The Miocene: The future of the past
M Steinthorsdottir, HK Coxall… - Paleoceanography …, 2021 - Wiley Online Library
Abstract The Miocene epoch (23.03–5.33 Ma) was a time interval of global warmth, relative
to today. Continental configurations and mountain topography transitioned toward modern …
to today. Continental configurations and mountain topography transitioned toward modern …
[HTML][HTML] The Eocene–Oligocene transition: a review of marine and terrestrial proxy data, models and model–data comparisons
Abstract The Eocene–Oligocene transition (EOT) was a climate shift from a largely ice-free
greenhouse world to an icehouse climate, involving the first major glaciation of Antarctica …
greenhouse world to an icehouse climate, involving the first major glaciation of Antarctica …
The rise and fall of the Cretaceous Hot Greenhouse climate
BT Huber, KG MacLeod, DK Watkins… - Global and Planetary …, 2018 - Elsevier
A compilation of foraminiferal stable isotope measurements from southern high latitude
(SHL) deep-sea sites provides a novel perspective important for understanding Earth's …
(SHL) deep-sea sites provides a novel perspective important for understanding Earth's …
Global extent of early Eocene hyperthermal events: A new Pacific benthic foraminiferal isotope record from Shatsky Rise (ODP Site 1209)
T Westerhold, U Röhl, B Donner… - Paleoceanography and …, 2018 - Wiley Online Library
Studying the dynamics of past global warming events during the late Paleocene to middle
Eocene informs our understanding of Earth's carbon cycle behavior under elevated …
Eocene informs our understanding of Earth's carbon cycle behavior under elevated …
Descent toward the Icehouse: Eocene sea surface cooling inferred from GDGT distributions
The TEX86 proxy, based on the distribution of marine isoprenoidal glycerol dialkyl glycerol
tetraether lipids (GDGTs), is increasingly used to reconstruct sea surface temperature (SST) …
tetraether lipids (GDGTs), is increasingly used to reconstruct sea surface temperature (SST) …
Climate transition at the Eocene–Oligocene influenced by bathymetric changes to the Atlantic–Arctic oceanic gateways
The Eocene–Oligocene Transition (∼ 33.9 Ma) marks the largest step transformation within
the Cenozoic cooling trend and is characterized by a sudden growth of the Antarctic ice …
the Cenozoic cooling trend and is characterized by a sudden growth of the Antarctic ice …
Earth system changes during the cooling greenhouse phase of the Late Cretaceous: Coniacian-Santonian OAE3 subevents and fundamental variations in organic …
A Mansour, M Wagreich - Earth-Science Reviews, 2022 - Elsevier
Abstract The Coniacian-Santonian (CS) was a time of differentiation in marine
sedimentation, characterized by organic carbon (OC)-rich black shales and carbonates …
sedimentation, characterized by organic carbon (OC)-rich black shales and carbonates …
[HTML][HTML] Global Cenozoic paleobathymetry with a focus on the Northern Hemisphere oceanic gateways
The evolution of the Northern Hemisphere oceanic gateways has facilitated ocean
circulation changes and may have influenced climatic variations in the Cenozoic time (66 …
circulation changes and may have influenced climatic variations in the Cenozoic time (66 …
The large-scale evolution of neodymium isotopic composition in the global modern and Holocene ocean revealed from seawater and archive data
Abstract Neodymium isotopic compositions (143 Nd/144 Nd or ε Nd) have been used as a
tracer of water masses and lithogenic inputs to the ocean. To further evaluate the …
tracer of water masses and lithogenic inputs to the ocean. To further evaluate the …
Atlantic-Pacific asymmetry in deep water formation
D Ferreira, P Cessi, HK Coxall… - Annual Review of …, 2018 - annualreviews.org
While the Atlantic Ocean is ventilated by high-latitude deep water formation and exhibits a
pole-to-pole overturning circulation, the Pacific Ocean does not. This asymmetric global …
pole-to-pole overturning circulation, the Pacific Ocean does not. This asymmetric global …