[HTML][HTML] Climate model and proxy data constraints on ocean warming across the Paleocene–Eocene Thermal Maximum
Constraining the greenhouse gas forcing, climatic warming and estimates of climate
sensitivity across ancient large transient warming events is a major challenge to the …
sensitivity across ancient large transient warming events is a major challenge to the …
Synchronous tropical and polar temperature evolution in the Eocene
Palaeoclimate reconstructions of periods with warm climates and high atmospheric CO2
concentrations are crucial for develo** better projections of future climate change. Deep …
concentrations are crucial for develo** better projections of future climate change. Deep …
The accuracy of mid-Pliocene δ18O-based ice volume and sea level reconstructions
Understanding the sensitivity of the polar ice caps to a modest global warming (2–3° C
above preindustrial) is of paramount importance if we are to accurately predict future sea …
above preindustrial) is of paramount importance if we are to accurately predict future sea …
[HTML][HTML] The DeepMIP contribution to PMIP4: Methodologies for selection, compilation and analysis of latest Paleocene and early Eocene climate proxy data …
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 …
[BUCH][B] Carbonate reservoirs: Porosity and diagenesis in a sequence stratigraphic framework
CH Moore, WJ Wade - 2013 - books.google.com
The 2nd Edition of Carbonate Reservoirs aims to educate graduate students and industry
professionals on the complexities of porosity evolution in carbonate reservoirs. In the …
professionals on the complexities of porosity evolution in carbonate reservoirs. In the …
Late Cretaceous–Neogene trends in deep ocean temperature and continental ice volume: Reconciling records of benthic foraminiferal geochemistry (δ18O and Mg …
We reconstruct trends in ice volume and deep ocean temperature for the past 108 Myr,
resolving variations on timescales of∼ 2 Myr and longer. We use a sea level record as a …
resolving variations on timescales of∼ 2 Myr and longer. We use a sea level record as a …
[HTML][HTML] Constraining the evolution of Neogene ocean carbonate chemistry using the boron isotope pH proxy
Over the course of the Neogene, the Earth underwent profound climatic shifts from the
sustained warmth of the middle Miocene to the development of Plio-Pleistocene glacial …
sustained warmth of the middle Miocene to the development of Plio-Pleistocene glacial …
Early Paleogene temperature history of the Southwest Pacific Ocean: Reconciling proxies and models
We present a new multiproxy (TEX86, δ18O and Mg/Ca), marine temperature history for
Canterbury Basin, eastern New Zealand, that extends from middle Paleocene to middle …
Canterbury Basin, eastern New Zealand, that extends from middle Paleocene to middle …
Ocean carbon storage across the middle Miocene: A new interpretation for the Monterey Event
Abstract The Miocene Climatic Optimum (MCO, 14–17 Ma) was~ 3–4° C warmer than
present, similar to estimates for 2100. Coincident with the MCO is the Monterey positive …
present, similar to estimates for 2100. Coincident with the MCO is the Monterey positive …
Late Miocene cooling coupled to carbon dioxide with Pleistocene-like climate sensitivity
Earth's climate cooled markedly during the late Miocene from 12 to 5 million years ago, with
far-reaching consequences for global ecosystems. However, the driving forces of these …
far-reaching consequences for global ecosystems. However, the driving forces of these …