[HTML][HTML] Rare earth elements in sedimentary phosphate deposits: solution to the global REE crisis?

P Emsbo, PI McLaughlin, GN Breit, EA du Bray… - Gondwana …, 2015 - Elsevier
The critical role of rare earth elements (REEs), particularly heavy REEs (HREEs), in high-
tech industries has created a surge in demand that is quickly outstripping known global …

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 …

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 …

[HTML][HTML] Marine 187Os/188Os isotope stratigraphy reveals the interaction of volcanism and ocean circulation during Oceanic Anoxic Event 2

ADC Du Vivier, D Selby, BB Sageman, I Jarvis… - Earth and Planetary …, 2014 - Elsevier
High-resolution osmium (Os) isotope stratigraphy across the Cenomanian–Turonian
Boundary Interval from 6 sections for four transcontinental settings has produced a record of …

[PDF][PDF] Does large igneous province volcanism always perturb the mercury cycle? Comparing the records of Oceanic Anoxic Event 2 and the end-Cretaceous to other …

LME Percival, HC Jenkyns, TA Mather… - American Journal of …, 2018 - ajsonline.org
Mercury (Hg) is increasingly being used as a sedimentary tracer of Large Igneous Province
(LIP) volcanism, and supports hypotheses of a coincidence between the formation of several …

Basalt‐seawater interaction, the Plenus Cold Event, enhanced weathering and geochemical change: deconstructing Oceanic Anoxic Event 2 (Cenomanian–Turonian …

HC Jenkyns, AJ Dickson, M Ruhl… - …, 2017 - Wiley Online Library
Abstract Oceanic Anoxic Event 2 (Cenomanian–Turonian: ca 94 Ma) represents a major
palaeoceanographic phenomenon that took place during an interval of extreme global …

Sedimentary mercury enrichments as a marker for submarine large igneous province volcanism? Evidence from the Mid‐Cenomanian event and Oceanic Anoxic …

JD Scaife, M Ruhl, AJ Dickson… - Geochemistry …, 2017 - Wiley Online Library
Abstract Oceanic Anoxic Event 2 (OAE 2), during the Cenomanian‐Turonian transition (∼
94 Ma), was the largest perturbation of the global carbon cycle in the mid‐Cretaceous and …

Decoupling of the carbon cycle during Ocean Anoxic Event 2

JS Eldrett, D Minisini, SC Bergman - Geology, 2014 - pubs.geoscienceworld.org
Abstract The Cenomanian to Turonian boundary transition (ca. 95–93 Ma) represents one of
the most profound global perturbations in the carbon cycle of the past 140 my This interval is …

The large-scale evolution of neodymium isotopic composition in the global modern and Holocene ocean revealed from seawater and archive data

K Tachikawa, T Arsouze, G Bayon, A Bory, C Colin… - Chemical …, 2017 - Elsevier
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 …

Obliquity forcing of organic matter accumulation during Oceanic Anoxic Event 2

SR Meyers, BB Sageman, MA Arthur - Paleoceanography, 2012 - Wiley Online Library
An analysis of orbitally influenced climate‐sensitive sedimentation is conducted across a
meridional transect of the proto‐North Atlantic, to reconstruct the behavior of the carbon …