Results 31 to 40 of about 358 (131)
Geophysical Research Letters, Volume 53, Issue 7, 16 April 2026.Abstract Understanding the mechanisms linking low‐latitude monsoon variability and high‐latitude ice‐sheet discharge is critical for elucidating past atmospheric teleconnections, yet direct evidence for such linkages during the last glacial period remains limited. Here we present a high‐resolution terrigenous input record from the South China Sea (SCS)
Haosen Wang +6 more
wiley +1 more source
Geologica Balcanica, 1992 This is the second paper of a series dedicated to the Eocene small foraminifera from the Burgas region (East Bulgaria). Published herein are descriptions of 23 species of calcareous foraminifers from the families of Cymbaloporidae, Asterigerinidae, Nonionidae, Chilostomellidae, Alabaminidae, Oridorsalidae, Heterolepidae, Gavelinellidae, Rotaliidae ...
Stefka Darakchieva, Sava Juranov
openaire +1 more source
Holocene sea‐level and environmental changes on the Isle of Mull, Scotland
Journal of Quaternary Science, Volume 41, Issue 3, Page 400-418, April 2026.ABSTRACT Sea‐level and coastal changes are reconstructed on the Isle of Mull, western Scotland, from 10 988 to 10 507 cal BP to the present. This research has produced the first SLIP for the Isle of Mull. A multiproxy approach including pollen, spore, foraminifera and diatom analyses reveals palaeoenvironmental changes from two coastal sites.
Katherine A. Selby +6 more
wiley +1 more source
Geochemistry, Geophysics, Geosystems, Volume 27, Issue 4, April 2026.Abstract The late Eocene to early Oligocene is an intriguing Paleogene period in which the Earth climate state changed from Warmhouse to Coolhouse. Accurate age models are essential for investigating these climate transitions. The southwestern Pacific International Ocean Discovery Program (IODP) Site U1553, with its almost complete succession of the ...
Yang Zhang +5 more
wiley +1 more source
Paleoceanography and Paleoclimatology, Volume 41, Issue 4, April 2026.Abstract Robust evidence indicates that late Pleistocene glacial‐interglacial climate cycles are linked to periodic, orbitally‐forced changes in the partitioning of CO2 between the deep ocean and atmosphere. The extent to which changes in deep ocean carbon storage are related to climate on longer timescales is less well understood.
Joseph B. Novak +2 more
wiley +1 more source
Earth Surface Processes and Landforms, Volume 51, Issue 3, March 2026.Abstract Evaluating the state of activity of Deep‐Seated Gravitational Slope Deformation (DSGSD) is a challenge that requires multidisciplinary analytical approaches. This research focuses on the slope‐scale gravitational process, framing the role of the Quaternary morphodynamics of a river valley where multiple DSGSDs coexist, to reconstruct the ...
Giorgia Berardo +5 more
wiley +1 more source
Geoarchaeology, Volume 41, Issue 2, March/April 2026.ABSTRACT This paper presents the results of minero‐petrographic and chemical analyses of pottery and potential local raw materials from Ustica, a small volcanic island off the coast of Palermo (Sicily), inhabited during the Middle Neolithic. Typologically, the pottery shows cultural connections to the Bicromica and Serra d'Alto traditions, linking ...
G. Montana +6 more
wiley +1 more source
New Zealand Geological Timescale 2025
New Zealand Journal of Geology and Geophysics, Volume 69, Issue 1, March 2026.New Zealand Geological Timescale 2025 (NZGT 2025) is the first comprehensive update and revision of the New Zealand Geological Timescale in a decade. The criteria used to establish age ranges of New Zealand Stages within the NZGT have been reviewed, calibrated, and revised where required against the 2023/04 International Chronostratigraphic Chart and ...
Christopher D. Clowes +13 more
wiley +1 more source
Borings formed by Late Cretaceous endobiontic foraminifers within larger benthic foraminifers
, 2002 Nielsen, Jan Kresten (2002): Borings formed by Late Cretaceous endobiontic foraminifers within larger benthic foraminifers.
openaire +2 more sources
Alien Benthic Foraminifers from Turkish Strait System
International Journal of Environment and Geoinformatics, 2018 The Sea of Marmara is under the influence of the Black Sea and the Mediterranean. The salinity difference between these two seas causes the formation of two-layer stratification in the Sea of Marmara, an upper layer formed by the fresh waters of the Black Sea and a denser layer formed below 25 m of depth, by the more saline waters of the Mediterranean.
MERİÇ, Engin +4 more
openaire +3 more sources