​​​​​​​ Late Paleocene deposition of an organic-rich sedimentary facies on the
continental shelf and slope of New Zealand and eastern Australia has been linked to short …

Abstract The 7% carbon-13 depletion in cold water phytoplankton provides a striking signal
that is traceable in deep-sea cores taken in high latitude regions of the Southern …

The timing and magnitude of carbon isotope excursions is essential for understanding the
global transfer of carbon among the oceansland, and atmosphere. Numerous studies have …

Abstract The Cretaceous/Paleogene (K/Pg) boundary is well-represented across a range of
depositional settings in New Zealand. Trends in fossil assemblages and marine lithofacies …

Paleogene strata throughout much of the southwest Pacific is comprised of thick
successions of fine-grained siliceous to calcareous sediments. However, during the Late …

A distinctive organic-rich marine mudstone of Late Paleocene age occurs in most of New
Zealand's sedimentary basins and has been identified as a potential source rock for oil and …

C 3 land plants dominated the Paleozoic landscape since the Devonian and played an
essential role in enhancing continental chemical weathering. Vast amount of organic carbon …

Holocene sediments buried on the continental shelf seaward of the Waipaoa River,
northeastern New Zealand, preserve a stratigraphic record of terrestrial environmental …

Abstract During the Middle Miocene, Earth's climate transitioned from a relatively warm
phase (Miocene climatic optimum) to a colder mode with reestablishment of permanent ice …

Carbon-isotope measurements (δ13C) of leaf-wax n-alkanes from the Paleocene–Eocene
Thermal Maximum (PETM) in the Bighorn Basin, Wyoming, reveal a negative carbon isotope …