A variety of ice core and marine records have demonstrated regular climatic shifts in atmospheric and ocean temperature and nutrient content between glacial and interglacial periods. Reconstructions of Antarctic Intermediate Water (AAIW) have primarily focused upon the changes in the Atlantic, yet AAIW flows northward throughout the world’s oceans after forming in subantarctic waters in the Southern Ocean. The trace metal content of benthic foraminifera is commonly used to reconstruct changes in the nutrient content and temperature of waters. Trace metal incorporation into foraminiferal tests is usually controlled by environmental parameters. This proves not to be the case in the aragonitic foraminifera Hoeglundina elegans. Multi-element an...
This dissertation assesses the changing dominance of high-latitude intermediate waters and its impac...
© The Author(s), 2014. This article is distributed under the terms of the Creative Commons Attributi...
The Intermediate Mode Waters formed in the Southern Ocean are critical for the lower thermocline ven...
Sediment cores from the southern continental margin of Australia are near the formation region of An...
Reconstruction of intermediate water properties is important for understanding feedbacks within the ...
The use of δ13C within foraminifera as a nutrient proxy is complicated by air-sea exchange processes...
AbstractReconstruction of intermediate water properties is important for understanding feedbacks wit...
This dissertation assesses the changing dominance of high-latitude intermediate waters and its impac...
The extent of sea-ice and its interactions with biological and physical processes in the Southern Oc...
Antarctic Intermediate Water (AAIW) is an important conduit for nutrients to reach the nutrient-poor...
Reconstruction of intermediate water properties is important for understanding feedbacks within the ...
Deep‐sea sediment core FR1/97 GC‐12 is located 990 mbsl in the northern Tasman Sea, southwest Pacifi...
The main objective of this study was to reconstruct the evolution of the intermediate water circulat...
High-resolution textural, carbonate, microfossil, and oxygen (delta18O) and carbon (delta13C) stable...
Glacial/interglacial changes in Southern Ocean’s air-sea gas exchange have been considered as import...
This dissertation assesses the changing dominance of high-latitude intermediate waters and its impac...
© The Author(s), 2014. This article is distributed under the terms of the Creative Commons Attributi...
The Intermediate Mode Waters formed in the Southern Ocean are critical for the lower thermocline ven...
Sediment cores from the southern continental margin of Australia are near the formation region of An...
Reconstruction of intermediate water properties is important for understanding feedbacks within the ...
The use of δ13C within foraminifera as a nutrient proxy is complicated by air-sea exchange processes...
AbstractReconstruction of intermediate water properties is important for understanding feedbacks wit...
This dissertation assesses the changing dominance of high-latitude intermediate waters and its impac...
The extent of sea-ice and its interactions with biological and physical processes in the Southern Oc...
Antarctic Intermediate Water (AAIW) is an important conduit for nutrients to reach the nutrient-poor...
Reconstruction of intermediate water properties is important for understanding feedbacks within the ...
Deep‐sea sediment core FR1/97 GC‐12 is located 990 mbsl in the northern Tasman Sea, southwest Pacifi...
The main objective of this study was to reconstruct the evolution of the intermediate water circulat...
High-resolution textural, carbonate, microfossil, and oxygen (delta18O) and carbon (delta13C) stable...
Glacial/interglacial changes in Southern Ocean’s air-sea gas exchange have been considered as import...
This dissertation assesses the changing dominance of high-latitude intermediate waters and its impac...
© The Author(s), 2014. This article is distributed under the terms of the Creative Commons Attributi...
The Intermediate Mode Waters formed in the Southern Ocean are critical for the lower thermocline ven...