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Geology defines microbiome structure and composition in nunataks and valleys of the Sør Rondane Mountains, East Antarctica
Published 2024-02-01“…Here we examined the composition of bacterial and micro-eukaryotic communities using amplicon sequencing of rRNA genes in 105 soil samples from the Sør Rondane Mountains (East Antarctica), differing in bedrock or substrate type and associated physicochemical conditions. …”
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142
Uranium record from a 3 m snow pit at Dome Argus, East Antarctica.
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143
Stratigraphic noise and its potential drivers across the plateau of Dronning Maud Land, East Antarctica
Published 2023-10-01“…Here, we assess the amount and structure of stratigraphic noise at seven sites along a 120 km transect on the plateau of Dronning Maud Land, East Antarctica. Replicated oxygen isotope records of 1 m length were used to estimate signal-to-noise ratios as a measure of stratigraphic noise at sites characterised by different accumulation rates (43–64 mm w.e. a<span class="inline-formula"><sup>−1</sup></span>), snow surface roughnesses and slope inclinations. …”
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144
The Bedrock Topography Deduced from Multiple Radar Echoes Observed in the Mizuho Plateau, East Antarctica
Published 1978-03-01Get full text
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145
Structural Geology and Petrology of East Ongul Island, East Antarctica Part I. Structural Geology
Published 1962-01-01Get full text
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146
Brief communication: Organochlorine pesticides in an archived firn core from Law Dome, East Antarctica
Published 2016-10-01“…Organochlorine pesticides (OCPs) were, for the first time, quantified in archived firn cores from East Antarctica representative of 1945–1957 and 1958–1967 (current era, C.E.). …”
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147
A topographic hinge-zone divides coastal and inland ice dynamic regimes in East Antarctica
Published 2023-01-01“…The Heimefrontfjella escarpment in Dronning Maud Land, East Antarctica divides inland precipitation-dominated ice dynamics from coastal dynamics dominated by grounding line migration, suggest inverse model simulations constrained by cosmogenic nuclide measurements.…”
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148
Systems Analysis of complex glaciological processes and application to calving of Amery Ice Shelf, East Antarctica
Published 2017-04-01“…Here we apply Systems Analysis to the Amery rift system, East Antarctica. We develop a scalable ‘System Model’ driven by a coarsely-sampled dataset characteristic of glaciological observations in remote locations, and validate it using rift lengths observed in 2000–06 and 2012. …”
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149
The vertical structure of precipitation at two stations in East Antarctica derived from micro rain radars
Published 2019-01-01“…Two observatories dedicated to precipitation have been set up at the Belgian station Princess Elisabeth (PE) and at the French station Dumont d'Urville (DDU) in East Antarctica. Among other instruments, both sites have a vertically pointing micro rain radar (MRR) working at the K band. …”
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150
ICE VELOCITY MEASUREMENT IN EAST ANTARCTICA FROM 1960s TO 1980s BASED ON ARGON AND LANDSAT IMAGERY
Published 2017-09-01“…Furthermore, a 1960-80s ice flow speed map in the main glaciers of East Antarctica is produced for the first time.…”
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A new approach to estimate ice dynamic rates using satellite observations in East Antarctica
Published 2017-05-01“…Despite available estimates on ice dynamic rates obtained from radar altimetry, information about ice sheet changes due to changes in the ice dynamics are still limited, especially in East Antarctica. Without understanding ice dynamic rates, it is not possible to properly assess changes in ice sheet mass balance and surface elevation or to develop ice sheet models. …”
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153
Climatic signals from 76 shallow firn cores in Dronning Maud Land, East Antarctica
Published 2015-05-01“…The Southern Annular Mode (SAM) has exhibited a positive trend since the mid-1960s, which is assumed to lead to a cooling of East Antarctica. This is not confirmed by the firn core data in our data set. …”
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154
Radar Sounding Confirms a Hydrologically Active Deep-Water Subglacial Lake in East Antarctica
Published 2020-07-01“…Lake CookE2, upstream of Cook Glacier in East Antarctica, is an “active” subglacial lake that experiences episodic discharge and recharge of basal water. …”
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155
Field measurement of the photosynthesis of mosses with a portable CO2 porometer at Langhovde, East Antarctica
Published 1994-07-01“…The photosynthesis of mosses was measured with a portable CO_2 porometer (modified Koito KIP9000) at Langhovde, East Antarctica in January 1988. An assimilation chamber, 10cm×10cm×6.5cm, which was made for this measurement, was used in collecting data for 9h in Sample 1 and 11h in Sample 2. …”
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156
Age-related environmental gradients influence invertebrate distribution in the Prince Charles Mountains, East Antarctica
Published 2016-01-01“…We used biodiversity information derived from high-throughput sequencing (HTS) to elucidate the relationship between soil properties and invertebrate biodiversity in the Prince Charles Mountains, East Antarctica. Across 136 analysed soil samples collected from Mount Menzies, Mawson Escarpment and Lake Terrasovoje, we found invertebrate distribution in the Prince Charles Mountains significantly influenced by soil salinity and/or sulfur content. …”
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157
Recent increase in the surface mass balance in central East Antarctica is unprecedented for the last 2000 years
Published 2024-04-01“…Here, we use data from firn cores drilled near Vostok station (central East Antarctica) to analyze the surface mass balance variability over the past 2200 years. …”
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158
Exhumation and tectonic history of inaccessible subglacial interior East Antarctica from thermochronology on glacial erratics
Published 2022-10-01“…Glacially transported igneous rocks eroded from the deep interior of ice-covered East Antarctica constrain a remarkable episodic cooling and exhumation history that helps unravel its mysterious tectonic evolution over the last 500 million years.…”
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159
Spatial variability and post-depositional diffusion of stable isotopes in high accumulation regions of East Antarctica
Published 2022-08-01“…We analyzed the spatio-temporal variations of snow accumulation, stable isotopic composition, and factors controlling their distribution along two transects in the Dronning Maud Land (DML) and Princess Elizabeth Land (PEL) regions of East Antarctica. The δ18O and δD variations are dominantly influenced by snow accumulation in the DML region and temperature in the PEL region. …”
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