Results 101 to 110 of about 6,307 (249)

How did the planktonic foraminifera respond to the extreme environmental stress induced by the OAE2 (Bonarelli Level) in the Bottaccione section (Gubbio, Italy)?

, 2002
Revets S. A. (Ed.), Forams 2002, International Symposium on Foraminifers, The University of Westrern Austarlia, Perth, 4-8 February ...
LUCIANI, Valeria, COCCIONI R
core  

(Table 2) Occurrence of larger benthic foraminifers in ODP Hole 133-823C

, 1993
(Table 2) Occurrence of larger benthic foraminifers in ODP Hole 133 ...
Christian Betzler (6960023), Betzler, Christian, George C H Chaproniere (6969149), Chaproniere, George C H   +3 more
core   +1 more source

(Table 4) Distribution and relative abundance of planktonic foraminifers in ODP Hole 114-704B

, 1991
(Table 4) Distribution and relative abundance of planktonic foraminifers in ODP Hole 114 ...
Robert Bourrouilh (7963379), Claude Pujol (6981449), Bourrouilh, Robert, Pujol, Claude   +3 more
core   +1 more source

Chukhonastovka – the reference section of the Turonian-Lower Santonian from the Volga-Ilovlya interfluve (the Volga right bank area near Volgograd). Paper 2. Characteristics of the Oryctocomplexes [PDF]

Известия Саратовского университета. Новая серия: Серия Науки о Земле
A representative complex of the Turonian-Santonian carbonate-producing invertebrates has been revealed. It comprised benthic foraminifers, diverse echinoderms, brachiopods, calcareous and siliceous sponges.
Pervushov, Evgeniy Mikhaylovich, Ryabov, Ilya P., Kalyakin, Evgeniy Aleksandrovich, Shelepov, Dmirtiy Aleksandrovich, Ilinskiy, Egor Igorevich   +4 more
doaj   +1 more source

Foraminifer of the Gulf of Cambay

, 1969
(Uploaded by Plazi from the Biodiversity Heritage Library) No abstract provided.
openaire   +2 more sources

(Appendix Table 1) Absolute abundances of benthic foraminifers in DSDP Hole 94-608

, 1987
(Appendix Table 1) Absolute abundances of benthic foraminifers in DSDP Hole 94 ...
Ellen Thomas (6963716), Thomas, Ellen
core   +1 more source

(Table 4) Ranges of benthic foraminifers from the early Oligocene to the early Miocene in DSDP Hole 22-214

, 1990
Benthic foraminifers were counted according to the following scheme: 1 = present, 2 = 2 or more, 3 = 3-5, 4 = 5-10, 6 = 10-30, 7 = 30-50, 8 = 50-75, and 9 = 75-150.
Anne Boersma (6886019), Boersma, Anne
core   +1 more source

Oligocene-Early Miocene Planktonic Microbiostratigraphy and Paleoenvironments of the South Slovakian Basin (Lučenec Depression)

Geologica Carpathica, 2015
Oligocene and Lower Miocene sediments of the Lučenec Depression were studied to demonstrate the planktonic bioevents and climatic proxies from the Číž Formation (Rupelian) and Lučenec Formation (Chattian-Aquitanian) on the basis of quantitative analyses ...
Ozdínová Silvia, Soták Ján
doaj   +1 more source

Pro‐197 mutations confer resistance to thiencarbazone but not to foramsulfuron in ALS‐resistant Poa annua populations

Pest Management Science, Volume 82, Issue 10, Page 10134-10146, October 2026.
Foramsulfuron remains effective on Pro‐197 Poa annua, but co‐formulation with thiencarbazone reduces efficacy due to limited activity and antagonism. Therefore, foramsulfuron + thiencarbazone should be used in fields without ALS‐resistant weeds to ensure effective in‐crop control.
Vijaya Bhaskar Alwarnaidu Vijayarajan, Iniya Vijayakumar, Rafa Ruiz‐Partida, Fabian Runge, Joel Torra, Jorge Lozano‐Juste, Patrick Dermot Forristal   +6 more
wiley   +1 more source

(Table 13) Ranges of benthic foraminifers through the early to middle Miocene in ODP Hole 115-715A

, 1990
Benthic foraminifers were counted according to the following scheme: 1 = present, 2 = 2 or more, 3 = 3-5, 4 = 5-10, 6 = 10-30, 7 = 30-50, 8 = 50-75, and 9 = 75-150.
Anne Boersma (6886019), Boersma, Anne
core   +1 more source