Results 61 to 70 of about 42,104 (227)

Climate conditions on the South‐Iberian Palaeomargin during the latest Pliensbachian to early Toarcian: A mineralogical and geochemical study from hemipelagic deposits

Sedimentology, Volume 73, Issue 5, Page 1631-1663, August 2026.
ABSTRACT The integrated analysis of lithofacies, mineralogy and geochemistry of the hemipelagic marine succession exposed in La Cerradura section (South‐Iberian Palaeomargin) provides new information to characterise the palaeoenvironmental conditions during the latest Pliensbachian to early Toarcian, including the Jenkyns Event.
Chaima Ayadi, Isabel Abad, Elisa Laita, Ali Mokhtar Samet, Matías Reolid   +4 more
wiley   +1 more source

Foraminiferal, ostracod, and calcareous nannofossil biostratigraphy of the latest Badenian – Sarmatian interval (Middle Miocene, Paratethys) from Poland, Romania and the Republic of Moldova

Geologica Carpathica, 2017
This study presents detailed foraminiferal, ostracod, and calcareous nannofossil analyses of five Middle Miocene sections located in the Central Paratethyan realm, namely in Poland, Romania and the Republic of Moldova. Based on foraminiferal distribution,
Dumitriu Simina Dumitriţa, Loghin Sergiu, Dubicka Zofia, Melinte-Dobrinescu Mihaela Carmen, Paruch-Kulczycka Jolanta, Ionesi Viorel   +5 more
doaj   +1 more source

(Table T3) Calcareous nannofossil abundance of ODP Hole 189-1170A sediments

, 2003
(Table T3) Calcareous nannofossil abundance of ODP Hole 189-1170A ...
Wei, Wuchang, Wuchang Wei (6964964), Kristeen L McGonigal (6960401), McGonigal, Kristeen L   +3 more
core   +1 more source

Marine Sediment Record of Eruption‐Fed Vertical Density Currents, Kermadec Arc (Rangitāhua)

Geochemistry, Geophysics, Geosystems, Volume 27, Issue 7, July 2026.
Abstract Products of explosive volcanism can be transported into the oceans, where they form marine tephra layers. The processes responsible for their deposition are often complex, involving multiple transport mechanisms. During the RV Investigator voyage IN2022‐V02 (2022), a 35‐cm‐thick marine tephra unit was piston‐cored at 2,460 m water depth in the
Janne M. Scheffler, Martin Jutzeler, Steffen Kutterolf, Rebecca J. Carey, Josephin Wolf, Jacek Raddatz, Kuo‐Lung Wang, Hao‐Yang Lee   +7 more
wiley   +1 more source

Integrated biostratigraphy of two Upper Maastrichtian – Palaeocene successions in north-central Sinai, Egypt

Geologia Croatica, 2012
Integration of the calcareous nannofossil and planktonic foraminiferal biostratigraphies has been performed for theUpper Maastrichtian – Palaeocene successions at Gebel Umm Khushayb and west El-Hassana sections (north-centralSinai, Egypt).
Mahmoud Faris, Sherif Farouk
doaj   +1 more source

Biostratigraphy of Gurpi Formation in Samand anticline (Lurestan province) Based on calcareous nannofossils [PDF]

Journal of Stratigraphy and Sedimentology Researches, 2017
The present study is an attempt to biostratigraphically classify the rocks of Gurpi Formation at Samand Anticline with the help of calcareous nannofossils. The succession measures 197 meters in thickness and consists of shale, marl and marly limestone. A
samira shahriyary, Anoshiravan Kani, Hassan Amiribakhtiar   +2 more
doaj   +1 more source

Regional Variations in Sea Ice and Primary Productivity in the Bering Sea During Marine Isotope Stage 11

Geochemistry, Geophysics, Geosystems, Volume 27, Issue 7, July 2026.
Abstract Marine Isotope Stage (MIS) 11 (424–374 ka) has long been an analog for Holocene climate because it is the most recent interglacial period with similar orbital conditions. However, there is global and regional variability in the climate response to MIS 11 warmth.
N. S. Thompson, B. E. Caissie
wiley   +1 more source

(Table T2) Calcareous nannofossil abundance across the Oligocene/Miocene boundary of ODP Hole 189-1168A sediments

, 2003
(Table T2) Calcareous nannofossil abundance across the Oligocene/Miocene boundary of ODP Hole 189-1168A ...
Wei, Wuchang, Wuchang Wei (6964964), Kristeen L McGonigal (6960401), McGonigal, Kristeen L   +3 more
core   +1 more source

Tracing the Migration of Fronts in the Pacific Southern Ocean Across the Mid‐Pleistocene Transition

Paleoceanography and Paleoclimatology, Volume 41, Issue 7, July 2026.
Abstract The Southern Ocean is a key driver of global climate variability, yet its dynamics during the Mid‐Pleistocene Transition (MPT; ∼1.25–0.7 Ma) remain poorly understood, especially in the South Pacific sector. The Polar Frontal Zone (PFZ) underwent significant latitudinal shifts during this critical period of climate reorganization.
V. M. Sinnen, O. Esper, M. Duffy, C. R. Riesselman, F. Lamy, T. Frederichs, C. B. Lange   +6 more
wiley   +1 more source

(Table 7) Quaternary calcareous nannofossil datums in ODP Hole 130-807A

, 1993
(Table 7) Quaternary calcareous nannofossil datums in ODP Hole 130 ...
Toshiaki Takayama (6967418), Takayama, Toshiaki   +1 more
core   +1 more source