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Input of particulate organic and dissolved inorganic carbon from the Amazon to t...
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Detrital zircon ages in Buller and Takaka terranes, New Zealand: constraints on...
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Detrital zircon ages in Buller and Takaka terranes, New Zealand: constraints on...
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Detrital zircon ages in Buller and Takaka terranes, New Zealand: constraints on...
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Palynological evidence for Holocene environmental change and uplift on Wireless...
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On the use of electromagnetic induction sounding to determine winter and spring...
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Hill Slope Variations in Chlorophyll Fluorescence Indices and Leaf Traits in a S...
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Linking the incidence and age patterns of clinical malaria to parasite prevalenc...
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Diamond, subcalcic garnet, and mantle metasomatism: Kimberlite sampling patterns...
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Moissanite (SiC) from kimberlites:Polytypes, trace elements, inclusions and spec...
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Sr-Isotope chronostratigraphy of Paleogene-Neogene marine deposits: Austral Basi...
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How Do Global Weather Patterns Influence Days Suitable for Fieldwork
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Accumulation of marine microplastics along a trophic gradient as determined by a...
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East Antarctic sources of extensive Lower–Middle Ordovician turbidites in the La...
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Herschel and beyond: FIR and submillimetre space missions and possible synergies...
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Twenty one years of 1km resolution AVHRR Sea Surface Temperature data over the A...
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Oxygen and carbon isotope evidence for seawater-hydrothermal alteration of the M...
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Sr-isotope chronostratigraphy of Paleogene-Neogene marine deposits: Austral Basi...
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How Do Global Weather Patterns Influence Days Suitable for Fieldwork
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Borers and encrusters as indicators of the presence of hermit crabs in Antarctic...
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