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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Asia
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Middle East
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Iran
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Fars Iran (1)
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Zagros (2)
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Caribbean region
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West Indies
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Antilles
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Greater Antilles
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Cuba (1)
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Europe
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Pyrenees
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Spanish Pyrenees (2)
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Southern Europe
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Greece
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Peloponnesus Greece (1)
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Iberian Peninsula
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Spain
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Aragon Spain
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Teruel Spain (1)
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Catalonia Spain
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Lleida Spain
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Tremp Spain (1)
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Iberian Mountains (2)
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Spanish Pyrenees (2)
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Italy
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Apennines
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Southern Apennines (1)
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Apulia Italy
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Bari Italy (1)
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Basilicata Italy
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Potenza Italy (1)
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Campania Italy (2)
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Mexico
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Chiapas Mexico (1)
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San Luis Potosi Mexico (1)
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elements, isotopes
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isotope ratios (1)
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isotopes
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stable isotopes
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Sr-87/Sr-86 (1)
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metals
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alkaline earth metals
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strontium
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Sr-87/Sr-86 (1)
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fossils
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Invertebrata
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Protista
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Foraminifera
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Miliolina
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Miliolacea
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Alveolinellidae (1)
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Rotaliina (1)
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microfossils (12)
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geologic age
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Cenozoic
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Tertiary
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Paleogene
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Eocene
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middle Eocene
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Bartonian (1)
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upper Eocene
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Priabonian (1)
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Paleocene (2)
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Mesozoic
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Cretaceous
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Upper Cretaceous
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Campanian
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upper Campanian (1)
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Cenomanian
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upper Cenomanian (2)
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Maestrichtian
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lower Maestrichtian (2)
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Senonian (2)
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Turonian
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lower Turonian (1)
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Primary terms
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Asia
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Middle East
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Iran
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Fars Iran (1)
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Zagros (2)
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-
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biogeography (1)
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Caribbean region
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West Indies
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Antilles
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Greater Antilles
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Cuba (1)
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-
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Cenozoic
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Tertiary
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Paleogene
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Eocene
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middle Eocene
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Bartonian (1)
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upper Eocene
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Priabonian (1)
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-
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Paleocene (2)
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-
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Europe
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Pyrenees
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Spanish Pyrenees (2)
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Southern Europe
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Greece
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Peloponnesus Greece (1)
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-
Iberian Peninsula
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Spain
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Aragon Spain
-
Teruel Spain (1)
-
-
Catalonia Spain
-
Lleida Spain
-
Tremp Spain (1)
-
-
-
Iberian Mountains (2)
-
Spanish Pyrenees (2)
-
-
-
Italy
-
Apennines
-
Southern Apennines (1)
-
-
Apulia Italy
-
Bari Italy (1)
-
-
Basilicata Italy
-
Potenza Italy (1)
-
-
Campania Italy (2)
-
-
-
-
Invertebrata
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Protista
-
Foraminifera
-
Miliolina
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Miliolacea
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Alveolinellidae (1)
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-
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Rotaliina (1)
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-
-
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isotopes
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stable isotopes
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Sr-87/Sr-86 (1)
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-
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Mesozoic
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Cretaceous
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Upper Cretaceous
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Campanian
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upper Campanian (1)
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Cenomanian
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upper Cenomanian (2)
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Maestrichtian
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lower Maestrichtian (2)
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Senonian (2)
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Turonian
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lower Turonian (1)
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-
-
-
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metals
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alkaline earth metals
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strontium
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Sr-87/Sr-86 (1)
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-
-
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Mexico
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Chiapas Mexico (1)
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San Luis Potosi Mexico (1)
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paleoecology (2)
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paleogeography (1)
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sediments
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marine sediments (1)
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sediments
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sediments
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marine sediments (1)
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In Memory of Josep Serra-Kiel (1948–2019)
Imperforate Larger Benthic Foraminifera from Shallow-water Carbonate Facies (middle and Late Eocene), Zagros Mountains, Iran
New Rotaliids (benthic Foraminifera) from the Late Cretaceous of the Pyrenees in Northeastern Spain
BENTHIC FORAMINIFERA IN THE AFTERMATH OF THE CENOMANIAN-TURONIAN BOUNDARY EXTINCTION EVENT IN THE CARBONATE PLATFORM FACIES OF THE SOUTHERN APENNINES (ITALY)
PRAETABERINA NEW GENUS (TYPE SPECIES: TABERINA BINGISTANI HENSON, 1948): A STRATIGRAPHIC MARKER FOR THE LATE CENOMANIAN
PALEOENVIRONMENTAL DISTRIBUTION OF LARGER FORAMINIFERA IN UPPER CRETACEOUS SILICICLASTIC–CARBONATE DEPOSITS (ARÉN SANDSTONE FORMATION, SOUTH PYRENEES, NORTHEASTERN SPAIN)
ARCHITECTURE AND AGE OF THE FORAMINIFERAL GENUS TABERINA
MEMORIAL TO LUKAS HOTTINGER (1933–2011)
THE LATE CRETACEOUS GENERA CUVILLIERINELLA , CYCLOPSEUDEDOMIA , AND RHAPYDIONINA (RHAPYDIONINIDAE, FORAMINIFERIDA) IN SHALLOW-WATER CARBONATES OF PYLOS (PELOPONNESE, GREECE)
CENOMANIAN RHAPYDIONINIDS (FORAMINIFERIDA): ARCHITECTURE OF THE SHELL AND STRATIGRAPHY
SHELL ARCHITECTURE IN THE LATE CRETACEOUS FORAMINIFERAL SUBFAMILY CLYPEORBINAE SIGAL, 1952
LEPIDORBITOIDES MINIMA DOUVILLÉ FROM MEXICO, A FORAMINIFERAL INDEX FOSSIL FOR THE CAMPANIAN
Praealveolina (Foraminifera) species; a tool to date Cenomanian platform sediments
Cretaceous
Abstract Cretaceous rocks crop out extensively in the three main Alpine orogenic belts of Spain: the Betic Cordillera, the Pyrenees and the Iberian Ranges. These rocks, deformed during Cenozoic Alpine convergence, are almost entirely sedimentary (with the exception of rare volcanic and meta-morphic rocks) and were deposited in an enormous variety of environments ranging from alluvial fans to pelagic seas. There were four main basins – Betic, Pyrenean, Basque-Cantabrian and Iberian (Fig. 12.1 ) – each of which originated in Triassic and Jurassic times in response to continental break-up at the start of the Alpine cycle. They subsequently underwent a polyphase evolution in the Cretaceous period when palaeo-geography and sedimentation in Iberia were strongly influenced by the relative movements of the contiguous Eurasian and African plates. Initiation of the North Atlantic spreading in earliest Cretaceous time led to a decrease in relative sinistral motion between Iberia and Africa (e.g. Ziegler 1988 a ). This was followed by a phase of rapid counterclockwise rotation of Iberia relative to Europe and the progressive opening of the Bay of Biscay, which lasted from late Aptian to early Campanian times (e.g. Olivet 1996 ). Finally, a third phase of basin evolution was heralded by the onset of Late Cretaceous oblique convergence between Africa and Europe (e.g. Savostin et al . 1986 ; Reicherter & Pletsch 2000 ). In addition to this changing tectonic setting, other factors, such as climate and eustasy, were also important controlling influences. The Cretaceous climate of Iberia