Results 71 to 80 of about 73,101 (168)

Sea surface temperature changes in the southern California borderlands during the last glacial-interglacial cycle [PDF]

, 1996
A variety of evidence suggests that average sea surface temperatures (SSTs) during the last glacial maximum in the California Borderlands region were significantly colder than during the Holocene.
Bandy, Bard, Berelson, Berger, Bond, Bond, Bradshaw, Clark, CLIMAP Project Members, Climate: Long-Range Investigation, Cooperative Holocene Mapping Project (COHMAP) Members, Coulbourn, Dansgaard, David M. Anderson, Epstein, Fairbanks, Fairbanks, Fischer, Gorsline, Gorsline, Grootes, Hickey, Hickey, Hickey, Hutson, Huyer, Imbrie, Imbrie, Jahnke, Jianning Le, Kahn, Kennett, Kennett, Kheradpir, Lowell D. Stott, Martin, Martin, Martinson, McIntyre, Okada, Overpeck, P. Graham Mortyn, Prahl, Prell, Reynolds, Robert C. Thunell, Sautter, Sautter, Taylor, Thunell, Thunell, Thunell, Tont   +52 more
core   +2 more sources

SOME MICROFOSSILS (DASYCLADALES, BENTHIC FORAMINIFERA, SPONGES) FROM THE UPPER JURASSIC MOZDURAN FORMATION (NE IRAN, KOPET-DAGH) AND THEIR BIOSTRATIGRAPHIC AND PALAEOBIOGEOGRAPHIC IMPORTANCE

Rivista Italiana di Paleontologia e Stratigrafia, 2019
The Mozduran Formation represents mainly carbonatic shallow-water deposits from the Kopet-Dagh basin of northeast Iran. Longtime considered to be of exclusively Late Jurassic (Oxfordian-Kimmeridgian) age, its ranging into the Early Cretaceous has been ...
FELIX SCHLAGINTWEIT, ZOHREH KADIVAR, KOOROSH RASHIDI   +2 more
doaj   +1 more source

A revision of the Lower Cretaceous foraminiferal genus Falsogaudryinella from northwest Europe and Romania, and its relationship to Uvigerinammina [PDF]

, 1995
We emend the definition of the foraminiferal genus Falsogaudryinella Bartenstein, 1977 based on observations of the type species, F. tealbyensis from the Barremian Lower Tealby Clay of Lincolnshire, U.K.
Kaminski, M.A., Neagu, T., Platon, E.
core  

Petrogenesis of diachronous mixed siliciclastic-carbonate megafacies in the cool-water Oligocene Tikorangi Formation, Taranaki Basin, New Zealand [PDF]

, 2003
The Oligocene (Whaingaroan-Waitakian) Tikorangi Formation is a totally subsurface, lithostratigraphically complex, mixed siliciclastic-limestone-rich sequence forming an important fracture reservoir within Taranaki Basin, New Zealand.
Berggren W. A., Bernecker T., Driscoll N. W., Hood S. D., Hudson D. S., Hume T. R., Mauri S., Morgans H. E. G., Mullins H. T., Mullins H. T., Naish T. R., Nelson C. S., Nelson C. S., Palmer J. A., Rao C. P., Scott G. H., Simpson J., Tucker M., Westphal H., Young J.   +19 more
core   +2 more sources

Reading the Fine Print: Ultra-Microstructures of Foraminiferal Calcification Revealed Using Focused Ion Beam Microscopy

Frontiers in Marine Science, 2018
The elemental composition of calcite is of critical value in paleoceanographic reconstructions, yet little is known about biological processes underlying elemental uptake by foraminifers during calcification.
Yukiko Nagai, Yukiko Nagai, Katsuyuki Uematsu, Ryoji Wani, Takashi Toyofuku, Takashi Toyofuku   +5 more
doaj   +1 more source

Miocene deep-water agglutinated foraminifera from the Lomonosov Ridge and the opening of the Fram Strait [PDF]

, 2009
Deep-water agglutinated Foraminifera (DWAF) were recovered from Miocene to Pliocene sediments in 103 samples from IODP Hole M0002A on the Lomonosov Ridge.
Kaminski, M.A., Kender, S., Silye, L.
core  

Recalibration of the Tethyan shallow-benthic zonation across the Paleocene-Eocene boundary: the Egyptian record

Geologica Acta, 2009
The Galala Mountains in Egypt provide an excellent platform-basin transect with deposits spanning the Paleocene/ Eocene (P/E) boundary. These interfingering deposits enable a recalibration between platform and open marine biostratigraphic schemes.
C. SCHEIBNER, R.P. SPEIJER
doaj  

Chronology for climate change: Developing age models for the biogeochemical ocean flux study cores [PDF]

, 2004
We construct age models for a suite of cores from the northeast Atlantic Ocean by means of accelerator mass spectrometer dating of a key core, BOFS 5K, and correlation with the rest of the suite.
Manighetti, B, Maslin, M, McCave, IN, Shackleton, NJ   +3 more
core   +1 more source

An integrated biostratigraphy and seismic stratigraphy for the late Neogene continental margin succession in northern Taranaki Basin, New Zealand [PDF]

, 2006
Our aim has been to develop an integrated biostratigraphy and seismic stratigraphy for the Pliocene and Pleistocene formations (Ariki, Mangaa, Giant Foresets) in northern Taranaki Basin to better understand the evolution of the modern continental margin ...
Armentrout JM, Armstrong PA, Bé AWH, Bé AWH, Crundwell MP, Hansen RJ, Hayward BW, Hayward BW, Hornibrook NdeB, Hoskins RH, Hoskins RH, Mitchum RM, Murray JW, Pilaar WFH, Shell BP, Strong CP, Vail PR, Waghorn DB   +17 more
core   +2 more sources

Representing Zooplankters: An Example from the Foraminifera

Geosciences
Because of their excellent preservation record, testate zooplankters provide valuable proxy ocean climate data through the Quaternary–Recent. Commonly, specimen abundances are sought, which are time-consuming to collect manually and require taxonomic ...
George H. Scott
doaj   +1 more source