scholarly journals The seasonal cycle of ocean-atmosphere CO2flux in Ryder Bay, west Antarctic Peninsula

2015 ◽  
Vol 42 (8) ◽  
pp. 2934-2942 ◽  
Author(s):  
Oliver J. Legge ◽  
Dorothee C. E. Bakker ◽  
Martin T. Johnson ◽  
Michael P. Meredith ◽  
Hugh J. Venables ◽  
...  
Keyword(s):  
Antarctic Peninsula ◽  
Seasonal Cycle ◽  
West Antarctic ◽  
Ocean Atmosphere ◽  
West Antarctic Peninsula

scholarly journals The seasonal cycle of carbonate system processes in Ryder Bay, West Antarctic Peninsula

2017 ◽  
Vol 139 ◽  
pp. 167-180 ◽  
Author(s):  
Oliver J. Legge ◽  
Dorothee C.E. Bakker ◽  
Michael P. Meredith ◽  
Hugh J. Venables ◽  
Peter J. Brown ◽  
...  
Keyword(s):  
Antarctic Peninsula ◽  
Seasonal Cycle ◽  
Carbonate System ◽  
West Antarctic ◽  
West Antarctic Peninsula

The role of fish in the Antarctic marine food web: differences between inshore and offshore waters in the southern Scotia Arc and west Antarctic Peninsula

2002 ◽  
Vol 14 (4) ◽  
pp. 293-309 ◽  
Author(s):  
ESTEBAN BARRERA-ORO
Keyword(s):  
Food Web ◽  
Antarctic Peninsula ◽  
Demersal Fish ◽  
Pelagic Fish ◽  
West Antarctic ◽  
Antarctic Marine ◽  
Scotia Arc ◽  
West Antarctic Peninsula ◽  
The Antarctic

The role of fish in the Antarctic food web in inshore and offshore waters is analysed, taking as an example the coastal marine communities of the southern Scotia Arc (South Orkney Islands and South Shetland Islands) and the west Antarctic Peninsula. Inshore, the ecological role of demersal fish is more important than that of krill. There, demersal fish are major consumers of benthos and also feed on zooplankton (mainly krill in summer). They are links between lower and upper levels of the food web and are common prey of other fish, birds and seals. Offshore, demersal fish depend less on benthos and feed more on zooplankton (mainly krill) and nekton, and are less accessible as prey of birds and seals. There, pelagic fish (especially lantern fish) are more abundant than inshore and play an important role in the energy flow from macrozooplankton to higher trophic levels (seabirds and seals). Through the higher fish predators, energy is transferred to land in the form of fish remains, pellets (birds), regurgitation and faeces (birds and seals). However, in the general context of the Antarctic marine ecosystem, krill (Euphausia superba) plays the central role in the food web because it is the main food source in terms of biomass for most of the high level predators from demersal fish up to whales. This has no obvious equivalent in other marine ecosystems. In Antarctic offshore coastal and oceanic waters the greatest proportion of energy from the ecosystem is transferred to land directly through krill consumers, such as flying birds, penguins, and seals. Beside krill, the populations of fish in the Antarctic Ocean are the second most important element for higher predators, in particular the energy-rich pelagic Myctophidae in open waters and the pelagic Antarctic silver fish (Pleuragramma antarcticum) in the high Antarctic zone. Although the occurrence of these pelagic fish inshore has been poorly documented, their abundance in neritic waters could be higher than previously believed.

scholarly journals Changes in the upper ocean mixed layer and phytoplankton productivity along the West Antarctic Peninsula

2018 ◽  
Vol 376 (2122) ◽  
pp. 20170173 ◽  
Author(s):  
Oscar Schofield ◽  
Michael Brown ◽  
Josh Kohut ◽  
Schuyler Nardelli ◽  
Grace Saba ◽  
...  
Keyword(s):  
Sea Ice ◽  
Antarctic Peninsula ◽  
Mixed Layer ◽  
Carbon Fixation ◽  
Upper Ocean ◽  
The West ◽  
Phytoplankton Productivity ◽  
West Antarctic ◽  
West Antarctic Peninsula

The West Antarctic Peninsula (WAP) has experienced significant change over the last 50 years. Using a 24 year spatial time series collected by the Palmer Long Term Ecological Research programme, we assessed long-term patterns in the sea ice, upper mixed layer depth (MLD) and phytoplankton productivity. The number of sea ice days steadily declined from the 1980s until a recent reversal that began in 2008. Results show regional differences between the northern and southern regions sampled during regional ship surveys conducted each austral summer. In the southern WAP, upper ocean MLD has shallowed by a factor of 2. Associated with the shallower mixed layer is enhanced phytoplankton carbon fixation. In the north, significant interannual variability resulted in the mixed layer showing no trended change over time and there was no significant increase in the phytoplankton productivity. Associated with the recent increases in sea ice there has been an increase in the photosynthetic efficiency (chlorophyll a -normalized carbon fixation) in the northern and southern regions of the WAP. We hypothesize the increase in sea ice results in increased micronutrient delivery to the continental shelf which in turn leads to enhanced photosynthetic performance. This article is part of the theme issue ‘The marine system of the West Antarctic Peninsula: status and strategy for progress in a region of rapid change’.

Enhanced oceanic CO2 uptake along the rapidly changing West Antarctic Peninsula

2019 ◽  
Vol 9 (9) ◽  
pp. 678-683 ◽  
Author(s):  
Michael S. Brown ◽  
David R. Munro ◽  
Colette J. Feehan ◽  
Colm Sweeney ◽  
Hugh W. Ducklow ◽  
...  
Keyword(s):  
Antarctic Peninsula ◽  
Co2 Uptake ◽  
West Antarctic ◽  
West Antarctic Peninsula

scholarly journals Sedimentary Nutrient Supply in Productive Hot Spots off the West Antarctic Peninsula Revealed by Silicon Isotopes

2020 ◽  
Vol 34 (12) ◽  
Author(s):  
Lucie Cassarino ◽  
Katharine R. Hendry ◽  
Sian F. Henley ◽  
Ellen MacDonald ◽  
Sandra Arndt ◽  
...  
Keyword(s):  
Antarctic Peninsula ◽  
Hot Spots ◽  
Nutrient Supply ◽  
The West ◽  
Silicon Isotopes ◽  
West Antarctic ◽  
West Antarctic Peninsula
Sign in / Sign up

Export Citation Format

Share Document