Antarctic terrestrial life–challenging the history of the frozen continent?
P Convey, JAE Gibson, CD Hillenbrand… - Biological …, 2008 - Wiley Online Library
Antarctica is a continent locked in ice, with almost 99.7% of current terrain covered by
permanent ice and snow, and clear evidence that, as recently as the Last Glacial Maximum …
permanent ice and snow, and clear evidence that, as recently as the Last Glacial Maximum …
[HTML][HTML] Reconstruction of ice-sheet changes in the Antarctic Peninsula since the Last Glacial Maximum
This paper compiles and reviews marine and terrestrial data constraining the dimensions
and configuration of the Antarctic Peninsula Ice Sheet (APIS) from the Last Glacial Maximum …
and configuration of the Antarctic Peninsula Ice Sheet (APIS) from the Last Glacial Maximum …
[LIVRE][B] Antarctic climate change and the environment
J Turner, R Bindschadler, P Convey, G Di Prisco… - 2009 - epic.awi.de
To understand how planet Earth works we study it increasingly as a system–a collection of
interdependent parts or spheres–the lithosphere, the hydrosphere, the cryosphere, the …
interdependent parts or spheres–the lithosphere, the hydrosphere, the cryosphere, the …
14C Chronostratigraphic Techniques in Paleolimnology
Down-core paleolimnological investigations of lake-sediment sequences require sufficient
age control to enable comparisons and correlations on local, regional and global scales …
age control to enable comparisons and correlations on local, regional and global scales …
Modelling and prediction of major soil chemical properties with Random Forest: Machine learning as tool to understand soil-environment relationships in Antarctica
RG Siqueira, CM Moquedace, EI Fernandes-Filho… - Catena, 2024 - Elsevier
Abstract Digital Soil Map** includes quantitative estimations of soil attributes in areas with
little or no soil information, being important in remote landscapes such as the Antarctic ice …
little or no soil information, being important in remote landscapes such as the Antarctic ice …
Mechanisms of Holocene palaeoenvironmental change in the Antarctic Peninsula region
The Antarctic Peninsula is one of the three fastest warming regions on Earth. Here we
review Holocene proxy records of marine and terrestrial palaeoclimate in the region, and …
review Holocene proxy records of marine and terrestrial palaeoclimate in the region, and …
Periglacial processes and landforms in the South Shetland Islands (northern Antarctic Peninsula region)
J López-Martínez, E Serrano, T Schmid, S Mink… - Geomorphology, 2012 - Elsevier
Periglacial processes and landforms together with the presence of permafrost are among
the most relevant geomorphological elements in the northern Antarctic Peninsula region …
the most relevant geomorphological elements in the northern Antarctic Peninsula region …
Late Holocene palaeoclimatic records from lake sediments on James Ross Island, Antarctica
S Björck, S Olsson, C Ellis-Evans, H Håkansson… - Palaeogeography …, 1996 - Elsevier
Sediment profiles from several lakes/ponds in the northern, ice-free area of James Ross
Island, Antarctica, were the subject of a multi-disciplinary palaeoenvironmental investigation …
Island, Antarctica, were the subject of a multi-disciplinary palaeoenvironmental investigation …
[HTML][HTML] Terrestrial and submarine evidence for the extent and timing of the Last Glacial Maximum and the onset of deglaciation on the maritime-Antarctic and sub …
This paper is the maritime and sub–Antarctic contribution to the Scientific Committee for
Antarctic Research (SCAR) Past Antarctic Ice Sheet Dynamics (PAIS) community Antarctic …
Antarctic Research (SCAR) Past Antarctic Ice Sheet Dynamics (PAIS) community Antarctic …
A conceptual model of the controlling factors of soil organic carbon and nitrogen densities in a permafrost‐affected region on the eastern Qinghai‐Tibetan Plateau
Many investigations of the preservation of soil organic carbon (SOC) in permafrost regions
have examined roles of geomorphology, pedogenesis, vegetation cover, and permafrost …
have examined roles of geomorphology, pedogenesis, vegetation cover, and permafrost …