scholarly journals Geographic and temporal patterns of non-lethal attacks on humpback whales by killer whales in the eastern South Pacific and the Antarctic Peninsula

2018 ◽  
Vol 37 ◽  
pp. 207-218
Author(s):  
JJ Capella ◽  
F Félix ◽  
L Flórez-González ◽  
J Gibbons ◽  
B Haase ◽  
...  
2017 ◽  
Vol 45 (2) ◽  
pp. 253-260
Author(s):  
M. V. Reyes Reyes ◽  
S. Baumann-Pickering ◽  
A. Simonis ◽  
M. L. Melcón ◽  
J. Trickey ◽  
...  

2020 ◽  
pp. 95-99
Author(s):  
Judith Allen ◽  
Carole Carlson ◽  
Peter T. Stevick

The Antarctic Humpback Whale Catalogue (AHWC) is an international collaborative project investigating movement patterns of humpback whales in the Southern Ocean and corresponding lower latitude waters. The collection contains records contributed by 261 researchers and opportunistic sources. Photographs come from all of the Antarctic management areas, the feeding grounds in southern Chile and also most of the known or suspected low-latitude breeding areas and span more than two decades. This allows comparisons to be made over all of the major regions used by  Southern Hemisphere humpback whales. The fluke, left dorsal fin/flank and right dorsal fin/flank collections represent 3,655, 413 and 407 individual whales respectively. There were 194 individuals resighted in more than one year, and 82 individuals resighted in more than one region. Resightings document movement along the western coast of South America and movement between the Antarctic Peninsula and western coast of South America and Central America. A single individual from Brazil was resighted off South Georgia, representing the first documented link between the Brazilian breeding ground and any feeding area. A second individual from Brazil was resighted off Madagascar, documenting long distance movement of a female between non-adjacent breeding areas. Resightings also include two matches between American Samoa and the Antarctic Peninsula, documenting the first known feeding site for American Somoa and setting a new long distance seasonal migration record. Three matches between Sector V and eastern Australia support earlier evidence provided by Discovery tags. Multiple resightings of individuals in the Antarctic Peninsula during more than one season indicate that humpback whales in this area show some degree of regional feeding area fidelity. The AHWC provides a powerful non-lethal and non-invasive tool for investigating the movements and population structure of the whales utilising the Southern Ocean Sanctuary. Through this methodical, coordinated comparison and maintenance of collections from across the hemisphere, large-scale movement patterns may be examined, both within the Antarctic, and from the Antarctic to breeding grounds at low latitudes.


Oryx ◽  
1982 ◽  
Vol 16 (5) ◽  
pp. 430-430
Author(s):  
Peter Kinnear

Nigel Bonner has documented sightings of humpbacks Megaptera novaeangliae off the west coast of the Antarctic Peninsula which seem to indicate some recovery of stocks (Oryx 16, 3: 231–232). It may therefore be worth placing on record the following sightings of this species made from Argentine Islands for 1970/72, when I was stationed at the British Antarctic Survey base.


Polar Biology ◽  
2008 ◽  
Vol 31 (7) ◽  
pp. 771-781 ◽  
Author(s):  
L. Dalla Rosa ◽  
E. R. Secchi ◽  
Y. G. Maia ◽  
A. N. Zerbini ◽  
M. P. Heide-Jørgensen

2020 ◽  
pp. 275-282
Author(s):  
Claire Garrigue ◽  
Rochelle Constantine ◽  
Michael Poole ◽  
Nan Hauser ◽  
Phil Clapham ◽  
...  

The movement of individual humpback whales between regional breeding grounds of Oceania (South Pacific) was documented by individualidentification photographs collected from 1999 to 2004. Photographs were collected with comparable effort across the six years in four primaryisland breeding grounds: New Caledonia, Tonga (Vava’u) the Cook Islands and French Polynesia (Mo’orea and Rurutu); with smaller effort inadjacent regions: Vanuatu, Fiji, Samoa, Niue and American Samoa. Interchange among wintering grounds was assessed first with all usablephotographs included in each regional catalogue, representing 1,080 regional sightings (including within-region and between-region resightings)of 949 individual whales from Oceania. From this, 28 cases of movement between (mostly adjacent) regions were documented. Previouslyundocumented interchange was found between regions of central Oceania and the western South Pacific. No individual was sighted in more thantwo regions during this six-year period. The documented movement between regions was one-directional, except for one individual sighted first inFrench Polynesia, then in American Samoa and then back in French Polynesia (each in different years). Only one whale was resighted in more thanone region during the same winter season. No directional trend was apparent and movement between regions did not seem to be sex specific. Asystematic quality control review of all catalogues was then implemented to calculate standardised indices of within-region return and betweenregion interchange, resulting in a quality controlled catalogue of 776 regional sightings of 659 individuals. The standardised indices confirmed thatthe probability of between-region interchange was low, relative to within-region return, supporting the assumption of multiple management unitsor stocks in Oceania. The relative isolation of breeding regions and the movement of individuals across the longitudinal borders of Antarcticmanagement Areas V and VI has important implications for the allocation of historical catches from the Antarctic and therefore, for assessingcurrent levels of recovery for breeding stocks


2021 ◽  
Author(s):  
Holly Fearnbach ◽  
John W. Durban ◽  
David K. Ellifrit ◽  
Alyssa Paredes ◽  
Leigh S. Hickmott ◽  
...  

2021 ◽  
Author(s):  
James Brean ◽  
Manuel Dall’Osto ◽  
Rafel Simó ◽  
Zongbo Shi ◽  
David C. S. Beddows ◽  
...  

2021 ◽  
pp. 1-27
Author(s):  
H. Jay Zwally ◽  
John W. Robbins ◽  
Scott B. Luthcke ◽  
Bryant D. Loomis ◽  
Frédérique Rémy

Abstract GRACE and ICESat Antarctic mass-balance differences are resolved utilizing their dependencies on corrections for changes in mass and volume of the same underlying mantle material forced by ice-loading changes. Modeled gravimetry corrections are 5.22 times altimetry corrections over East Antarctica (EA) and 4.51 times over West Antarctica (WA), with inferred mantle densities 4.75 and 4.11 g cm−3. Derived sensitivities (Sg, Sa) to bedrock motion enable calculation of motion (δB0) needed to equalize GRACE and ICESat mass changes during 2003–08. For EA, δB0 is −2.2 mm a−1 subsidence with mass matching at 150 Gt a−1, inland WA is −3.5 mm a−1 at 66 Gt a−1, and coastal WA is only −0.35 mm a−1 at −95 Gt a−1. WA subsidence is attributed to low mantle viscosity with faster responses to post-LGM deglaciation and to ice growth during Holocene grounding-line readvance. EA subsidence is attributed to Holocene dynamic thickening. With Antarctic Peninsula loss of −26 Gt a−1, the Antarctic total gain is 95 ± 25 Gt a−1 during 2003–08, compared to 144 ± 61 Gt a−1 from ERS1/2 during 1992–2001. Beginning in 2009, large increases in coastal WA dynamic losses overcame long-term EA and inland WA gains bringing Antarctica close to balance at −12 ± 64 Gt a−1 by 2012–16.


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