The trace element (TE) and isotopic composition of calcareous foraminifera has been
invaluable in advancing our understanding of environmental change throughout the …

Abstract The El Niño Southern Oscillation (ENSO) is highly dependent on coupled
atmosphere-ocean interactions and feedbacks, suggesting a tight relationship between …

The trace element and isotopic composition of foraminifera shells are widely used in
paleoceanography to reconstruct past ocean conditions. Individual foraminifer analysis (IFA) …

Modern observations have presented linkages between subsurface waters of the western
Pacific warm pool and both El Niño/Southern Oscillation-related and extratropic-controlled …

Marine heatwaves (MHWs) are warm sea surface temperature (SST) anomalies with
substantial ecological and economic consequences. Observations of MHWs are based on …

Particle mixing by benthic fauna beneath the sediment‐water interface (or bioturbation)
fundamentally challenges the proxy based retrieval of past climatic conditions from deep …

Abstract Changes in vertical geochemical gradients within the Western Pacific Warm Pool
(WPWP) are important indicators of the region's upper ocean response to climate changes …

Under future climate scenarios, ocean temperatures that are presently extreme and qualify
as marine heatwaves (MHW) are forecasted to increase in frequency and intensity, but little …

We use a single foraminifera enabled, holistic hydroclimate-to-sediment transient modelling
approach to fundamentally evaluate the efficacy of discrete-depth individual foraminifera …

The equatorial Pacific is a nexus of key oceanic and atmospheric phenomena, and its
regional climate has critical implications for hydroclimate, the partitioning of CO 2, and …