| Title | Author(s) | Publication | DOI | View cores |
|---|---|---|---|---|
| Holocene sea-level change and ice-sheet history in the Vestfold Hills, East Antarctica | Zwartz, Dan and Bird, Michael and Stone, John and Lambeck, Kurt | Earth and Planetary Science Letters, 1998 | 10.1016/S0012-821X(97)00204-5 |
|
| Sedimentological and stable-isotope evolution of lakes in the Vestfold Hills, Antarctica | Bird, Michael I and Chivas, Allan R and Radnell, Christopher J and Burton, Harry R | Palaeogeography, Palaeoclimatology, Palaeoecology, 1991 | 10.1016/0031-0182(91)90039-T |
|
| Non-Core name | Region | Landform type | Comments | |
|---|---|---|---|---|
| Ace Lake | Antarctica, East Antarctica |
| Sample ID | Core depth (m) |
Lithology | Facies interpretation | Carbon type | Sample preparation type | Age (14C yr ± 1σ) | Calibrated age, median probability (cal. yr BP) | Calibrated age, 2σ range (cal. yr BP) | Comments |
|---|---|---|---|---|---|---|---|---|---|
| ace_Llm | None - None | Not Lithology Reported | No Facies Interpretation Reported | Lacustrine to marine sediment | None | ± | Calibrated age for default reservoir correction not available | Derived lacustrine to marine transition. Dated by lacustrine sediment | |
| ace_Lml | None - None | Not Lithology Reported | No Facies Interpretation Reported | Marine to lacustrine | None | ± | Calibrated age for default reservoir correction not available | Derived marine to lacustrine transition. Dated by lacustrine sediment | |
| ANU-6419 | None - None | Not Lithology Reported | No Facies Interpretation Reported | Unknown | None | ± | Calibrated age for default reservoir correction not available | Marine. Age older than timing of recent isolation. Younger than previous transition from lacustrine to marine. | |
| ANU-8166 | None - None | Not Lithology Reported | No Facies Interpretation Reported | Unknown | None | ± | Calibrated age for default reservoir correction not available | Lacustrine. Age older than timing of lacustrine to marine conditions. |
No associated documents.