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NARROW
GeoRef Subject
-
all geography including DSDP/ODP Sites and Legs
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Africa
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East Africa
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Tanzania (2)
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North Africa
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Egypt (1)
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Morocco
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Rif (1)
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Antarctica
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Asia
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Far East
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stable isotopes
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Invertebrata
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-
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Trilobitomorpha
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Cnidaria
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Scleractinia (1)
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Mollusca
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Cephalopoda
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Protista
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Vermes
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Paleocene-Eocene Thermal Maximum (2)
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Mesozoic
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lower Turonian (3)
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Paleozoic
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Devonian
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Old Red Sandstone (1)
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Primary terms
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Africa
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North Africa
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West Africa (1)
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Far East
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carbon
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upper Holocene (2)
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Pleistocene
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upper Pleistocene
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upper Quaternary (2)
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Tertiary
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Neogene
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Miocene
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Puerto Madryn Formation (1)
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upper Miocene
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Messinian (1)
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Pliocene
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lower Pliocene (1)
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Paleogene
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Eocene
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lower Eocene
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Sparnacian (1)
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Ypresian
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London Clay (1)
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middle Eocene
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Lutetian (1)
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Nanjemoy Formation (1)
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upper Eocene (2)
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Oligocene
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lower Oligocene (1)
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Paleocene
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lower Paleocene
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Danian (2)
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K-T boundary (2)
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upper Paleocene
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Thanetian (1)
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Paleocene-Eocene Thermal Maximum (2)
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Chordata
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Vertebrata
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Reptilia
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climate change (2)
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Leg 39
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DSDP Site 356 (1)
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ecology (4)
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Europe
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United Kingdom
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England
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Lincolnshire England (1)
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Scotland
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Hebrides
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Inner Hebrides
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Raasay (1)
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-
-
Highland region Scotland
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Inverness-shire Scotland
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Raasay (1)
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-
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Wales (1)
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-
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Wadden Sea (1)
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-
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geochemistry (1)
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Graptolithina (1)
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Indian Ocean
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Wombat Plateau (1)
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Integrated Ocean Drilling Program
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Expedition 318
-
IODP Site U1357 (1)
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Invertebrata
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Mandibulata
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Crustacea
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Copepoda (1)
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Ostracoda (2)
-
-
-
Trilobitomorpha
-
Trilobita (1)
-
-
-
Cnidaria
-
Anthozoa
-
Zoantharia
-
Scleractinia (1)
-
-
-
-
Mollusca
-
Cephalopoda
-
Coleoidea
-
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-
Belemnitidae (1)
-
-
-
-
-
Protista
-
Foraminifera (5)
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Radiolaria (1)
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Thecamoeba (2)
-
-
Vermes
-
Annelida (1)
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scolecodonts (1)
-
-
-
isotopes
-
radioactive isotopes
-
C-14 (1)
-
-
stable isotopes
-
C-13/C-12 (5)
-
N-15/N-14 (1)
-
O-18/O-16 (3)
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S-34/S-32 (1)
-
-
-
land use (1)
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Mediterranean Sea
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Ionian Sea (1)
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-
-
Mesozoic
-
Cretaceous
-
Lower Cretaceous
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Albian
-
lower Albian (1)
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-
Berriasian (1)
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-
Middle Cretaceous (1)
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Upper Cretaceous
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Campanian
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upper Campanian (1)
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Cenomanian
-
upper Cenomanian (1)
-
-
Coniacian (1)
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Gulfian
-
Eagle Ford Formation (1)
-
-
K-T boundary (2)
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Navesink Formation (1)
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Santonian (1)
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Senonian (3)
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Turonian
-
lower Turonian (3)
-
-
-
-
Jurassic
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Lower Jurassic
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Hettangian (1)
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lower Liassic (1)
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Pliensbachian (1)
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Sinemurian (1)
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Toarcian (1)
-
-
Middle Jurassic
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Bathonian (1)
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Callovian (1)
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-
Upper Jurassic
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Oxfordian (1)
-
-
-
Triassic
-
Upper Triassic
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Norian (1)
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Rhaetian
-
Penarth Group (1)
-
-
-
-
-
nitrogen
-
N-15/N-14 (1)
-
-
North America
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Strait of Georgia (1)
-
-
Ocean Drilling Program
-
Leg 104 (1)
-
Leg 113
-
ODP Site 690 (1)
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Leg 120
-
ODP Site 747 (1)
-
-
Leg 122
-
ODP Site 761 (1)
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-
Leg 159
-
ODP Site 959 (1)
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-
Leg 166
-
ODP Site 1007 (1)
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Leg 174AX (1)
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Leg 189
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ODP Site 1172 (1)
-
-
-
oxygen
-
dissolved oxygen (1)
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O-18/O-16 (3)
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Pacific Ocean
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East Pacific
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Northeast Pacific (2)
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North Pacific
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Northeast Pacific (2)
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Northwest Pacific
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East China Sea (1)
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South China Sea (1)
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Yellow Sea
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Bohai Sea (1)
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-
-
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South Pacific
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Southwest Pacific
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Tasman Sea (1)
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-
-
West Pacific
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Northwest Pacific
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East China Sea (1)
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South China Sea (1)
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Yellow Sea
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Peridiniales
New investigation of the cyst–motile relationship for Votadinium spinosum reveals a Protoperidinium claudicans species complex (Dinophyceae, Peridiniales)
Taxonomic revision, phylogeny, and cyst wall composition of the dinoflagellate cyst genus Votadinium Reid (Dinophyceae, Peridiniales, Protoperidiniaceae)
Phylogenetic subdivision of the genus Protoperidinium (Peridiniales, Dinophyceae) with emphasis on the Monovela Group
Abstract The genus Protoperidinium is the most diverse of the thecate dinoflagellates in both coastal and offshore environments. This genus consists of c. 300 species ( Hoppenrathetal.2009 ), all of which are completely heterotrophic. Although several different classification schemes in the genus Protoperidinium Berg (formerly the genus Peridinium Ehrenberg) have been proposed by different scientists (e.g. Jörgensen1912 ; Lebour1925 ; Abe´ 1981), the genus has been treated as a well-established taxonomic unit even after the revision of the genus Peridinium by Balech (1974). Since the plate formula and the shape of each plate developed in Protoperidinium species are stable, the combination of plate topology and shape have been regarded as key features for subdivision within the genus and identification of species.