Whaling in the Antarctic (Australia v Japan: New Zealand Intervening)

2021 ◽  
Author(s):  
Andersen Elisabeth ◽  
Vöneky Silja
Keyword(s):  
New Zealand ◽  
The Antarctic

The search for an alternative strategy: New Zealand and the Antarctic

1983 ◽  
Vol 72 (288) ◽  
pp. 466-472 ◽  
Author(s):  
Laurie Barber ◽  
Michael Selby
Keyword(s):  
New Zealand ◽  
Alternative Strategy ◽  
The Antarctic

Mawson’s views on use of natural resources in the Antarctic and sub-Antarctic

Polar Record ◽  
2021 ◽  
Vol 57 ◽  
Author(s):  
Peter D. Shaughnessy ◽  
Mark Pharaoh
Keyword(s):  
New Zealand ◽  
Natural Resources ◽  
Historical Context ◽  
Wildlife Sanctuary ◽  
Elephant Seals ◽  
Macquarie Island ◽  
Antarctic Expedition ◽  
Southern Elephant Seals ◽  
Meteorological Observations ◽  
The Antarctic

Abstract Sir Douglas Mawson is a well-known Antarctic explorer and scientist. Early in his career, he recognised opportunities for commerce in Antarctic and sub-Antarctic regions. While at Cape Denison, Antarctica, in 1913 on the Australasian Antarctic Expedition (AAE), the Adelie Blizzard magazine was produced. Mawson contributed articles about Antarctic natural resources and their possible use. Later, he advocated Australia be involved in pelagic whaling. He collected seal skins and oil for their commercial value to be assessed by the Hudson’s Bay Company. During the AAE, Mawson visited Macquarie Island where an oiling gang was killing southern elephant seals and royal penguins. Mawson was concerned that they were over-exploited and lobbied successfully to stop the killing. His plans for Macquarie Island included a wildlife sanctuary, with a party to supervise access, send meteorological observations to Australia and New Zealand, and be self-funded by harvesting elephant seals and penguins. Macquarie Island was declared a sanctuary in 1933. Although Mawson has been recognised as an early proponent of conservation, his views on conservation of living natural resources were inconsistent. They should be placed in their historical context: in the early twentieth century, utilisation of living natural resources was viewed more favourably than currently.

New trigonioid bivalves from the Early Jurassic to earliest Cretaceous of the Antarctic Peninsula region: systematics and austral paleobiogeography

1995 ◽  
Vol 69 (1) ◽  
pp. 66-84 ◽  
Author(s):  
Simon R. A. Kelly
Keyword(s):  
New Zealand ◽  
Antarctic Peninsula ◽  
Southern Africa ◽  
Late Jurassic ◽  
Early Jurassic ◽  
South Shetland Islands ◽  
Shetland Islands ◽  
Livingston Island ◽  
History Of ◽  
The Antarctic

New discoveries of trigonioid bivalves are documented from three areas in the Antartic Peninsula: the Fossil Bluff Group of Alexander Island, the Latady Formation of the Orville Coast, and the Byers Group of Livingston Island, South Shetland Islands. Eleven taxa are described, representing six genera or subgenera. The faunas are characterized by genera including Vaugonia (Vaugonia), the first Early Jurassic trigonioid recognized on the continent; Vaugonia (V.) and V. (Orthotrigonia?) in the Late Jurassic; and Iotrigonia (Iotrigonia), Myophorella (Scaphogonia), and Pterotrigonia (Pterotrigonia), which span the Jurassic–Cretaceous boundary, reaching the Berriasian stage. The following species are new: Pterotrigonia (P.) cramei n. sp., Pterotrigonia (P.) thomsoni n. sp., Vaugonia (V.) orvillensis n. sp., and V. (Orthotrigonia?) quiltyi n. sp. The faunas show affinities with those of New Zealand and southern Africa. Trigonioids characterize the shallower marine biofacies in the Jurassic of the Antarctic and reflect the principal shallowing events in the history of the region.

Records of vagrant fur seals (family Otariidae) in South Australia

2014 ◽  
Vol 36 (2) ◽  
pp. 154 ◽  
Author(s):  
Peter D. Shaughnessy ◽  
Catherine M. Kemper ◽  
David Stemmer ◽  
Jane McKenzie
Keyword(s):  
New Zealand ◽  
South Australia ◽  
The South ◽  
South Indian Ocean ◽  
Fur Seals ◽  
South Indian ◽  
Fur Seal ◽  
New Zealand Fur Seal ◽  
The Antarctic ◽  
Subantarctic Fur Seals

Two fur seal species breed on the southern coast of Australia: the Australian fur seal (Arctocephalus pusillus doriferus) and the New Zealand fur seal (A. forsteri). Two other species are vagrants: the subantarctic fur seal (A. tropicalis) and the Antarctic fur seal (A. gazella). We document records of vagrant fur seals in South Australia from 1982 to 2012 based primarily on records from the South Australian Museum. There were 86 subantarctic fur seals: 49 specimens and 37 sightings. Most (77%) were recorded from July to October and 83% of all records were juveniles. All but two specimens were collected between July and November. Sightings were prevalent during the same period, but there were also nine sightings during summer (December–February), several of healthy-looking adults. Notable concentrations were near Victor Harbor, on Kangaroo Island and Eyre Peninsula. Likely sources of subantarctic fur seals seen in South Australia are Macquarie and Amsterdam Islands in the South Indian Ocean, ~2700 km south-east and 5200 km west of SA, respectively. There were two sightings of Antarctic fur seals, both of adults, on Kangaroo Island at New Zealand fur seal breeding colonies. Records of this species for continental Australia and nearby islands are infrequent.

Atmospheric CO2 concentrations and δ13C values across the Antarctic Circumpolar Current between New Zealand and Antarctica

Tellus B ◽  
2007 ◽  
Vol 59 (1) ◽  
pp. 130-137 ◽  
Author(s):  
Antonio Longinelli ◽  
Federico Giglio ◽  
Leonardo Langone ◽  
Renzo Lenaz ◽  
Carlo Ori ◽  
...  
Keyword(s):  
New Zealand ◽  
Antarctic Circumpolar Current ◽  
Atmospheric Co2 ◽  
Δ13c Values ◽  
Co2 Concentrations ◽  
Circumpolar Current ◽  
Atmospheric Co2 Concentrations ◽  
The Antarctic

Against all odds: the birth of the Commonwealth Trans-Antarctic Expedition, 1955–1958

Polar Record ◽  
2011 ◽  
Vol 49 (1) ◽  
pp. 50-61
Author(s):  
Stephen Hicks ◽  
Bryan Storey ◽  
Philippa Mein Smith
Keyword(s):  
New Zealand ◽  
The United States ◽  
Weddell Sea ◽  
Antarctic Expedition ◽  
Foreign Office ◽  
Polar Research Institute ◽  
Antarctic Continent ◽  
British Foreign Office ◽  
The Many ◽  
The Antarctic

ABSTRACTWhen the Commonwealth Trans-Antarctic Expedition 1955–1958 advance party sailed from the Millwall Docks in November 1955, bound for the Weddell Sea, their departure was the product of five years of intensive effort on the part of Vivian Fuchs to achieve the first overland crossing of the Antarctic continent. This paper investigates the many obstacles that had to be overcome leading up to Theron sailing and explains the manner in which they were overcome by the Fuchs-Wordie-Clifford triumvirate. The British Foreign Office was particularly opposed to the expedition with the office's focus on sovereignty rather than science while an alternative proposal from Duncan Carse raised a unique set of difficulties. The withdrawal from involvement by the Scott Polar Research Institute Director, Colin Bertram, indicated further disaffection. Most important, if political and financial goals were to be met, was the need for participation by several Commonwealth countries of which New Zealand was the essential partner. Fortunately, the vigorous efforts of a few Antarctic enthusiasts in New Zealand were successful in moving their government to assert its long dormant position in the Ross Dependency. New Zealand's commitment turned the tide of commonwealth apathy towards the TAE. Although the TAE preceded the IGY, events, including the dominating IGY presence of the United States, caused the two projects to become tightly interwoven. For these reasons the years leading up to the departure of Theron were as intriguing as the crossing journey itself.

Convention on the Regulation of Antarctic Mineral Resource Activities: a major addition to the Antarctic Treaty System

Polar Record ◽  
1989 ◽  
Vol 25 (152) ◽  
pp. 19-32 ◽  
Author(s):  
Peter J. Beck
Keyword(s):  
Mineral Resource ◽  
New Zealand ◽  
Future Development ◽  
Political Development ◽  
Significant Development ◽  
Antarctic Treaty ◽  
Key Terms ◽  
The Antarctic ◽  
Antarctic Environment ◽  
Antarctic Treaty System

AbstractIn June 1988, at the final session of the Fourth Special Antarctic Treaty Consultative Meeting in Wellington, New Zealand, the Convention on the Regulation of Antarctic Mineral Resource Activities (CRAMRA) was adopted, bringing to a successful conclusion six years of negotiations. Christopher Beeby, chairman of the discussions, presented the convention as the most important political development affecting Antarctica since the 1959 treaty, especially as it established the ability of the Antarctic Treaty System to reach an internal accommodation even upon matters raising serious political, legal, environmental and other issues. There remain uncertainties regarding the future development of the Antarctic minerals question; for example, when will the minerals convention and the proposed institutional framework come into effect, will its ratification encourage mining, can the fragile Antarctic environment be adequately protected against mining, how will certain key terms and concepts be defined, and will the regime's operation bring latent tensions to the surface? It is also difficult to predict how other governments will react to the convention, in the light of recent UN resolutions on Antarctica. The convention is perceived within the Antarctic Treaty system as a significant development, but it will be some time before a considered evaluation of the Antarctic Minerals Regime can be conducted.

Gyrothyris williamsi sp. nov. and inter-relationships of some taxa from waters around New Zealand and the southern oceans (Rhynchonelliformea: Terebratelloidea)

2007 ◽  
Vol 98 (3-4) ◽  
pp. 425-435 ◽  
Author(s):  
Maria Aleksandra Bitner ◽  
Bernard L. Cohen ◽  
Sarah. L. Long ◽  
Bertrand Richer de Forges ◽  
Michiko Saito
Keyword(s):  
New Zealand ◽  
Phylogenetic Analyses ◽  
Large Subunit ◽  
Phylogenetic Reconstruction ◽  
Sister Group ◽  
Last Common Ancestor ◽  
Rdna Sequences ◽  
Sw Pacific ◽  
Rates Of Evolution ◽  
The Antarctic

ABSTRACTThis paper describes a terebratelloid articulate brachiopod, Gyrothyris williamsi sp. nov., based on 95 specimens from seamounts on the Lord Howe Rise, Coral Sea, SW Pacific Ocean. The new species is attributed to Gyrothyris on the basis of (a) morphological and growth trajectory similarities; (b) phylogenetic analyses of an alignment of DNA sequence (∼2900-sites) obtained from nuclear-encoded small- and large-subunit ribosomal RNA genes (SSU and LSU); and (c) the presence of a distinctive, two-part deletion in the LSU gene. It is distinguished morphologically from Gyrothyris mawsoni and its subspecies by both internal and external morphology and by its isolated geographical distribution, which extends the patchy, known range of this genus to an area some 2000 km north of its previous northern limit around New Zealand. Phylogenetic analyses of the rDNAs and of mitochondrial cox1 gene sequences (663 sites) confirm previous indications that the New Zealand endemic terebratelloid genera form a clade (Neothyris (Calloria, Gyrothyris, Terebratella), but the position of Terebratella with respect to Calloria and Gyrothyris remains weakly established. These sequences disagree inexplicably about the closeness of the relationship between Neothyris parva and N. lenticularis. Analyses of the first sequences from Calloria variegata, a species restricted to the Hauraki Gulf, New Zealand, are consistent with the possibility that it originated locally, and recently, from C. inconspicua. Magellania venosa from S. America/Falklands joins with Antarctic Magellania fragilis and M. joubini to form an rDNA clade that excludes Terebratalia as the putative sister-group of the New Zealand terebratelloid clade. The cox1 (but not the rDNA) sequences of the New Zealand clade pass a test for clock-like rates of evolution, and maximum likelihood pairwise distances suggest that if genetic isolation between the ancestor of Antarctic Magellania and the last common ancestor of the New Zealand terebratelloid clade was initiated by separation of the Antarctic and New Zealand plates ∼90 Mya, isolation from M. venosa was initiated earlier, perhaps ∼145 Mya. However, in the simple phylogenetic reconstruction presented here from cox1 sequences, S. American and Antarctic Magellania spp. do not yield a well-supported clade, perhaps because of differences in base composition.

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