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Foraminifera taxon details

Checked: verified by a taxonomic editorFissurina orbignyana variabilis (Wright, 1891) 
AphiaID: 466552

Classification: Biota > Checked: verified by a taxonomic editorChromista (Kingdom) > Checked: verified by a taxonomic editorHarosa (Subkingdom) > Checked: verified by a taxonomic editorRhizaria (Infrakingdom) > Checked: verified by a taxonomic editorForaminifera (Phylum) > Checked: verified by a taxonomic editorForaminifera incertae sedis (Class) > Checked: verified by a taxonomic editorLagenida (Order) > Checked: verified by a taxonomic editorPolymorphinoidea (Superfamily) > Checked: verified by a taxonomic editorEllipsolagenidae (Family) > Checked: verified by a taxonomic editorEllipsolageninae (Subfamily) > Checked: verified by a taxonomic editorFissurina (Genus) > Checked: verified by a taxonomic editorFissurina orbignyana (Species)
Status Unaccepted: synonym, or anything that is not accepted unaccepted
Accepted name  Checked: verified by a taxonomic editorPalliolatella variabilis (Wright, 1891)
Rank Subspecies
Parent Checked: verified by a taxonomic editorFissurina orbignyana Seguenza, 1862
Synonymised
names
  Checked: verified by a taxonomic editorLagena orbignyana var. variabilis (Wright, 1891)
Source Not documented
Environment marine
Distribution 
From editor or global species database
North Atlantic Ocean
Checked: verified by a taxonomic editorEast U.S. Continental Shelf [details]
(no group)
Checked: verified by a taxonomic editorNew Zealand Exclusive Economic Zone [details]
Attribute Unreviewed: has not been verified by a taxonomic editorFunctional group benthos » Stage adult (inherited from Checked: verified by a taxonomic editorForaminifera) [details]
Checked: verified by a taxonomic editorFossil range Phanerozoic > Mesozoic > Cretaceous > Cretaceous, Upper (100.5 Ma) (inherited from Checked: verified by a taxonomic editorFissurina orbignyana Seguenza, 1862) [details]
Checked: verified by a taxonomic editorFossil range Phanerozoic > Cenozoic > Paleogene > Paleocene (66.0 Ma) (inherited from Checked: verified by a taxonomic editorFissurina orbignyana Seguenza, 1862) [details]
Checked: verified by a taxonomic editorFossil range Phanerozoic > Cenozoic > Paleogene > Eocene (56.0 Ma) (inherited from Checked: verified by a taxonomic editorFissurina orbignyana Seguenza, 1862) [details]
Checked: verified by a taxonomic editorFossil range Phanerozoic > Cenozoic > Paleogene > Oligocene (33.9 Ma) (inherited from Checked: verified by a taxonomic editorFissurina orbignyana Seguenza, 1862) [details]
Checked: verified by a taxonomic editorFossil range Phanerozoic > Cenozoic > Neogene > Miocene (23.03 Ma) (inherited from Checked: verified by a taxonomic editorFissurina orbignyana Seguenza, 1862) [details]
Checked: verified by a taxonomic editorFossil range Phanerozoic > Cenozoic > Quaternary > Pleistocene (2.558 Ma) (inherited from Checked: verified by a taxonomic editorFissurina orbignyana Seguenza, 1862) [details]
Checked: verified by a taxonomic editorFossil range Phanerozoic > Cenozoic > Quaternary > Holocene (0.0117 Ma) (inherited from Checked: verified by a taxonomic editorFissurina orbignyana Seguenza, 1862) [details]
Checked: verified by a taxonomic editorFossil range Phanerozoic > Cenozoic > Neogene > Pliocene (5.333 Ma) (inherited from Checked: verified by a taxonomic editorFissurina orbignyana Seguenza, 1862) [details]
ImageChecked: verified by a taxonomic editor 
Lagena orbignyana variabilis
Lagena orbignyana vari...
[image from synonym]
LSID urn:lsid:marinespecies.org:taxname:466552
Taxonomic
Edit history
 
Date   action   by
2010-03-26 06:48:17Z  created  Hayward, Bruce
2013-06-25 02:18:40Z  changed  Hayward, Bruce
  
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  Citation: Hayward, B. (2014). Fissurina orbignyana variabilis (Wright, 1891). In: Hayward, B.W., Cedhagen, T., Kaminski, M., Gross, O. (2014) World Foraminifera Database. Accessed through: Hayward, B.W., Cedhagen, T., Kaminski, M., Gross, O. (2014) World Foraminifera Database at http://www.marinespecies.org/foraminifera/aphia.php?p=taxdetails&id=466552 on 2014-09-23
  

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