We investigated the distinctive shallow sub-surface hydrology of the southwest Western Australia (SWWA) dune calcarenite using observed rainfall and rainfall δ18O; soil moisture, cave drip rate and dripwater δ18O over a six-year period: August 2005-Mar
Speleothems (cave deposits), used for palaeoenvironmental reconstructions, are deposited from cave d...
We report the results of the first multi-year monitoring and modelling study of the isotopic composi...
Groundwater resources are a reliable and important source of water. Considering most large groundwat...
We investigated the distinctive shallow sub-surface hydrology of the southwest Western Australia (SW...
There is an identified need to extend our baseline climate information beyond the relatively short d...
Speleothems from Golgotha Cave in SW Western Australia have been investigated to extend our knowledg...
Milankovitch-scale Quaternary climatic oscillations within south-east Australia are known to be char...
Southwest Western Australia (SWWA) experienced a clear climatic change during the late 20thC and has...
Speleothems are an important archive of paleoenvironmental information but a thorough understanding ...
Cave monitoring provides a crucial link between hydrological and climate processes and how they may ...
Paleoclimate studies are an important tool to aid our current knowledge and understanding of past cl...
We present a record of seasonal and inter-annual oxygen (δO) and carbon (δC) isotope ratios from an ...
Speleothem trace element time series are constructed from the infiltrating drip water geochemistry, ...
Oxygen isotope ratios in speleothems may be affected by external processes that are independent of c...
Palaeoclimate reconstruction is crucial for understanding past variability in Earth’s climate system...
Speleothems (cave deposits), used for palaeoenvironmental reconstructions, are deposited from cave d...
We report the results of the first multi-year monitoring and modelling study of the isotopic composi...
Groundwater resources are a reliable and important source of water. Considering most large groundwat...
We investigated the distinctive shallow sub-surface hydrology of the southwest Western Australia (SW...
There is an identified need to extend our baseline climate information beyond the relatively short d...
Speleothems from Golgotha Cave in SW Western Australia have been investigated to extend our knowledg...
Milankovitch-scale Quaternary climatic oscillations within south-east Australia are known to be char...
Southwest Western Australia (SWWA) experienced a clear climatic change during the late 20thC and has...
Speleothems are an important archive of paleoenvironmental information but a thorough understanding ...
Cave monitoring provides a crucial link between hydrological and climate processes and how they may ...
Paleoclimate studies are an important tool to aid our current knowledge and understanding of past cl...
We present a record of seasonal and inter-annual oxygen (δO) and carbon (δC) isotope ratios from an ...
Speleothem trace element time series are constructed from the infiltrating drip water geochemistry, ...
Oxygen isotope ratios in speleothems may be affected by external processes that are independent of c...
Palaeoclimate reconstruction is crucial for understanding past variability in Earth’s climate system...
Speleothems (cave deposits), used for palaeoenvironmental reconstructions, are deposited from cave d...
We report the results of the first multi-year monitoring and modelling study of the isotopic composi...
Groundwater resources are a reliable and important source of water. Considering most large groundwat...