A multi-year time series of marine mammal distribution in the Alaskan Arctic

2016 ◽  
Vol 140 (4) ◽  
pp. 3359-3359 ◽  
Author(s):  
Jessica Crance ◽  
Catherine Berchok
Hydrobiologia ◽  
2011 ◽  
Vol 670 (1) ◽  
pp. 87-109 ◽  
Author(s):  
Evangelos Spyrakos ◽  
Tania C. Santos-Diniz ◽  
Gema Martinez-Iglesias ◽  
Jesus M. Torres-Palenzuela ◽  
Graham J. Pierce

2015 ◽  
Vol 136 ◽  
pp. 175-200 ◽  
Author(s):  
Kathy J. Kuletz ◽  
Megan C. Ferguson ◽  
Brendan Hurley ◽  
Adrian E. Gall ◽  
Elizabeth A. Labunski ◽  
...  

2014 ◽  
Vol 8 ◽  
Author(s):  
Cory JD Matthews ◽  
Steven H Ferguson

Isotopic time series from sequentially sampled growth layer groups (GLGs) in marine mammal teeth can be combined to build chronologies allowing assessment of isotopic variation in marine ecosystems. Synchronous recording of baseline isotopic variation across dentinal GLGs of species with temporal and spatial overlap in foraging offers a unique opportunity for validation of marine mammal age estimation procedures through calibration of GLG deposition rates in one species against another whose GLG deposition has been independently determined. In this study, we compare trends in stable carbon isotope ratios (d13C) across dentinal GLGs of three eastern Canadian Arctic (ECA) beluga (Delphinapterus leucas) populations through the 1960s-2000s with a d13C time series measured across dentinal GLGs of ECA/Northwest Atlantic killer whales (Orcinus orca) from 1944-1999. We use confirmed annual GLG deposition in killer whales as a means to assess beluga GLG deposition, and show linear d13C declines across chronologies of both species were statistically indistinguishable when based on annual GLG deposition in beluga whales, but differed when based on biannual deposition. We suggest d13C declines reflect the oceanic 13C Suess effect, and provide additional support for annual GLG deposition in beluga whales by comparing rates of d13C declines across beluga GLGs with published annual d13C declines attributed to the oceanic 13C Suess effect in the North Atlantic.


2017 ◽  
Vol 4 ◽  
Author(s):  
Gregory K. Silber ◽  
Matthew D. Lettrich ◽  
Peter O. Thomas ◽  
Jason D. Baker ◽  
Mark Baumgartner ◽  
...  

2019 ◽  
Vol 146 (4) ◽  
pp. 2886-2886
Author(s):  
Bruce Martin ◽  
Xavier Mouy ◽  
Briand Gaudet ◽  
Katie Kowarski
Keyword(s):  

2019 ◽  
Vol 146 (4) ◽  
pp. 2804-2804
Author(s):  
Ally Rice ◽  
Ana Širović ◽  
Jennifer Trickey ◽  
John Hildebrand ◽  
Simone Baumann-Pickering

2021 ◽  
Author(s):  
Misiani Zachary ◽  
Lun Yin ◽  
Mwai Zacharia ◽  
Antonine Sakwa ◽  
Xiaohan Zhang ◽  
...  

2013 ◽  
Vol 67 ◽  
pp. 116-126 ◽  
Author(s):  
Lisanne A.M. Aerts ◽  
Alexandra E. McFarland ◽  
Bridget H. Watts ◽  
Kate S. Lomac-MacNair ◽  
Pamela E. Seiser ◽  
...  

1994 ◽  
Vol 144 ◽  
pp. 279-282
Author(s):  
A. Antalová

AbstractThe occurrence of LDE-type flares in the last three cycles has been investigated. The Fourier analysis spectrum was calculated for the time series of the LDE-type flare occurrence during the 20-th, the 21-st and the rising part of the 22-nd cycle. LDE-type flares (Long Duration Events in SXR) are associated with the interplanetary protons (SEP and STIP as well), energized coronal archs and radio type IV emission. Generally, in all the cycles considered, LDE-type flares mainly originated during a 6-year interval of the respective cycle (2 years before and 4 years after the sunspot cycle maximum). The following significant periodicities were found:• in the 20-th cycle: 1.4, 2.1, 2.9, 4.0, 10.7 and 54.2 of month,• in the 21-st cycle: 1.2, 1.6, 2.8, 4.9, 7.8 and 44.5 of month,• in the 22-nd cycle, till March 1992: 1.4, 1.8, 2.4, 7.2, 8.7, 11.8 and 29.1 of month,• in all interval (1969-1992):a)the longer periodicities: 232.1, 121.1 (the dominant at 10.1 of year), 80.7, 61.9 and 25.6 of month,b)the shorter periodicities: 4.7, 5.0, 6.8, 7.9, 9.1, 15.8 and 20.4 of month.Fourier analysis of the LDE-type flare index (FI) yields significant peaks at 2.3 - 2.9 months and 4.2 - 4.9 months. These short periodicities correspond remarkably in the all three last solar cycles. The larger periodicities are different in respective cycles.


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