Cephalopods as prey. III. Cetaceans

1996 ◽  
Vol 351 (1343) ◽  
pp. 1053-1065 ◽  

Over 80 % of odontocete species and two balaen whale species include cephalopods in their diet regularly. In 28 odontocetes they comprise the main food. Predominently cephalopod-eating species are found in the Physeteridae, Ziphiidae, Phocaenidae and Delphinidae. By far the most important of the 28 families of cephalopods represented in the diet of cetaceans are the oceanic Ommastrephidae, Histioteuthidae and the Cranchiidae, with the neritic Loliginidae assuming most importance on the continental shelves. Onychoteuthidae and Gonatidae assume greater importance in polar regions and the North Pacific. The other 22 families form a reservoir from which various cetaceans eat opportunistically and as their sizes permit. There are probably less than 60 cephalopod species regularly in the diet of cetaceans. Species composition of the food varies regionally, seasonally and annually. Locally, the greatest difference is found between cetaceans that live in oceanic water and continental shelf water. There is a positive correlation between the size of the prey and both the size of pelagic feeding cetacean species and the growth stage within a species. This leads to some partitioning of the food and less competition. Broad estimates show that the biomass of oceanic cephalopods consumed annually by the largest odontocete, Physeter catodon , may be over twice the biomass of fish caught by man. Regional estimates show that consumption by cetaceans of little known cephalopod species may greatly exceed the local catches of commercial fish.

Science ◽  
2019 ◽  
Vol 364 (6438) ◽  
pp. 386-389 ◽  
Author(s):  
Emma R. Kast ◽  
Daniel A. Stolper ◽  
Alexandra Auderset ◽  
John A. Higgins ◽  
Haojia Ren ◽  
...  

The million-year variability of the marine nitrogen cycle is poorly understood. Before 57 million years (Ma) ago, the 15N/14N ratio (δ15N) of foraminifera shell-bound organic matter from three sediment cores was high, indicating expanded water column suboxia and denitrification. Between 57 and 50 Ma ago, δ15N declined by 13 to 16 per mil in the North Pacific and by 3 to 8 per mil in the Atlantic. The decline preceded global cooling and appears to have coincided with the early stages of the Asia-India collision. Warm, salty intermediate-depth water forming along the Tethys Sea margins may have caused the expanded suboxia, ending with the collision. From 50 to 35 Ma ago, δ15N was lower than modern values, suggesting widespread sedimentary denitrification on broad continental shelves. δ15N rose at 35 Ma ago, as ice sheets grew, sea level fell, and continental shelves narrowed.


2009 ◽  
Vol 66 (7) ◽  
pp. 1633-1639 ◽  
Author(s):  
Diana L. Stram ◽  
Diana C. K. Evans

Abstract Stram, D. L., and Evans, D. C. K. 2009. Fishery management responses to climate change in the North Pacific. – ICES Journal of Marine Science, 66: 1633–1639. In the North Pacific, warming trends, coupled with declining sea ice, raise concerns about the effects of climate change on fish populations and ecosystem dynamics. Scientists are only beginning to understand the potential feedback mechanisms that will affect everything from plankton populations to major commercial fish species distributions, yet fishery managers have a responsibility to prepare for and respond to changing fishing patterns and potential ecosystem effects. There are ways for fishery managers to be proactive, while waiting for better information to unfold. The North Pacific Fishery Management Council (Council) and the National Marine Fisheries Service have jurisdiction over offshore fisheries in Alaska, USA. Recently, the Council has undertaken risk-averse management actions, in light of uncertainty about the effects of warming trends (and loss of sea ice) and resulting changes to fishing activities in the North Pacific. The Council has assessed whether opportunities for unregulated fishing could result from changes in fish distribution, has closed the Arctic Ocean to all commercial fishing pending further research, and has established extensive area closures where fishing with bottom-trawl gear is prohibited to protect vulnerable crab habitat and to control the northern expansion of the trawl fleet into newly ice-free waters. In cases where linkages between climate variables and fish distributions can be identified, the Council is developing adaptive management measures to respond to varying distributions of fish and shellfish. Finally, the Council has also tried to re-examine existing information to gain a better understanding of climate and ecosystem effects on fishery management. The pilot Fishery Ecosystem Plan for the Aleutian Islands maps interactions among climate factors and ecosystem components and suggests indicators for the Council to monitor.


2019 ◽  
Vol 617-618 ◽  
pp. 221-244 ◽  
Author(s):  
MR Baker ◽  
ME Matta ◽  
M Beaulieu ◽  
N Paris ◽  
S Huber ◽  
...  

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