demonstrate how this event started with a glacial thinning–induced rock-ice avalanche of 25 × 106 cubic meters plunging into Dickson Fjord, triggering a 200-meter-high tsunami. Simulations show that the tsunami stabilized into a 7-meter-high long-duration seiche with a frequency (11.45 millihertz) and slow amplitude decay that were nearly identical to the seismic signal. An oscillating, fjord-transverse single force with a maximum amplitude of 5 × 1011 newtons reproduced the seismic amplitudes and their radiation pattern relative to the fjord, demonstrating how a seiche directly caused the 9-day-long seismic signal. Our findings highlight how climate change is causing cascading, hazardous feedbacks between the cryosphere, hydrosphere, and lithosphere.

Science↗