In this paper we present geological evidence from the Larsemann Hills (Lambert Glacier – Amery Ice Shelf region, East Antarctica) of marine sediments at an altitude of c. 8 m a.s.l., as revealed by diatom, pigment and geochemical proxies in a lake sediment core. The sediments yielded radiocarbon dates between c. 26 650 and 28 750 14C yr BP (31 366–33 228 cal yr BP). This information can be used to constrain relative sea level adjacent to the Lambert Glacier at the end of Marine Isotope Stage 3. These data are compared with the age and altitude of Marine Isotope Stage 3 marine deposits elsewhere in East Antarctica and discussed with reference to late Quaternary ice sheet history and eustatic sea-level change
We present results of a multi-proxy study on marine sediment core JR179-PC466 recovered from the cre...
The Rauer Group is an archipelago in Prydz Bay, East Antarctica. The ice-free islands and the surrou...
Establishing accurate chronologies for Late Quaternary Antarctic marine sediments is often a challen...
We present a relative sea-level (RSL) history, constrained by AMS radiocarbon-dated marine–freshwate...
Little is known about the response of terrestrial East Antarctica to climate changes during the last...
Limited information on the East Antarctic Ice Sheet (EAIS) geometry during Marine Isotope Stage 3 (M...
Limited information on the East Antarctic Ice Sheet (EAIS) geometry during Marine Isotope Stage 3 (M...
Limited information on the East Antarctic Ice Sheet (EAIS) geometry during Marine Isotope Stage 3 (M...
The Lambert Glacier-Amery Ice Shelf system (LGAISS) is the largest outlet glacier system in East Ant...
An investigation was conducted during the austral summer, Jan.-Feb., 1972, at the east coast Liitzow...
A 100 cm long sediment sequence was recovered from Beaver Lake in Amery Oasis, East Antarctica, usin...
The reconstruction of past sea ice distribution in the Southern Ocean is crucial for an improved und...
In situ cosmogenic ¹⁰Be exposure dating, radiocarbon determinations, salt and sediment geochemistry,...
An investigation was conducted during the austral summer, Jan.-Feb., 1972, at the east coast Liitzow...
Antarctica's late Cenozoic (the past ∼15 million years) climate history is poorly known from direct ...
We present results of a multi-proxy study on marine sediment core JR179-PC466 recovered from the cre...
The Rauer Group is an archipelago in Prydz Bay, East Antarctica. The ice-free islands and the surrou...
Establishing accurate chronologies for Late Quaternary Antarctic marine sediments is often a challen...
We present a relative sea-level (RSL) history, constrained by AMS radiocarbon-dated marine–freshwate...
Little is known about the response of terrestrial East Antarctica to climate changes during the last...
Limited information on the East Antarctic Ice Sheet (EAIS) geometry during Marine Isotope Stage 3 (M...
Limited information on the East Antarctic Ice Sheet (EAIS) geometry during Marine Isotope Stage 3 (M...
Limited information on the East Antarctic Ice Sheet (EAIS) geometry during Marine Isotope Stage 3 (M...
The Lambert Glacier-Amery Ice Shelf system (LGAISS) is the largest outlet glacier system in East Ant...
An investigation was conducted during the austral summer, Jan.-Feb., 1972, at the east coast Liitzow...
A 100 cm long sediment sequence was recovered from Beaver Lake in Amery Oasis, East Antarctica, usin...
The reconstruction of past sea ice distribution in the Southern Ocean is crucial for an improved und...
In situ cosmogenic ¹⁰Be exposure dating, radiocarbon determinations, salt and sediment geochemistry,...
An investigation was conducted during the austral summer, Jan.-Feb., 1972, at the east coast Liitzow...
Antarctica's late Cenozoic (the past ∼15 million years) climate history is poorly known from direct ...
We present results of a multi-proxy study on marine sediment core JR179-PC466 recovered from the cre...
The Rauer Group is an archipelago in Prydz Bay, East Antarctica. The ice-free islands and the surrou...
Establishing accurate chronologies for Late Quaternary Antarctic marine sediments is often a challen...