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An environmental history of two freshwater lakes in the Larsemann Hills, Antarctica
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What this work says
Outgoing claims: the papers this work cites, builds on, or argues with.
inferredcites →https://doi.org/10.1007/bf00048724openalex-snapshot
24. Chemistry, physics and evolution of Antarctic saline lakes
inferredcites →https://doi.org/10.1111/j.1095-8312.1980.tb00097.xopenalex-snapshot
Evolution of Antarctic lake ecosystems
inferredcites →https://doi.org/10.1111/j.1469-185x.1986.tb00718.xopenalex-snapshot
ANTARCTIC AQUATIC ECOSYSTEMS AS HABITATS FOR PHYTOPLANKTON
inferredcites →https://doi.org/10.2216/i0031-8884-24-2-155.1openalex-snapshot
The genus Thalassiosira (Bacillariophyceae): studies on species occurring south of the Antarctic Convergence Zone
What points at this work
Incoming claims: where this work appears in other papers’ reference lists and arguments.
inferred← citeshttps://doi.org/10.11646/phytotaxa.712.1.8zenodo-depositor-declared
Cosmarium hiranoi sp. nov (Zygnematophyceae, Desmidiaceae): a new desmid species from a lake in Oasis Larsemann Hills (East Antarctica)
inferred← citeshttps://doi.org/10.2139/ssrn.4793650openalex-extracted
10be Exposure Age Evidence of Ice Sheet Histories in Larsemann Hills During the Last Glacial
inferred← citeshttps://doi.org/10.1002/esp.3290200608openalex-snapshot
Rates of rock surface lowering, Princess Elizabeth land, Eastern Antarctica
inferred← citeshttps://doi.org/10.1002/jqs.823openalex-snapshot
Late Quaternary deglaciation and climate history of the Larsemann Hills (East Antarctica)
inferred← citeshttps://doi.org/10.1007/1-4020-5277-4_13openalex-snapshot
Antarctic Lake Systems and Climate Change
inferred← citeshttps://doi.org/10.1007/978-3-642-56318-8_13openalex-snapshot
Plant Communities at Wilkes Land
inferred← citeshttps://doi.org/10.1007/978-3-642-56318-8_4openalex-snapshot
Wilkes Land (Casey Station)
inferred← citeshttps://doi.org/10.1007/bf00051985openalex-snapshot
Microbial diversity and function in Antarctic freshwater ecosystems
inferred← citeshttps://doi.org/10.1007/bf00051986openalex-snapshot
The diversity, distribution and ecology of diatoms from Antarctic inland waters
inferred← citeshttps://doi.org/10.1007/bf00678106openalex-snapshot
Radiometric dating of lake sediments from Signy Island (maritime Antarctic): evidence of recent climatic change
inferred← citeshttps://doi.org/10.1007/s00300-009-0676-4openalex-snapshot
Microbially mediated redox transformations of manganese (II) along with some other trace elements: a study from Antarctic lakes
inferred← citeshttps://doi.org/10.1007/s41651-026-00259-2openalex-snapshot
Enhancing Topographic Mapping Using Relief Shading: A Case Study of the Larsemann Hills, East Antarctica
inferred← citeshttps://doi.org/10.1007/s41748-020-00154-wopenalex-snapshot
Persistent Organic Pollutants in Lakes of Grovnes Peninsula at Larsemann Hill Area, East Antarctica
inferred← citeshttps://doi.org/10.1016/j.apgeochem.2012.08.009openalex-snapshot
Holocene lake development and glacial-isostatic uplift at Lake Skallen and Lake Oyako, Lützow-Holm Bay, East Antarctica: Based on biogeochemical facies and molecular signatures
inferred← citeshttps://doi.org/10.1016/j.catena.2025.109367openalex-snapshot
Mapping the paleo ice-flow in Larsemann Hills, East Antarctica by UAV remote sensing and terrain analysis
inferred← citeshttps://doi.org/10.1016/j.orggeochem.2017.01.003openalex-snapshot
Identification of a novel fatty acid in the cell membrane of Chryseobacterium frigidisoli PB4 T isolated from an East Antarctic glacier forefield
inferred← citeshttps://doi.org/10.1016/j.palaeo.2024.112357openalex-snapshot
10Be exposure age data reveals last Glacial ice sheet histories in the Larsemann Hills of East Antarctica
inferred← citeshttps://doi.org/10.1016/j.polar.2018.04.002openalex-snapshot
Inverted sediments in the coastal Antarctic lake: Evidence of paleostorm?
inferred← citeshttps://doi.org/10.1016/j.polar.2025.101214openalex-snapshot
A geological cross section of Neogene to Quaternary sediments in the Larsemann Hills, East Antarctica
inferred← citeshttps://doi.org/10.1016/j.quaint.2020.10.031openalex-snapshot
Last exposure process of the Larsemann Hills and adjacent area, East Antarctica, based on bedrock exposure ages
inferred← citeshttps://doi.org/10.1016/j.quascirev.2009.06.011openalex-snapshot
Holocene glacial history of Antarctica and the sub-Antarctic islands
inferred← citeshttps://doi.org/10.1016/s0012-821x(97)00204-5openalex-snapshot
Holocene sea-level change and ice-sheet history in the Vestfold Hills, East Antarctica
inferred← citeshttps://doi.org/10.1016/s1571-0866(04)80109-xopenalex-snapshot
Quaternary glacial and climate history of Antarctica
inferred← citeshttps://doi.org/10.1017/s0954102009002028openalex-snapshot
Deglaciation and weathering of Larsemann Hills, East Antarctica
inferred← citeshttps://doi.org/10.1023/a:1007947402927openalex-snapshot
A weighted-averaging regression and calibration model for inferring lakewater salinity from fossil diatom assemblages in saline lakes of the Vestfold Hills: a new tool for interpreting Holocene lake histories in Antarctica
inferred← citeshttps://doi.org/10.1023/a:1021661700899openalex-snapshot
Holocene environmental changes and development of Figurnoye Lake in the southern Bunger Hills, East Antarctica
inferred← citeshttps://doi.org/10.1023/a:1025570904093openalex-snapshot
Modelling diatom responses to climate induced fluctuations in the moisture balance in continental Antarctic lakes
inferred← citeshttps://doi.org/10.1029/2020jb020167openalex-snapshot
Ice Sheet Changes and GIA‐Induced Surface Displacement of the Larsemann Hills During the Last 50 kyr
inferred← citeshttps://doi.org/10.1111/j.1755-6724.2010.00271.xopenalex-snapshot
Minimum Bedrock Exposure Ages and Their Implications: Larsemann Hills and Neighboring Bolingen Islands, East Antarctica
inferred← citeshttps://doi.org/10.1130/0091-7613(2001)029<1103:bheaif>2.0.co;2openalex-snapshot
Bunger Hills, East Antarctica: Ice free at the Last Glacial Maximum
inferred← citeshttps://doi.org/10.1144/sp381.22openalex-snapshot
Sedimentary processes in two different polar periglacial environments: Examples from Schirmacher Oasis and Larsemann Hills, East Antarctica
inferred← citeshttps://doi.org/10.1191/0959683604hl702rpopenalex-snapshot
Coastal oceanographic conditions in the Prydz Bay region (East Antarctica) during the Holocene recorded in an isolation basin
inferred← citeshttps://doi.org/10.1515/ohs-2017-0034openalex-snapshot
Diatom assemblages as indicators of salinity gradients: a case study from a coastal lake
inferred← citeshttps://doi.org/10.17491/jgsi.2026.174510openalex-snapshot
Extending the Holocene Record of Marine Diatoms in East Antarctica: Evidence from the Larsemann Hills
inferred← citeshttps://doi.org/10.5194/bgd-7-4341-2010openalex-snapshot
Crustal uplifting rate associated with late-Holocene glacial-isostatic rebound at Skallen and Skarvsnes, Lützow-Holm Bay, East Antarctica: evidence of a synchrony in sedimentary and biological facies on geological setting
inferred← citeshttps://doi.org/10.5194/tc-15-2667-2021openalex-snapshot
Retention time of lakes in the Larsemann Hills oasis, East Antarctica
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