Results 51 to 60 of about 7,973 (217)

Foraminifera from the Tepetate Formation (Heim) at Las Pocitas, Baja California Sur, Mexico

open access: yesCiencias Marinas, 2008
In order to constrain the age and depositional paleoenvironment of the Tepetate Formation, benthic and planktonic foraminifera were analyzed in samples recovered from an exploration well located at Las Pocitas, Baja California Sur, Mexico.
AY Miranda-Martínez, AL Carreño
doaj   +1 more source

Complex marine ecological response during the Eocene-Oligocene revealed by global foraminiferal record. [PDF]

open access: yesNat Commun
The Eocene–Oligocene transition was the crucial turning point when Earth’s climate shifted to its current icehouse state. Understanding how the marine biosphere responded during this transition is not well-constrained, appearing as a simple extinction ...
Lu Z   +15 more
europepmc   +2 more sources

Planktonic foraminifera shell parameter, carbonate and particulate organic carbon fluxes in the Fram Strait from mooring FEVI30 at AWI HAUSGARTEN

open access: yes, 2023
Fluxes of planktonic foraminifera, carbonate and particulate organic carbon from the central station of the LTER (Long-Term Ecological Research) HAUSGARTEN observatory in the Fram Strait at two depths intervals (213 m, 2319 m) from a one-year time period
Tell, Franziska
core   +1 more source

Facies and paleoenvironmental reconstruction of Early–Middle Miocene deposits in the north-west of the Zagros Basin, Iran

open access: yesGeologica Carpathica, 2019
Facies analysis and paleoenvironmental reconstruction of the Burdigalian to Langhian Asmari Formation, outcropping in the Khorram Abad Anticline, in the north-west of the Zagros Basin allow us to interpret the carbonate ramp history during the Early ...
Roozpeykar Asghar   +3 more
doaj   +1 more source

A resolution for the coiling direction paradox in Neogloboquadrina pachyderma. [PDF]

open access: yes, 2006
We present new data on genotypic differences and biogeographic distribution of coiling types in the living planktonic foraminiferal morphospecies Neogloboquadrina pachyderma. The genetic evidence demonstrates that coiling direction in N.
Dick Kroon   +14 more
core   +1 more source

Palaeoenvironmental, palaeoecological and palaeobiogeographical implications of mixed fresh water and brackish marine assemblages from the Cretaceous-Palaeogene Deccan intertrappean beds at Jhilmili, Chhindwara District, central India

open access: yesRevista Mexicana de Ciencias Geológicas, 2018
The Deccan infra- and intertrappeans volcano-sedimentary sequences have been considered as terrestrial to fluvio-lacustrine deposits. Presence of planktonic foraminifera and brackish water ostracods in the Jhilmili basal Danian intertrappean beds ...
Ashu Khosla
doaj   +1 more source

STRATIGRAPHY AND MICROFACIES STUDIES ON SOME TERTIARY ROCKS IN NORTH GALALA PLATEAU, NORTH EASTERN DESERT, EGYPT [PDF]

open access: yesDelta Journal of Science, 2006
The early and middle Eocene successions of Wadi EL Qena (Sec. II) and Wadi El Agramiya (Sec. I) surface sections in west El Galala El-Baharia area, north Eastern Desert, were examined in detail.
A. Galal, A.S. EL-Dawoody
doaj   +1 more source

Projected impacts of climate change and ocean acidification on the global biogeography of planktonic Foraminifera [PDF]

open access: yesBiogeosciences, 2015
Planktonic Foraminifera are a major contributor to the deep carbonate flux and their microfossil deposits form one of the richest databases for reconstructing paleoenvironments, particularly through changes in their taxonomic and shell composition. Using
T. Roy, F. Lombard, L. Bopp, M. Gehlen
doaj   +1 more source

Integrated stratigraphy of the Waitakian-Otaian Stage boundary stratotype, Early Miocene, New Zealand

open access: yes, 1999
The base of the type section of the Otaian Stage at Bluecliffs, South Canterbury, is recognised as the stratotype for the boundary between the Waitakian and Otaian Stages.
G. H. Scott   +15 more
core   +1 more source

Planktonic Foraminifera Biostratigraphy Of Taeno Limestone, Ambon, Maluku Province, Indonesia

open access: yesJGEET: Journal of Geoscience, Engineering, Environment and Technology
The limestone became exposed to the surface because of an uplift event during the Quaternary period. This study aims to determine the age of limestone outcrops in the Taeno Traverse using planktonic foraminifera.
Zulfiah, Sanny V. Aponno, Erfin Elly
doaj   +1 more source

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