Metals and organochlorines in sperm whales (Physeter macrocephalus) stranded around the North Sea during the 1994/1995 winter

1996 ◽  
Vol 32 (1) ◽  
pp. 72-77 ◽  
Author(s):  
R.J. Law ◽  
R.L. Stringer ◽  
C.R. Allchin ◽  
B.R. Jones
2016 ◽  
Vol 42 (1) ◽  
pp. 35-41 ◽  
Author(s):  
Mette S. Hansen ◽  
Aage K. O. Alstrup ◽  
Jørgen H. Hansen ◽  
Mohammad N. S. Al-Sabi ◽  
Bettina Nonnemann ◽  
...  

1999 ◽  
Vol 183 ◽  
pp. 281-294 ◽  
Author(s):  
MB Santos ◽  
GJ Pierce ◽  
PR Boyle ◽  
RJ Reid ◽  
HM Ross ◽  
...  

2018 ◽  
Vol 88 ◽  
pp. 156-160 ◽  
Author(s):  
Marijke Autenrieth ◽  
Anja Ernst ◽  
Rob Deaville ◽  
Fabien Demaret ◽  
Lonneke L. IJsseldijk ◽  
...  

Author(s):  
Apolline ALFSEN ◽  
Mark BOSSELAERS ◽  
Olivier LAMBERT

In spite of a continuously expanding physeteroid fossil record, our understanding of the origin and early radiation of the two modern sperm whale families Kogiidae Gill, 1871 (including the pygmy and dwarf sperm whales, Kogia spp.) and Physeteridae Gray, 1821 (including the great sperm whale, Physeter Linnaeus, 1758) remains limited, especially due to the poorly resolved phylogenetic relationships of a number of extinct species. Among those, based on fragmentary cranial material from the late early to middle Miocene of Antwerp (Belgium, North Sea basin), the small-sized Thalassocetus antwerpiensis Abel, 1905 has been recognized for some time as the earliest branching kogiid. The discovery of a new diminutive physeteroid cranium from the late Miocene (Tortonian) of Antwerp leads to the description and comparison of a close relative of T. antwerpiensis. Thanks to the relatively young ontogenetic stage of this new specimen, the highly modified plate-like bones making the floor of its supracranial basin could be individually removed, a fact that greatly helped deciphering their identity and geometry. Close morphological similarities with T. antwerpiensis allow for the reassessment of several facial structures in the latter; the most important reinterpretation is the one of a crest-like structure, previously identified as a sagittal facial crest, typical for kogiids, and here revised as the left posterolateral wall of the supracranial basin, comprised of the left nasal (lost in kogiids for which the postnarial region is known) and the left maxilla. Implemented in a phylogenetic analysis, the new anatomical interpretations result in the new Belgian specimen and T. antwerpiensis being recovered as sister-groups in the family Physeteridae. Consequently, the geologically oldest kogiids are now dated from the Tortonian, further extending the ghost lineage separating these early late Miocene kogiid records from the estimated latest Oligocene to earliest Miocene divergence of kogiids and physeterids.


PLoS ONE ◽  
2018 ◽  
Vol 13 (8) ◽  
pp. e0201221 ◽  
Author(s):  
Lonneke L. IJsseldijk ◽  
Abbo van Neer ◽  
Rob Deaville ◽  
Lineke Begeman ◽  
Marco van de Bildt ◽  
...  

2016 ◽  
Vol 112 (1-2) ◽  
pp. 134-141 ◽  
Author(s):  
Bianca Unger ◽  
Elisa L. Bravo Rebolledo ◽  
Rob Deaville ◽  
Andrea Gröne ◽  
Lonneke L. IJsseldijk ◽  
...  

2017 ◽  
Vol 17 (4) ◽  
pp. 336-344 ◽  
Author(s):  
Klaus Heinrich Vanselow ◽  
Sven Jacobsen ◽  
Chris Hall ◽  
Stefan Garthe

AbstractThe Earth's atmosphere and the Earth's magnetic field protects local life by shielding us against Solar particle flows, just like the sun's magnetic field deflects cosmic particle radiation. Generally, magnetic fields can affect terrestrial life such as migrating animals. Thus, terrestrial life is connected to astronomical interrelations between different magnetic fields, particle flows and radiation. Mass strandings of whales have often been documented, but their causes and underlying mechanisms remain unclear. We investigated the possible reasons for this phenomenon based on a series of strandings of 29 male, mostly bachelor, sperm whales (Physeter macrocephalus) in the southern North Sea in early 2016. Whales’ magnetic sense may play an important role in orientation and migration, and strandings may thus be triggered by geomagnetic storms. This approach is supported by the following: (1) disruptions of the Earth's magnetic field by Solar storms can last about 1 day and lead to short-term magnetic latitude changes corresponding to shifts of up to 460 km; (2) many of these disruptions are of a similar magnitude to more permanent geomagnetic anomalies; (3) geomagnetic anomalies in the area north of the North Sea are 50–150 km in diameter; and (4) sperm whales swim about 100 km day−1, and may thus be unable to distinguish between these phenomena. Sperm whales spend their early, non-breeding years in lower latitudes, where magnetic disruptions by the sun are weak and thus lack experience of this phenomenon. ‘Naïve’ whales may therefore become disoriented in the southern Norwegian Sea as a result of failing to adopt alternative navigation systems in time and becoming stranded in the shallow North Sea.


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