Planktic foraminifera are commonly used for first-order age control in deep-sea sediments
from low-latitude regions based on a robust tropical–subtropical zonation scheme. Although …

Abstract The Late Miocene-Early Pliocene Biogenic Bloom (ca. 9.0–3.5 Ma) was a phase of
high marine biological productivity documented globally at multiple ocean sites, related to …

The absolute position during the Cenozoic of northern Zealandia, a continent that lies more
than 90% submerged in the southwest Pacific Ocean, is inferred from global plate motion …

Abstract International Ocean Discovery Program (IODP) Expedition 371 drilled six sites in
the Tasman Sea of the southwest Pacific between 27 July and 26 September 2017. The …

Modern and fossil benthic foraminifera have been widely documented from New Zealand,
but detailed studies of material collected from drilling expeditions in the Tasman Sea are …

International Ocean Discovery Program (IODP) Expedition 392 Site U1579 is located on the
shallowest part of the central Agulhas Plateau (39° 57.0725′ S, 26° 14.1793′ E) at 2492 …

A key objective of Expedition 396 was to constrain the role of breakup volcanism on the
Paleocene–Eocene Thermal Maximum (PETM). For a long time, it has been argued that …

This chapter outlines the procedures and methods employed for coring and drilling
operations as well as in the various shipboard laboratories of the R/V JOIDES Resolution …

Abstract The Late Lutetian Thermal Maximum (LLTM) was a transient and brief global
warming event recorded in the middle Eocene, at 41.52 Ma. The biotic response to the LLTM …

Abstract The Late Miocene-Early Pliocene Biogenic Bloom (9.0–3.5 Ma) is a widespread
paleoceanographic phenomenon marked by increased marine biological productivity and …