Only a few years ago most interested people thought (and many said in print) that accidental killing of Antarctic animals as a consequence of commercial fishing operations was minimal to non-existent. We now know that species in three major groups (fish, seals, seabirds) are seriously threatened by such incidental mortality.

The Antarctic continent and the peripheral ocean regions are the primary source of information on the Cenozoic cryosphere and events leading up to its development at least 36 million years ago. From a variety of data it is now apparent that the southern high latitudes have been subjected to a dynamic alternation of ice sheet expansion and decay through the late Palaeogene and Neogene. This history of climate change was accompanied by, and certainly strongly influenced by, significant vertical and horizontal lithosphere changes, including the evolution of major internal seaways and mountain ranges. The imprint of this record is preserved in the marine successions of the polar basins, in the world's bathyal and abyssal ocean basins and in the continental shelves of other continents, including those of the Northern Hemisphere. The Antarctic and extra-Antarctic terrestrial and marine data bases have developed separately in the past three decades and geospheric and biospheric information must now be integrated across latitudes. Future success in deciphering climate change depends on a better understanding of glacial–deglacial cycles from the point of view of both direct Antarctic and indirect or proxy extra-Antarctic data, through the complete temporal range of 107 to 103 years. Unfortunately, much of the high latitude record for the past 65 million years of earth history is presently veiled by thick ice sheets/ice shelves and deep and often ice-covered marine waters. Without the intensive application of the most advanced remote sampling equipment on the continent and in the Southern Ocean it will be difficult for this region to contribute significantly to global change and global climate programmes.

The diet of the emperor penguin Aptenodytes forsteri (Gray) in Amanda Bay, Princess Elizabeth Land, Antarctica, was studied by analysis of adult stomach contents during part of the chick-rearing period from August to October 1986. The penguins consumed almost entirely fish, mainly Pleuragramma antarcticum (Boulenger) (78% by number and 78% by mass). Other fish species, cephalopods and crustaceans were minor components. These results and those of the only other two, geographically distinct, quantitative studies of the diet of emperor penguins suggest that the diet of this species varies through the effects of local topography and hydrology on prey availability.

The dense High Salinity Shelf Water (HSSW) which spreads out below parts of the Ross Ice Shelf represents a heat-reservoir that can induce ablation if it comes into contact with the ice shelf base. One source of the mechanical energy necessary to lift the dense HSSW is small-scale turbulence induced by the shear of tidal currents at the sea-floor and at the ice shelf base. A one-dimensional Kraus-Turner-type model which is forced by a barotropic tidal current is coupled to the ice shelf by postulating that the ice-water interface is at the freezing point. The calculations indicate that the results of this two-layer approach allow a classification into a freezing and melting regime, depending strongly on the variability of the tidal currents with time and less on the intensity and the corresponding high production rate of turbulent kinetic energy. Based on an extended three-layer model ablation rates exceeding 0.4 m yr−1 are obtained in the south-eastern part of the Ross Ice Shelf. Advection processes in the mixed layer directly beneath the ice shelf base are not considered. These results can therefore be regarded as indicating the maximum amount of ablation occuring in the deeper reaches of the ice shelf cavity. Application of the three-layer model to the J9-area in the central Ross Ice Shelf indicate a tidally induced vertical heat flux of 1.8 W m−2 and a corresponding melting rate of 0.17 m yr−1. As supported by ice core measurements, however, an accumulation rate of 0.03–0.05 m yr−1 is estimated due to advection of freshwater produced immediately south of the J9-area.

Euphausiid life histories and distribution in the vicinity of South Georgia were studied from a series of samples taken in April 1980, November–December 1981, and July–August 1983. Size frequency data indicated a two-year life cycle for Euphausia frigida and the possibility of a three-year cycle for E. triacantha. The genus Thysanoessa was represented by a mixture of T. macrura and the dominant T. vicina. A one-year life cycle is proposed for the latter but that of the former is unknown. Spawning in E. frigida and to a lesser extent Thysanoessa spp. commenced as early as July and euphausiid calyptopes were a feature of the plankton for much of the year. E. superba eggs were found in low abundance over the shelf to the north of the island, but no hatched larvae were found. Behaviour patterns such as diurnal and seasonal migration partially confounded attempts to relate euphausiid distribution to environmental features. However calyptopes of most species, were generally more abundant in oceanic water deeper than 500 m and there was limited evidence that in August, E. frigida had commenced spawning in the colder part of the survey area.

At Radok Lake, northern Prince Charles Mountains, more than 2500 m of Permian Amery Group strata in the Beaver Lake graben are downfaulted against a Proterozoic metamorphic basement. An irregular blanket of late Cenozoic Pagodroma Tillite, up to 100 m thick, overlies the Permian strata and Proterozoic basement. The metamorphic basement comprises repeatedly deformed, high-grade felsic, mafic, aluminous and minor calc-silicate rocks derived from igneous and sedimentary precursors. Low- to medium-pressure granulite-facies metamorphism, assumed to be the ~1000 Ma event widely recorded in the East Antarctic Shield, was followed by incipient to moderate amphibolite-facies retrogression. Three folding events are recognized. Sporadic occurrences of pseudotachylite in the basement represent seismic faulting after substantial uplift and erosion. At the southern end of Radok Lake the Permian coarse alluvial fan facies, the Radok Conglomerate, is overlain disconformably by the Dart Fields Conglomerate, a basal member of the Bainmedart Coal Measures. Five kilometres along strike the deltaic Panorama Point beds, containing sideritic ironstone strata, are overlain conformably by arkosic sandstones of the basal Bainmedart Coal Measures. The Amery Group is intruded by two alnöite sills and at least five altered alkaline mafic dykes. The Pagodroma Tillite contains reworked marine microfossils and records the erosion of higher latitude Cenozoic marine sequences by an expanding ancestral Lambert Glacier.

Isolated fish remains including a tooth of the oldest described frilled shark, Chlamydoselachus thomsoni sp. nov. are described and figured from the Santa Marta Formation (Santonian–Campanian, Late Cretaceous) of James Ross Island, Antarctic Peninsula. Their geological and palaeoecological context is considered in the light of recent geological studies.

The regional geology and lithostratigraphy of the Late Cretaceous strata of north-east James Ross Island have been described by a number of authors (e.g. Olivero et al. 1986, Pirrie 1989). The aim of this short note is to describe a sequence of strata currently assigned to the Santa Marta Formation, and to reinterpret the processes and environments of deposition of this sequence.

An analysis is made of the climate of the Australian Antarctic station Mawson (67.6°S, 62.9°E) and its hinterland in the light of 30 years of observations and of previous investigations. Data are presented on free atmosphere temperature and wind structure, the synoptic meteorology of the region, solar radiation, surface temperature, sea ice, wind and weather. Emphasis is placed on the characteristics of the shallow south easterly katabatic winds averaging 11.1 m s−1 throughout the year and the frequent periods of intense gale associated with the effects of major Southern Ocean depressions. The climate of Mawson is believed to be typical of much of the coast of East Antarctica in regions where the ice-cap falls steeply to sea level.