For more than half a century, microfossils–especially foraminifera–have been widely used
as stratigraphic markers and paleoenvironmental indicators. Although increasing emphasis …

Five major planktonic and benthic foraminiferal extinction events occurred during the past
100 my: at the Cenomanian/Turonian (CT) boundary, at the Cretaceous/Tertiary (KT) …

The 77 m sediment core from Firth of Tay provides complete record of glacial retreat and
Holocene climate change on the Weddell Sea side of the Antarctic Peninsula that began …

In the late Paleocene to early Eocene, deep sea benthic foraminifera suffered their only
global extinction of the last 75 million years and diversity decreased worldwide by 30–50 …

Four cores raised from the eastern Norwegian Sea and adjacent Norwegian fjords at sites
influenced by Atlantic water have been investigated. Oxygen isotope analyses in benthic …

Foraminifer tests are prone to diagenetic recrystallization on a micron scale that can affect
their geochemical composition, hence it is important to identify fossil material that is well …

A high-resolution (∼ 4–5cm/kyr) giant piston core record (MD962085) retrieved during an
IMAGES II-NAUSICAA cruise from the continental slope of the southeast Atlantic Ocean …

The sensitivities of benthic foraminiferal Mg/Ca and Li/Ca to bottom water temperature and
carbonate saturation state have recently been assessed. Here we present a new approach …

We used modern epibenthic foraminifer tests of Cibicidoides mundulus and Planulina
wuellerstorfi from South Atlantic core top sediments in order to establish Mg/Ca‐temperature …

Bathyal benthic foraminifera and stable isotopes from the Caravaca and Zumaya sections of
Spain, indicate that the mass extinction near the Paleocene/Eocene (P/E) boundary (upper …