Bestley Sophie

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Bestley
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Sophie
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  • Article
    Marine ecosystem assessment for the Southern Ocean: birds and marine mammals in a changing climate
    (Frontiers Media, 2020-11-04) Bestley, Sophie ; Ropert-Coudert, Yan ; Bengtson Nash, Susan ; Brooks, Cassandra M. ; Cotté, Cédric ; Dewar, Meagan ; Friedlaender, Ari S. ; Jackson, Jennifer A. ; Labrousse, Sara ; Lowther, Andrew D. ; McMahon, Clive R. ; Phillips, Richard A. ; Pistorius, Pierre ; Puskic, Peter S. ; de Almeida Reis, Ana Olívia ; Reisinger, Ryan ; Santos, Mercedes ; Tarszisz, Esther ; Tixier, Paul ; Trathan, Phil N. ; Wege, Mia ; Wienecke, Barbara
    The massive number of seabirds (penguins and procellariiformes) and marine mammals (cetaceans and pinnipeds) – referred to here as top predators – is one of the most iconic components of the Antarctic and Southern Ocean. They play an important role as highly mobile consumers, structuring and connecting pelagic marine food webs and are widely studied relative to other taxa. Many birds and mammals establish dense breeding colonies or use haul-out sites, making them relatively easy to study. Cetaceans, however, spend their lives at sea and thus aspects of their life cycle are more complicated to monitor and study. Nevertheless, they all feed at sea and their reproductive success depends on the food availability in the marine environment, hence they are considered useful indicators of the state of the marine resources. In general, top predators have large body sizes that allow for instrumentation with miniature data-recording or transmitting devices to monitor their activities at sea. Development of scientific techniques to study reproduction and foraging of top predators has led to substantial scientific literature on their population trends, key biological parameters, migratory patterns, foraging and feeding ecology, and linkages with atmospheric or oceanographic dynamics, for a number of species and regions. We briefly summarize the vast literature on Southern Ocean top predators, focusing on the most recent syntheses. We also provide an overview on the key current and emerging pressures faced by these animals as a result of both natural and human causes. We recognize the overarching impact that environmental changes driven by climate change have on the ecology of these species. We also evaluate direct and indirect interactions between marine predators and other factors such as disease, pollution, land disturbance and the increasing pressure from global fisheries in the Southern Ocean. Where possible we consider the data availability for assessing the status and trends for each of these components, their capacity for resilience or recovery, effectiveness of management responses, risk likelihood of key impacts and future outlook.
  • Article
    First description of in situ chlorophyll fluorescence signal within East Antarctic coastal polynyas during fall and winter
    (Frontiers Media, 2023-07-27) Bourreau, Lucie ; Pauthenet, Etienne ; Le Ster, Loic ; Picard, Baptiste ; Portela, Esther ; Salle, Jean-Baptiste ; McMahon, Clive R. ; Harcourt, Robert ; Hindell, Mark ; Guinet, Christophe ; Bestley, Sophie ; Charrassin, Jean-Benoit ; DuVivier, Alice ; Sylvester, Zephyr ; Krumhardt, Kristen ; Jenouvrier, Stephanie ; Labrousse, Sara
    Antarctic coastal polynyas are persistent and recurrent regions of open water located between the coast and the drifting pack-ice. In spring, they are the first polar areas to be exposed to light, leading to the development of phytoplankton blooms, making polynyas potential ecological hotspots in sea-ice regions. Knowledge on polynya oceanography and ecology during winter is limited due to their inaccessibility. This study describes i) the first in situ chlorophyll fluorescence signal (a proxy for chlorophyll-a concentration and thus presence of phytoplankton) in polynyas between the end of summer and winter, ii) assesses whether the signal persists through time and iii) identifies its main oceanographic drivers. The dataset comprises 698 profiles of fluorescence, temperature and salinity recorded by southern elephant seals in 2011, 2019-2021 in the Cape-Darnley (CDP;67˚S-69˚E) and Shackleton (SP;66˚S-95˚E) polynyas between February and September. A significant fluorescence signal was observed until April in both polynyas. An additional signal occurring at 130m depth in August within CDP may result from in situ growth of phytoplankton due to potential adaptation to low irradiance or remnant chlorophyll-a that was advected into the polynya. The decrease and deepening of the fluorescence signal from February to August was accompanied by the deepening of the mixed layer depth and a cooling and salinification of the water column in both polynyas. Using Principal Component Analysis as an exploratory tool, we highlighted previously unsuspected drivers of the fluorescence signal within polynyas. CDP shows clear differences in biological and environmental conditions depending on topographic features with higher fluorescence in warmer and saltier waters on the shelf compared with the continental slope. In SP, near the ice-shelf, a significant fluorescence signal in April below the mixed layer (around 130m depth), was associated with fresher and warmer waters. We hypothesize that this signal could result from potential ice-shelf melting from warm water intrusions onto the shelf leading to iron supply necessary to fuel phytoplankton growth. This study supports that Antarctic coastal polynyas may have a key role for polar ecosystems as biologically active areas throughout the season within the sea-ice region despite inter and intra-polynya differences in environmental conditions.