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Title | Type | Journal | |||
Year | 2011 | Publication | Journal of Ornithology | Abbreviated Journal | |
Volume | 152 | Issue | 1 | Pages | 279-288 |
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Programme | 109 | ||||
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Series Volume | Series Issue | Edition | |||
ISSN | 2193-7206 | ISBN | Medium | ||
Area | Expedition | Conference | |||
Notes | Approved | yes | |||
Call Number | Serial | 8221 | |||
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Title | Unveiling the co-phylogeny signal between plunderfish Harpagifer spp. and their gut microbiomes across the Southern Ocean | Type | Journal | ||
Year | 2023 | Publication | Biorxiv | Abbreviated Journal | |
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Programme | 1044 | ||||
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Notes | Approved | yes | |||
Call Number | Serial | 8685 | |||
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Title | Factors affecting adult body condition in the endangered northern rockhopper penguin | Type | Journal | ||
Year | 2021 | Publication | Marine Biology | Abbreviated Journal | |
Volume | 168 | Issue | 3 | Pages | 27 |
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Programme | 109,394 | ||||
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Corporate Author | Thesis | Bachelor's thesis | |||
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Series Volume | Series Issue | Edition | |||
ISSN | 1432-1793 | ISBN | Medium | ||
Area | Expedition | Conference | |||
Notes | Approved | yes | |||
Call Number | Serial | 7792 | |||
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Author | Lynner Colton, Long Maureen D, | ||||
Title | Sub-slab anisotropy beneath the Sumatra and circum-Pacific subduction zones from source-side shear wave splitting observations | Type | Journal Article | ||
Year | 2014 | Publication | Geochemistry, Geophysics, Geosystems | Abbreviated Journal | |
Volume | 15 | Issue | 6 | Pages | 2262-2281 |
Keywords | source-side splitting, sub-slab anisotropy, shear wave splitting, 7240 Subduction zones, 7208 Mantle, | ||||
Abstract | Understanding the dynamics of subduction is critical to our overall understanding of plate tectonics and the solid Earth system. Observations of seismic anisotropy can yield constraints on deformation patterns in the mantle surrounding subducting slabs, providing a tool for studying subduction dynamics. While many observations of seismic anisotropy have been made in subduction systems, our understanding of the mantle beneath subducting slabs remains tenuous due to the difficulty of constraining anisotropy in the sub-slab region. Recently, the source-side shear wave splitting technique has been refined and applied to several subduction systems worldwide, making accurate and direct measurements of sub-slab anisotropy feasible and offering unprecedented spatial and depth coverage in the sub-slab mantle. Here we present source-side shear wave splitting measurements for the Central America, Alaska-Aleutians, Sumatra, Ryukyu, and Izu-Bonin-Japan-Kurile subduction systems. We find that measured fast splitting directions in these regions generally fall into two broad categories, aligning either with the strike of the trench or with the motion of the subducting slab relative to the overriding plate. Trench parallel fast splitting directions dominate beneath the Izu-Bonin, Japan, and southern Kurile slabs and part of the Sumatra system, while fast directions that parallel the motion of the downgoing plate dominate in the Ryukyu, Central America, northern Kurile, western Sumatra, and Alaska-Aleutian regions. We find that plate motion parallel fast splitting directions in the sub-slab mantle are more common than previously thought. We observe a correlation between fast direction and age of the subducting lithosphere; older lithosphere (>95 Ma) is associated with trench parallel splitting while younger lithosphere (<95 Ma) is associated with plate motion parallel fast splitting directions. Finally, we observe source-side splitting for deep earthquakes (transition zone depths) beneath Japan and Sumatra, suggesting the presence of anisotropy at midmantle depths beneath these regions.
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Programme | 133 | ||||
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Series Volume | Series Issue | Edition | |||
ISSN | 1525-2027 | ISBN | Medium | ||
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Notes | Approved | yes | |||
Call Number | Serial | 5036 | |||
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Title | Remote Antarctic feeding ground important for east Australian humpback whales | Type | Journal | ||
Year | 2014 | Publication | Marine Biology | Abbreviated Journal | |
Volume | 161 | Issue | 5 | Pages | 1087-1093 |
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Programme | 1014 | ||||
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Series Volume | Series Issue | Edition | |||
ISSN | 1432-1793 | ISBN | Medium | ||
Area | Expedition | Conference | |||
Notes | Approved | yes | |||
Call Number | Serial | 8160 | |||
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Title | How Elephant Seals (Mirounga leonina) Adjust Their Fine Scale Horizontal Movement and Diving Behaviour in Relation to Prey Encounter Rate | Type | Journal | ||
Year | 2016 | Publication | Plos one | Abbreviated Journal | |
Volume | 11 | Issue | 12 | Pages | e0167226 |
Keywords | Foraging Predation Acceleration Animal behavior Predator-prey dynamics Seals Swimming Water columns | ||||
Abstract | Understanding the diving behaviour of diving predators in relation to concomitant prey distribution could have major practical applications in conservation biology by allowing the assessment of how changes in fine scale prey distribution impact foraging efficiency and ultimately population dynamics. The southern elephant seal (Mirounga leonina, hereafter SES), the largest phocid, is a major predator of the southern ocean feeding on myctophids and cephalopods. Because of its large size it can carry bio-loggers with minimal disturbance. Moreover, it has great diving abilities and a wide foraging habitat. Thus, the SES is a well suited model species to study predator diving behaviour and the distribution of ecologically important prey species in the Southern Ocean. In this study, we examined how SESs adjust their diving behaviour and horizontal movements in response to fine scale prey encounter densities using high resolution accelerometers, magnetometers, pressure sensors and GPS loggers. When high prey encounter rates were encountered, animals responded by (1) diving and returning to the surface with steeper angles, reducing the duration of transit dive phases (thus improving dive efficiency), and (2) exhibiting more horizontally and vertically sinuous bottom phases. In these cases, the distance travelled horizontally at the surface was reduced. This behaviour is likely to counteract horizontal displacement from water currents, as they try to remain within favourable prey patches. The prey encounter rate at the bottom of dives decreased with increasing diving depth, suggesting a combined effect of decreased accessibility and prey density with increasing depth. Prey encounter rate also decreased when the bottom phases of dives were spread across larger vertical extents of the water column. This result suggests that the vertical aggregation of prey can regulate prey density, and as a consequence impact the foraging success of SESs. To our knowledge, this is one of only a handful of studies showing how the vertical distributions and structure of prey fields influence the prey encounter rates of a diving predator. | ||||
Programme | 109 | ||||
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Series Volume | Series Issue | Edition | |||
ISSN | 1932-6203 | ISBN | 1932-6203 | Medium | |
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Notes | Approved | yes | |||
Call Number | Serial | 6607 | |||
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Author | Christophe Sauser, Karine Delord, Christophe Barbraud | ||||
Title | Demographic sensitivity to environmental forcings: a multi-trait, multi-colony approach | Type | Journal | ||
Year | 2021 | Publication | Oikos | Abbreviated Journal | |
Volume | 130 | Issue | 6 | Pages | 943-957 |
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Programme | 109 | ||||
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Series Volume | Series Issue | Edition | |||
ISSN | 1600-0706 | ISBN | 1600-0706 | Medium | |
Area | Expedition | Conference | |||
Notes | Approved | yes | |||
Call Number | Serial | 8039 | |||
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Title | Assessing recent trends in high-latitude Southern Hemisphere surface climate | Type | Journal | ||
Year | 2016 | Publication | Nature Climate Change | Abbreviated Journal | |
Volume | 6 | Issue | 10 | Pages | 917-926 |
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Abstract | Understanding the causes of recent climatic trends and variability in the high-latitude Southern Hemisphere is hampered by a short instrumental record. Here, we analyse recent atmosphere, surface ocean and sea-ice observations in this region and assess their trends in the context of palaeoclimate records and climate model simulations. Over the 36-year satellite era, significant linear trends in annual mean sea-ice extent, surface temperature and sea-level pressure are superimposed on large interannual to decadal variability. Most observed trends, however, are not unusual when compared with Antarctic palaeoclimate records of the past two centuries. With the exception of the positive trend in the Southern Annular Mode, climate model simulations that include anthropogenic forcing are not compatible with the observed trends. This suggests that natural variability overwhelms the forced response in the observations, but the models may not fully represent this natural variability or may overestimate the magnitude of the forced response. | ||||
Programme | 1154 | ||||
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ISSN | 1758-6798 | ISBN | 1758-6798 | Medium | |
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Notes | Approved | yes | |||
Call Number | Serial | 6737 | |||
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Title | Activity-stability relationships in extremophilic enzymes. | Type | Conference - International - Poster | ||
Year | 2004 | Publication | Abbreviated Journal | ||
Volume | Issue | Pages | |||
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Programme | 193 | ||||
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Notes | Approved | yes | |||
Call Number | Serial | 3915 | |||
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Author | Alessio Gusmeroli, Erin Pettit, Catherine Ritz, Joseph Kennedy, Maurine Montagnat, Eric Lefebvre, Gael Durand, Sepp Kipfstuhl, and Simon Sheldon. | ||||
Title | The relationship between climate and ice rheology at Dome C, East Antarctica: a comparison of fabric determined by borehole sonic logging and thin sections. | Type | Conference - International - Communication | ||
Year | 2011 | Publication | Abbreviated Journal | ||
Volume | Vol. 13, EGU2011-2341, 2011 | Issue | Pages | ||
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Abstract | Understanding past climate changes as recorded in annual layers within ice sheets is a societal and scientific priority. Oxygen isotopes from several deep ice-cores in Greenland and Antarctica have revealed oscillations with a 100 kyr periodicity extending back at least 740 kyr BP. The EPICA Dome C ice core, the longest climate record obtained from ice, records eight glacial-interglacial transitions where abrupt climate transitions typically separate warm periods (interglacial) from cool periods (glacial). These warm and cool periods are referred to as Marine Isotope Stages (MIS).
Many scientists have observed that the physical properties of glacial ice differs from those of interglacial ice. Glacial ice typically has smaller crystals, higher impurity content, and stronger fabric (preferred orientation of crystal c-axes). Because ice deformation is sensitive to the orientation of crystals, ice flow patterns are sensitive to the fabric and, therefore, to this glacial-interglacial dichotomy. Indeed at Dome C an abrupt, unexpected strengthening of the fabric at the depth of 1750 m marks the transition between the warm MIS5 and the cold MIS6. Because there is a positive feedback between fabric development and ice deformation, changes in ice fabric may be therefore used to understand climate transitions. We present a vertical-profile of compressional (P) wave speeds acquired every 0.1m in the 3.2 km-deep EPICA Dome C borehole. Each measurements samples ice crystals within a volume approximately 3 m long and 2 m wide ice. We relate the P-wave speeds to fabric through the known seismic anisotropy of a single ice-crystals (P-wave speed is 5% faster when propagates along the crystallographic c-axis than the basal plane). We integrate this seismically-derived fabric profile with the more sparse (about 100 m for most of the core) thin-section-derived fabric to present a more complete vertical-profile of fabric. We provide a preliminary comparison of the shifts in fabric which occur at each of the abrupt climate transitions and relate these to other measurements made on the ice core and in the borehole such as dust and oxygen isotopes. |
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Programme | 902 | ||||
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Notes | Approved | yes | |||
Call Number | Serial | 3592 | |||
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