Terri Souster

Terri Souster
  • Doctor of Philosophy
  • PostDoc Position at UiT The Arctic University of Norway

Post Doctoral Researcher at The Arctic University of Norway. Cumulative stressors on Arctic marine ecosystems

About

18
Publications
5,884
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409
Citations
Introduction
Currently working on benthic blue carbon data for the coastal shallows on the Antarctic Peninsula and The Arctic's Barents Sea. I am a self-motivated, independent and conscientious marine scientist with extensive research experience who works well, both independently, and within a team. My research interests are biodiversity, physiology and ecology. I have worked as a marine biologist for the past 12 years. During this time I have become competent in GIS and multivariate statistical analysis and
Current institution
UiT The Arctic University of Norway
Current position
  • PostDoc Position

Publications

Publications (18)
Article
Sea lice are ectoparasites that can be found in high numbers in and around salmon farms, where they are a threat to fish health and can induce high aquacultural costs. Large numbers of suitable hosts facilitate the infection and subsequent release of their planktonic larvae in the surrounding environment where they can potentially infect wild salmo...
Article
Full-text available
Oceanographic changes adjacent to Antarctica have global climatic and ecological impacts. However, this is the most challenging place in the world to obtain marine data due to its remoteness and inhospitable nature, especially in winter. Here, we present more than 2000 Conductivity-Temperature-Depth (CTD) profiles and associated water sample data c...
Article
Full-text available
Meaningful protection of global oceans lags far behind that of land and has taken little consideration of climate mitigation potential to date (such as through assessment of blue carbon stocks and change). With the new emphasis on synergistic approaches to the identification and conservation of both carbon- and species- rich habitats, we need much...
Article
Full-text available
Simple Summary Seafloor biodiversity provides a key ecosystem service, as an efficient route for carbon to be removed from the atmosphere to become buried (long-term) in marine sediment. Protecting near intact ecosystems, particularly those that are hotspots of biodiversity, with high numbers of unique species (endemics), is increasingly being reco...
Article
Full-text available
Simple Summary Solving biodiversity loss and climate change are part of the same problem; intact natural habitats can provide powerful and efficient climate mitigation if protected. Beyond the land (forests), there is little appreciation of just how important ocean nature is to climate mitigation. Carbon captured, stored and the rate at which it is...
Article
Full-text available
Unprecedented and dramatic transformations are occurring in the Arctic in response to climate change, but academic, public, and political discourse has disproportionately focussed on the most visible and direct aspects of change, including sea ice melt, permafrost thaw, the fate of charismatic megafauna, and the expansion of fisheries. Such narrati...
Article
The flapper skate, Dipturus intermedius (Parnell, 1837), is the largest of all European skate and rays (Superorder: Batoidea). It is found in coastal waters of the European continental shelf and slopes in the North-East (NE) Atlantic. With the 2006 IUCN Red List of Threatened Species classification of ‘common skate’ as Critically Endangered, and th...
Article
Full-text available
The flow of carbon from atmosphere to sediment fauna and sediments reduces atmospheric CO 2 , which in turn reduces warming. Here, during the Changing Arctic Ocean Seafloor programme, we use comparable methods to those used in the Antarctic (vertical, calibrated camera drops and trawl-collected specimens) to calculate the standing stock of zoobenth...
Preprint
Full-text available
Cite this article: Souster TA, Barnes DKA, Hopkins J. 2020 Variation in zoobenthic blue carbon in the Arctic's Barents Sea shelf sediments. Phil. Trans. R. Soc. A 378: 20190362. http://dx.
Conference Paper
Full-text available
As oceans warm, reducing the extent of sea-ice and-ice shelves, increased carbon capture by phytoplankton and storage by southern polar benthos (sea bed organisms), is potentially the largest negative feedback on climate change. Teasing apart biological processes within and between geographic regions is vital to our understanding of global carbon c...
Article
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The waters of the Southern Ocean exhibit extreme seasonality in primary production, with marine life living below 0 °C for much of the year. The metabolic cold adaptation (MCA) hypothesis suggests that polar species need elevated basal metabolic rates to enable activity in such cold which should result in higher metabolic rates, or at least rates s...
Article
Full-text available
Juvenile stages are often thought to be less resistant to thermal challenges than adults, yet few studies make direct comparisons using the same methods between different life history stages. We tested the resilience of juvenile stages compared to adults in 4 species of Antarctic marine invertebrate over 3 different rates of experimental warming. T...
Article
Full-text available
Climate change and human activities are expected to have a major impact on the structure and functioning of marine ecosystems and the biogeochemical cycles they mediate in the coming years. Here we describe time series measurements of biogenic bromocarbons (CHBr3 and CH2Br2) collected in coastal waters of the western Antarctic Peninsula which is on...
Article
Full-text available
Regeneration of arms in brittle stars is thought to proceed slowly in low temperature environments. Here a survey of natural arm damage and arm regeneration rates is documented in the Antarctic brittle star Ophiura crassa. This relatively small ophiuroid, a detritivore found amongst red macroalgae, displays high levels of natural arm damage and rep...
Article
Full-text available
The West Antarctic Peninsula (WAP) is a hotspot of recent rapid regional warming and ice loss. The WAP sea surface freezes each winter to form a `fast-ice' skin that can reduce iceberg drift and collisions between their keels and the sea bed, in what is termed scouring. Scouring disturbance is thus inversely correlated with fast-ice duration. We ex...
Article
In recent decades, the west Antarctic Peninsula (WAP) has warmed more rapidly than anywhere else in the Southern Hemisphere. Associated with this, there has been a marked shortening of the sea ice season, a retreat of the majority of glaciers, and an increase in precipitation. Each of these changes in the freshwater system has the potential to exer...

Questions

Question (1)
Question
I was hoping you could help me with a quick stats query
I have species richness data from 2011, 2 factors season and depth and I have plotted the data on a graph with +/- SD (figure attached).
Looking at the figure looks to me there is no significant difference in depth or season.
However, I wanted to run a GLM to test for difference but I can not get the data normalised, I have tried multiple transformations and the data are still not normally distributed (Attached minitab file with the data). The transformations did not even allow me to get the data to being close to normalisation as I appreciate ANOVA is a robust test.
I then thought I would put the data into PRIMER and did a fourth root transformation, resemblance matrix and then ran a 2 way crossed ANOSIM which gave me the result of Season ANOSIM R = 0.092 P < 0.001 Depth ANOSIM R = 0.507 P < 0.001 which says that north season and depth are significantly different (Right?)
which is not what I was expecting or my figure shows so now I am thinking I have either done something wrong or misunderstood something. I have chatted this through with a couple of work colleagues but we are not getting anywhere and I was hoping you could have a look for me (PRIMER FILE WITH DATA ATTACHED).

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