Ann Holbourn mostly deals with Oceanography, Paleontology, Carbon cycle, Glacial period and Benthic zone. Her research investigates the connection between Oceanography and topics such as Climatology that intersect with issues in δ18O. Her work on Unconformity and Subsidence as part of general Paleontology study is frequently linked to Eccentricity, therefore connecting diverse disciplines of science.
Her studies in Carbon cycle integrate themes in fields like Carbonate compensation depth, Holocene climatic optimum and Isotopes of carbon. Her work carried out in the field of Glacial period brings together such families of science as Paleozoic, Sponge spicule, Seafloor spreading, Reef and Upwelling. Her Benthic zone study focuses on Foraminifera in particular.
Ann Holbourn mainly investigates Oceanography, Paleontology, Benthic zone, Sediment core and Foraminifera. The various areas that Ann Holbourn examines in her Oceanography study include Glacial period and Climatology. Her Climatology study frequently draws connections to adjacent fields such as Throughflow.
Her Paleontology study integrates concerns from other disciplines, such as Sea level and Table. Her research in Sediment core intersects with topics in Sea surface temperature, Hydrology, Geochemistry, Isotopes of oxygen and Mineralogy. Her research brings together the fields of Plankton and Foraminifera.
Her primary areas of investigation include Oceanography, Sediment core, Benthic zone, Geochemistry and Isotopes of oxygen. Her Late Miocene research extends to Oceanography, which is thematically connected. Her Benthic zone research is multidisciplinary, incorporating elements of Bottom water and Paleontology.
Her studies deal with areas such as Global cooling and Total organic carbon as well as Paleontology. Her Geochemistry research focuses on subjects like Structural basin, which are linked to Isotope analysis. Ann Holbourn has researched Isotopes of oxygen in several fields, including Environmental chemistry, Sea surface temperature, Pulleniatina obliquiloculata and Cibicidoides wuellerstorfi.
Ann Holbourn spends much of her time researching Oceanography, Paleontology, Benthic zone, Glacial period and Foraminifera. Ann Holbourn regularly ties together related areas like International Ocean Discovery Program in her Oceanography studies. Her Paleontology research includes themes of Global cooling and Total organic carbon.
Her Benthic zone research integrates issues from Bottom water, Range and Isotopes of oxygen. Her biological study spans a wide range of topics, including Pleistocene and Ice sheet. Her Foraminifera research is multidisciplinary, incorporating perspectives in Salinity, Greenhouse gas and Paleoceanography.
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An astronomically dated record of Earth's climate and its predictability over the last 66 million years.
Thomas Westerhold;Norbert Marwan;Norbert Marwan;Anna Joy Drury;Anna Joy Drury;Diederik Liebrand.
Impacts of orbital forcing and atmospheric carbon dioxide on Miocene ice-sheet expansion
Ann E L Holbourn;Wolfgang Kuhnt;Michael Schulz;Helmut Erlenkeuser.
Orbitally-paced climate evolution during the middle Miocene “Monterey” carbon-isotope excursion
Ann E L Holbourn;Wolfgang Kuhnt;Michael Schulz;José Abel Flores.
Earth and Planetary Science Letters (2007)
A Cenozoic record of the equatorial Pacific carbonate compensation depth
Heiko Pälike;Mitchell W. Lyle;Hiroshi Nishi;Isabella Raffi.
Neogene History of the Indonesian Throughflow
Wolfgang Kuhnt;Ann Holbourn;Robert Hall;Mafia Zuvela.
Geophysical monograph (2004)
Atlas of Benthic Foraminifera
Ann E. L. Holbourn;Andrew S. Henderson;Norman MacLeod.
Middle Miocene climate cooling linked to intensification of eastern equatorial Pacific upwelling
Ann Holbourn;Wolfgang Kuhnt;Mitch Lyle;Leah Schneider.
Global perturbation of the carbon cycle at the onset of the Miocene Climatic Optimum
Ann Holbourn;Wolfgang Kuhnt;Karlos G.D. Kochhann;Nils Andersen.
Changes in the thermocline structure of the Indonesian outflow during Terminations I and II
Jian Xu;Ann Holbourn;Wolfgang Kuhnt;Zhimin Jian.
Earth and Planetary Science Letters (2008)
Middle to late Miocene stepwise climate cooling: Evidence from a high-resolution deep water isotope curve spanning 8 million years
Ann Holbourn;Wolfgang Kuhnt;Steven Clemens;Warren Prell.
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