Results 71 to 80 of about 145,521 (218)

Millennial‐Scale Deoxygenation in the Southern California Oxygen Minimum Zone Over the Last Glacial Cycle

open access: yesGeophysical Research Letters, Volume 53, Issue 20, 28 October 2026.
Abstract Past variability of oxygen minimum zones (OMZs) provides key insights into future ocean deoxygenation. However, California margin OMZ records remain temporally limited, restricting evaluation of mechanisms across full glacial–interglacial cycles.
Fang Qian   +4 more
wiley   +1 more source

Valanginian to Barremian Benthic Foraminifera from ODP Site 766 (Leg 123, Indian Ocean) [PDF]

open access: yes, 1995
A Valanginian to Barremian bathyal foraminiferal assemblage (118 taxa belonging to 51 genera) is documented from ODP Site 766, drilled near the foot of the Exmouth Plateau off northwest Australia.
Holbourn, A.E.L., Kaminski, M.A.
core  

Foraminifera from the Campanian–Maastrichtian of the Miriri Sub-Basin, Paraíba Basin, Brazil: implications for biostratigraphy and paleoenvironmental reconstruction [PDF]

open access: yesAnais da Academia Brasileira de Ciências
This study investigates the core RT-01-PB from the Miriri Sub-Basin, Paraíba Basin, analyzing planktic and benthic foraminifera from the upper Campanian to lower Maastrichtian. The strata belong to the Itamaracá and Gramame formations. Lithostratigraphic,
HOLES P. DE SANTANA   +4 more
doaj   +1 more source

Evidence for Submarine Landslides at Climate Transitions in a High Arctic Fjord (Grise Fiord, Nunavut)

open access: yesEarth Surface Processes and Landforms, Volume 51, Issue 10, October 2026.
Seafloor mapping in a high Arctic fjord (Grise Fiord) revealed many submarine landslides triggered by iceberg groundings, coastal debris flows and delta collapses. The dating of three of them suggests that they occurred at past climate transitions. ABSTRACT Arctic fjords are experiencing rapid environmental change driven by amplified high‐latitude ...
C. Stancu   +11 more
wiley   +1 more source

Benthic foraminifera factors of sediment core M5/2_91MC

open access: yes, 2001
Benthic foraminifera factors of sediment core M5 ...
Edelman-Furstenberg, Yael   +7 more
core   +1 more source

Field settlement trap designs for Cassiopea spp. polyp recruitment: A preliminary study

open access: yesLimnology and Oceanography: Methods, Volume 24, Issue 10, October 2026.
Abstract High densities of upside‐down jellyfish (Cassiopea spp.) have been documented in anthropogenically disturbed coastal ecosystems including Jobos Bay, Puerto Rico. However, understanding their field ecology remains limited because most studies are laboratory‐based, focusing on life history and symbiotic relationships.
Natalia B. López‐Figueroa   +11 more
wiley   +1 more source

Relative abundances of benthic foraminifera in surface sediments (Table A3)

open access: yes, 2003
Relative abundances of benthic foraminifera in surface sediments (Table ...
Wenzhöfer, Frank   +9 more
core   +1 more source

Sea Surface Conditions and Antarctic Bottom Water Formation Offshore Cape Darnley, East Antarctica, Over the Last 600 ka: New Insights From the Diatom Record

open access: yesPaleoceanography and Paleoclimatology, Volume 41, Issue 10, October 2026.
Abstract The Cape Darnley marine region of East Antarctica is one of only four sectors where Antarctic Bottom Water (AABW) is produced. AABW formation at Cape Darnley is highly dependent on surface ocean processes—specifically, the high production of frazil ice. Here, we investigated the sea surface conditions at Cape Darnley over the past 600 thousand
M. Husdell   +10 more
wiley   +1 more source

(Table S2) Factor score matrix of benthic foraminifera assemblage

open access: yes, 2010
(Table S2) Factor score matrix of benthic foraminifera ...
Takata, Hiroyuki   +8 more
core   +1 more source

On the Fidelity of Oxygen Isotope‐Based Sea Level Reconstructions: A Case Study of Marine Isotope Stage 3

open access: yesPaleoceanography and Paleoclimatology, Volume 41, Issue 10, October 2026.
Abstract Although foraminiferal oxygen isotope records (δ18OF) have long been used to develop time‐continuous estimates of past global ice volume, growing evidence indicates that the ice volume and temperature contributions to δ18OF diverge considerably over the last glacial cycle.
Tamara Pico   +5 more
wiley   +1 more source

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