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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Africa
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East Africa
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Ethiopia (1)
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Zambia (1)
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Madagascar (1)
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North Africa
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Atlas Mountains
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Egypt (1)
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Southern Africa
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Asia
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halogens
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isotope ratios (10)
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isotopes
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metals
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oxygen
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fossils
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Chordata
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Vertebrata
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Pisces
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Osteichthyes
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Sarcopterygii
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Tetrapoda
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Aves
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Mammalia
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Theria
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Artiodactyla
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Carnivora
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Rodentia
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Reptilia
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Diapsida
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Archosauria
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Crocodilia
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dinosaurs
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Ornithischia
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Triceratops (1)
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Ornithopoda
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Hadrosauridae (2)
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Saurischia
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Theropoda
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Coelurosauria
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Pterosauria
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Ichthyosauria (3)
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Lepidosauria
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Squamata
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Lacertilia
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Sauropterygia
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Synapsida
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Therapsida (3)
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coprolites (1)
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cyanobacteria (2)
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Graptolithina
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Hemichordata (2)
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Invertebrata
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Arthropoda
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Chelicerata
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Merostomata
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Mandibulata
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Crustacea
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Ostracoda
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Myodocopida (1)
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Podocopida
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Bairdiomorpha
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Bairdiidae
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Bairdia (1)
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Cypridocopina
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Cyprididae (1)
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Insecta
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Pterygota
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Neoptera
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Endopterygota
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Hymenoptera (1)
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Trilobitomorpha
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Trilobita (4)
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Brachiopoda
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Articulata
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Productida (1)
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Rhynchonellida
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Spiriferida (1)
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Bryozoa
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Cnidaria
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Tabulata (4)
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Echinodermata
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Asterozoa
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Crinozoa
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Mollusca
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Bivalvia
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Pterioida
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Cephalopoda
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Gastropoda
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Porifera
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Protista
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Foraminifera
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Radiolaria (1)
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Vermes
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Priapulida (1)
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Metazoa (3)
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microfossils
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Conodonta
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problematic microfossils (3)
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palynomorphs
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Dinoflagellata (3)
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miospores
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Plantae
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diatoms (1)
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Pteridophyta
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Spermatophyta
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Coniferales
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Taxodiaceae
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Glossopteridales (1)
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problematic fossils
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problematic microfossils (3)
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Pterobranchia (1)
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thallophytes (1)
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Cenozoic
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Tertiary
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-
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White River Group (1)
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Mesozoic
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Cretaceous
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Lower Cretaceous
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Agrio Formation (1)
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Cloverly Formation (1)
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Middle Cretaceous (1)
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Senonian (4)
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Two Medicine Formation (1)
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-
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Jurassic
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Lower Jurassic
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Pliensbachian (3)
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Toarcian (3)
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Triassic-Jurassic boundary (1)
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Middle Jurassic
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Upper Jurassic
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Arab Formation (1)
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Hanifa Formation (1)
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Morrison Formation (1)
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Sundance Formation (1)
-
-
-
Triassic
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Middle Triassic
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Muschelkalk (1)
-
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Upper Triassic
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Chinle Formation (1)
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Rhaetian (1)
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Triassic-Jurassic boundary (1)
-
-
-
-
Paleozoic
-
Cambrian
-
Lower Cambrian
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Tommotian (1)
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Middle Cambrian
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Burgess Shale (1)
-
-
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Carboniferous
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Lower Carboniferous
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Dinantian (1)
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Mississippian
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Lower Mississippian
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-
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Upper Mississippian
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Chesterian (1)
-
-
-
Pennsylvanian
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Conemaugh Group (1)
-
Middle Pennsylvanian
-
Atokan
-
Atoka Formation (1)
-
-
Desmoinesian
-
Hartshorne Sandstone (1)
-
-
-
Upper Pennsylvanian (2)
-
-
Upper Carboniferous
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Westphalian (2)
-
-
-
Devonian
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Lower Devonian
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Emsian (1)
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Lochkovian (1)
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-
Middle Devonian
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Eifelian (1)
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Hamilton Group (1)
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lower Paleozoic (1)
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Ordovician
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Lower Ordovician
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Middle Ordovician
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Darriwilian (1)
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-
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Upper Ordovician
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Hirnantian (1)
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Red River Formation (2)
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-
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Permian
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Khuff Formation (2)
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Lower Permian (1)
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Upper Permian (3)
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Read Bay Formation (1)
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Silurian
-
Lower Silurian
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Llandovery
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Telychian (1)
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Wenlock (2)
-
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Middle Silurian
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Rochester Formation (1)
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Upper Silurian (1)
-
-
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Phanerozoic (7)
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Precambrian
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-
upper Precambrian
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Proterozoic
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Neoproterozoic
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Doushantuo Formation (1)
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Ediacaran (7)
-
Riphean
-
upper Riphean (1)
-
-
Vendian (3)
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Wilpena Group (1)
-
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Sinian
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Doushantuo Formation (1)
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-
-
-
-
-
igneous rocks
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igneous rocks
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plutonic rocks
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granites (1)
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volcanic rocks (1)
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volcanic ash (1)
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metamorphic rocks
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metamorphic rocks
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metaigneous rocks
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serpentinite (1)
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metasomatic rocks
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serpentinite (1)
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minerals
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carbonates (1)
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halides
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chlorides
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halite (1)
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kainite (1)
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phosphates
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apatite (1)
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-
silicates
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framework silicates
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zeolite group
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heulandite (1)
-
-
-
-
sulfates
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kainite (1)
-
-
-
Primary terms
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absolute age (2)
-
Africa
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East Africa
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Ethiopia (1)
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Zambia (1)
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Madagascar (1)
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North Africa
-
Atlas Mountains
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Moroccan Atlas Mountains
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Anti-Atlas (1)
-
-
-
Egypt (1)
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Morocco
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Moroccan Atlas Mountains
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Anti-Atlas (1)
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Western Sahara (1)
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Southern Africa
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Namibia (1)
-
-
-
Arctic region
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Greenland
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paleobiology
The effects of the Jenkyns Event on the radiation of Early Jurassic dinoflagellate cysts
Abstract This contribution is an overview of the Early Jurassic dinoflagellate cysts of the Lusitanian Basin in Portugal, with particular emphasis on the effects of the Jenkyns Event (Toarcian Oceanic Anoxic Event) on the evolution of this planktonic group. We review and discuss data from 214 samples from six Lower Jurassic successions (upper Sinemurian to upper Toarcian) in the Lusitanian Basin. The late Pliensbachian radiation of dinoflagellate cysts was well recognized in this basin. The pre-Jenkyns Event interval is highly productive, with maximum abundance and species richness values. However, this palaeoenvironmental perturbation severely affected the evolution of this group for the remainder of the Early Jurassic. The prolonged recovery of the dinoflagellates in the Toarcian following the Jenkyns Event is not typical of the northern regions (Arctic and Boreal realms), where new species began to evolve earlier compared with southern European basins.
Tabelliscolex (Cricocosmiidae: Palaeoscolecidomorpha) from the early Cambrian Chengjiang Biota and the evolution of seriation in Ecdysozoa
Primary tissues dominated ground-level trunk diameter in Sigillaria : evidence from the Wuda Tuff, Inner Mongolia
Phylogenetic paleoecology: macroecology within an evolutionary framework
Zoogeographical and stratigraphical distribution of the genus Zonocypris : Supportive evidence for Anatolian Diagonal and description of a new species from Turkey
The “earliest tabulate corals” are not tabulates
Seven rules for simulations in paleobiology
Cretaceous to Recent net continental uplift from paleobiological data: Insights into sub-plate support
Introvert and pharynx of Mafangscolex , a Cambrian palaeoscolecid
The Herefordshire Lagerstätte: fleshing out Silurian marine life
Estimation, not significance
Life span bias explains live–dead discordance in abundance of two common bivalves
Extreme rarity of competitive exclusion in modern and fossil marine benthic ecosystems
New perspectives on pterosaur palaeobiology
Abstract: Pterosaurs were the first vertebrates to evolve powered flight and occupied the skies of the Mesozoic for 160 million years. They occurred on every continent, evolved their incredible proportions and anatomy into well over 100 species, and included the largest flying animals of all time among their ranks. Pterosaurs are undergoing a long-running scientific renaissance that has seen elevated interest from a new generation of palaeontologists, contributions from scientists working all over the world and major advances in our understanding of their palaeobiology. They have especially benefited from the application of new investigative techniques applied to historical specimens and the discovery of new material, including detailed insights into their fragile skeletons and their soft tissue anatomy. Many aspects of pterosaur science remain controversial, mainly due to the investigative challenges presented by their fragmentary, fragile fossils and notoriously patchy fossil record. With perseverance, these controversies are being resolved and our understanding of flying reptiles is increasing. This volume brings together a diverse set of papers on numerous aspects of the biology of these fascinating reptiles, including discussions of pterosaur ecology, flight, ontogeny, bony and soft tissue anatomy, distribution and evolution, as well as revisions of their taxonomy and relationships.
Abstract: Understanding the ecological roles of pterosaurs is a challenging pursuit, but one aided by a growing body of fossil evidence for their dietary preferences and roles as food sources for other species. Pterosaur foraging behaviour is represented by preserved gut content, stomach regurgitates, coprolites and feeding traces. Pterosaurs being eaten by other species are recorded by tooth marks and teeth embedded in their fossil bones, consumer gut content and regurgitate, and their preservation entangled with predatory animals. This palaeoecological record has improved in recent years, but remains highly selective. The Jurassic rhamphorhynchid Rhamphorhynchus , Cretaceous ornithocheiroid Pteranodon and azhdarchid pterosaurs currently have the most substantial palaeoecological records. The food species and consumers of these taxa conform to lifestyle predictions for these groups. Rhamphorhynchus and Pteranodon ate and were eaten by aquatic species, matching expectations of these animals as sea-going, perhaps partly aquatic species. Possible azhdarchid pterosaur foraging traces alongside pterosaur tracks, and evidence that these animals were eaten by dinosaurs and Crocodyliformes, are consistent with hypotheses that azhdarchids foraged and lived in terrestrial settings. Fossil evidence of pterosaur palaeoecology remains rare: researchers are strongly encouraged to put specimens showing details of dietary preferences, foraging strategies or interactions with other animals on record.
Pelvic musculature of Vectidraco daisymorrisae and consequences for pterosaur locomotion
Abstract: The unique morphology of pterosaurs makes them a compelling group to study, but the lack of ready analogues or descendant clades presents problems when inferring their biology and ecology. In this paper, the extant phylogenetic bracket is used to reconstruct the musculature of the pterosaur Vectidraco daisymorrisae and a detailed comparison is made between the musculature of this taxon and other reconstructions in the literature. M. iliofibularis is reconstructed as originating upon the angular process of the posterior iliac process, putting it into a mechanically advantageous position as an abductor. M. flexor tibialis internus is reconstructed as greatly enlarged over the ancestral state, probably in response to the reduction of M. caudofemoralis brevis and the tail. This enlargement is considered to correspond to the increasing role of M. flexor tibialis internus as a hip retractor.