We use all available chronostratigraphic constraints - biostratigraphy, magnetostratigraphy, radioisotopic dates, strontium-isotope stratigraphy, and correlation of compositional and physical properties to well-dated global or regional records - to construct a preliminary age model for ANDRILL SMS Project's AND-2A drillcore (77°45.488'S, 165°16.605'E, 383.57 m water depth). These diverse chronostratigraphic constraints are consistent with each other and are distributed throughout the 1138.54 m-thick section, resulting in a well-constrained age model. The sedimentary succession comprises a thick early and middle Miocene section below 224.82 mbsf and a condensed middle/late Miocene to Recent section above this. The youngest sediments are Brun...
During the austral spring of 2007, the Southern McMurdo (SMS) Project recovered a 1138.54 meter lo...
The ANDRILL Southern McMurdo Sound (SMS) Project was carried out in December of 2007 by an internati...
The Integrated Ocean Drilling Program Expedition 318 to the Wilkes Land margin of Antarctica recover...
We use all available chronostratigraphic constraints - biostratigraphy, magnetostratigraphy, radiois...
We use all available chronostratigraphic constraints – biostratigraphy, magnetostratigraphy, radioi...
Chronostratigraphic data available for the preliminary age model for the upper 700 m for the AND-1B ...
Chronostratigraphic data available for the preliminary age model for the upper 700 m for the AND-1B ...
Present understanding of Antarctic climate change during the Early to Mid-Miocene, including major c...
The 624.15 m glaciomarine sedimentary succession recovered in the CRP-2/2A drillcore comprises lower...
The lowest 501 m (similar to 1139-638 m) of the AND-2A core from southern Mc-Murdo Sound is the most...
An 823 m thick glaciomarine Cenozoic section sitting unconformably on the Lower Devonian Beacon Supe...
The ANDRILL Program successfully recovered a 1285 m-long succession of cyclic glacimarine sediment w...
New paleomagnetic results from lower-to-middle Miocene samples from Ocean Drilling Program (ODP) Hol...
During the austral spring of 2007, the Southern McMurdo (SMS) Project recovered a 1138.54 meter lo...
The ANDRILL Southern McMurdo Sound (SMS) Project was carried out in December of 2007 by an internati...
The Integrated Ocean Drilling Program Expedition 318 to the Wilkes Land margin of Antarctica recover...
We use all available chronostratigraphic constraints - biostratigraphy, magnetostratigraphy, radiois...
We use all available chronostratigraphic constraints – biostratigraphy, magnetostratigraphy, radioi...
Chronostratigraphic data available for the preliminary age model for the upper 700 m for the AND-1B ...
Chronostratigraphic data available for the preliminary age model for the upper 700 m for the AND-1B ...
Present understanding of Antarctic climate change during the Early to Mid-Miocene, including major c...
The 624.15 m glaciomarine sedimentary succession recovered in the CRP-2/2A drillcore comprises lower...
The lowest 501 m (similar to 1139-638 m) of the AND-2A core from southern Mc-Murdo Sound is the most...
An 823 m thick glaciomarine Cenozoic section sitting unconformably on the Lower Devonian Beacon Supe...
The ANDRILL Program successfully recovered a 1285 m-long succession of cyclic glacimarine sediment w...
New paleomagnetic results from lower-to-middle Miocene samples from Ocean Drilling Program (ODP) Hol...
During the austral spring of 2007, the Southern McMurdo (SMS) Project recovered a 1138.54 meter lo...
The ANDRILL Southern McMurdo Sound (SMS) Project was carried out in December of 2007 by an internati...
The Integrated Ocean Drilling Program Expedition 318 to the Wilkes Land margin of Antarctica recover...