Climate evolution through the onset and intensification of Northern Hemisphere Glaciation
Abstract The Pliocene Epoch (∼ 5.3–2.6 million years ago, Ma) was characterized by a
warmer than present climate with smaller Northern Hemisphere ice sheets, and offers an …
warmer than present climate with smaller Northern Hemisphere ice sheets, and offers an …
Coccolithophore cell biology: chalking up progress
AR Taylor, C Brownlee… - Annual review of marine …, 2017 - annualreviews.org
Coccolithophores occupy a special position within the marine phytoplankton because of
their production of intricate calcite scales, or coccoliths. Coccolithophores are major …
their production of intricate calcite scales, or coccoliths. Coccolithophores are major …
[图书][B] Planktic foraminifers in the modern ocean
R Schiebel, C Hemleben - 2017 - Springer
The purpose of this book is to provide timely and comprehensive information on extant
planktic foraminifers. This book is based on 'Modern Planktonic Foraminifera'published by …
planktic foraminifers. This book is based on 'Modern Planktonic Foraminifera'published by …
[HTML][HTML] The DeepMIP contribution to PMIP4: Methodologies for selection, compilation and analysis of latest Paleocene and early Eocene climate proxy data …
CJ Hollis, T Dunkley Jones… - Geoscientific Model …, 2019 - gmd.copernicus.org
The early Eocene (56 to 48 million years ago) is inferred to have been the most recent time
that Earth's atmospheric CO 2 concentrations exceeded 1000 ppm. Global mean …
that Earth's atmospheric CO 2 concentrations exceeded 1000 ppm. Global mean …
Trace element proxies for surface ocean conditions: A synthesis of culture calibrations with planktic foraminifera
The trace element composition of planktic foraminiferal calcite provides a useful means of
determining past surface ocean conditions. We have assembled the results of culture …
determining past surface ocean conditions. We have assembled the results of culture …
Planktic foraminifera form their shells via metastable carbonate phases
The calcium carbonate shells of planktic foraminifera provide our most valuable
geochemical archive of ocean surface conditions and climate spanning the last 100 million …
geochemical archive of ocean surface conditions and climate spanning the last 100 million …
Making the otolith magnesium chemical calendar-clock tick: plausible mechanism and empirical evidence
KE Limburg, MJ Wuenschel, K Hüssy… - Reviews in Fisheries …, 2018 - Taylor & Francis
The incorporation of a number of readily measured trace elements into otoliths is considered
to be under some sort of physiological control, but rarely are explicit mechanisms proposed …
to be under some sort of physiological control, but rarely are explicit mechanisms proposed …
Nanometer-scale chemistry of a calcite biomineralization template: Implications for skeletal composition and nucleation
Plankton, corals, and other organisms produce calcium carbonate skeletons that are integral
to their survival, form a key component of the global carbon cycle, and record an archive of …
to their survival, form a key component of the global carbon cycle, and record an archive of …
Stable oxygen isotopes and Mg/Ca in planktic foraminifera from modern surface sediments of the Western Pacific Warm Pool: Implications for thermocline …
Mg/Ca and stable oxygen isotope compositions (δ18O) of planktic foraminifera tests are
commonly used as proxies to reconstruct past ocean conditions including variations in the …
commonly used as proxies to reconstruct past ocean conditions including variations in the …
Insights from fossil-bound nitrogen isotopes in diatoms, foraminifera, and corals
Nitrogen is a major limiting element for biological productivity, and thus understanding past
variations in nitrogen cycling is central to understanding past and future ocean …
variations in nitrogen cycling is central to understanding past and future ocean …