Amino acid-based geochronological analyses were carried out on fossil mollusc shell and foraminifera from Unit 3.1, Cape Roberts Project core CRP-1. Ratios of D-alloIsoleucine to L-Isoleucine (D/L) were measured from 19 fossil samples using cation exchange High Performance Liquid Chromatography (HPLC) methods. Preliminary interpretation of these results suggest that Unit 3.1 contains carbonate fossils having multiple ages. The interpreted ages have a bimodal distribution between ~220 Ka (Quaternary) and ~2.4 Ma (Pliocene). However, these results lack a comprehensive regional and taxonomic context for amino acid studies in Antarctica and therefore should be regarded as preliminary age estimates of fossil shell ages
Numerical ages derived from amino acid racemization (AAR) geochronology are typically based on calib...
Amino acid racemization (AAR) geochronology is a powerful tool for dating Quaternary marine sediment...
Numerical ages derived from amino acid racemization (AAR) geochronology are typically based on calib...
In this study, we demonstrate the utility of amino acid geochronology based on single-foraminiferal ...
[1] In this study, we demonstrate the utility of amino acid geochronology based on single-foramini...
AbstractAminostratigraphic studies of continental deposits in the UK have hitherto relied almost exc...
Sea-level records of past interglacials are important archives for understanding long term mechanism...
Amino acid racemisation (AAR) analyses (total acid hydrolysate) on the fossil bivalve molluscs, Pect...
Calibrated amino acid racemisation methods allow paleobiologists to quantify the age distributions o...
Shell middens are one of the most important and widespread indicators for human exploitation of mari...
The deep-sea environment is among the most stable on Earth, making it well suited for amino acid geo...
AbstractShell middens are one of the most important and widespread indicators for human exploitation...
While amino acid (AA) geochronology has been widely applied to foraminiferal biomineral proteins, th...
Marine and ice-core records show that the Earth has experienced a succession of glacials and intergl...
Numerical ages derived from amino acid racemization (AAR) geochronology are typically based on calib...
Numerical ages derived from amino acid racemization (AAR) geochronology are typically based on calib...
Amino acid racemization (AAR) geochronology is a powerful tool for dating Quaternary marine sediment...
Numerical ages derived from amino acid racemization (AAR) geochronology are typically based on calib...
In this study, we demonstrate the utility of amino acid geochronology based on single-foraminiferal ...
[1] In this study, we demonstrate the utility of amino acid geochronology based on single-foramini...
AbstractAminostratigraphic studies of continental deposits in the UK have hitherto relied almost exc...
Sea-level records of past interglacials are important archives for understanding long term mechanism...
Amino acid racemisation (AAR) analyses (total acid hydrolysate) on the fossil bivalve molluscs, Pect...
Calibrated amino acid racemisation methods allow paleobiologists to quantify the age distributions o...
Shell middens are one of the most important and widespread indicators for human exploitation of mari...
The deep-sea environment is among the most stable on Earth, making it well suited for amino acid geo...
AbstractShell middens are one of the most important and widespread indicators for human exploitation...
While amino acid (AA) geochronology has been widely applied to foraminiferal biomineral proteins, th...
Marine and ice-core records show that the Earth has experienced a succession of glacials and intergl...
Numerical ages derived from amino acid racemization (AAR) geochronology are typically based on calib...
Numerical ages derived from amino acid racemization (AAR) geochronology are typically based on calib...
Amino acid racemization (AAR) geochronology is a powerful tool for dating Quaternary marine sediment...
Numerical ages derived from amino acid racemization (AAR) geochronology are typically based on calib...