World Foraminifera Database
Current number of valid recent species recorded: 8,955
Current number of valid fossil species recorded: 28,001
Current number of total valid (fossil + recent) species recorded: 36,530
The World Foraminifera Database
This World Database of all species of Foraminifera ever described (recent and fossil), is part of the World Register of Marine Species (WoRMS), a global initiative to provide a register of all marine organisms.
Searching the database (fossil and/or recent)
The default setting is to search the whole database of fossil and recent species. If you would like to only search the recent (living) taxa then tick the 'extant' box in the Taxon Search window.
What are Foraminifera?
Foraminifera (‘hole bearers’), foraminifers or forams for short, are a large phylum of amoeboid protozoans (single celled) with reticulating pseudopods, fine strands of cytoplasm that branch and merge
to form a dynamic net. They usually produce a test (or shell) which can have one or more chambers, and are made of calcium carbonate (CaCO3) or mineral grains or other particles glued together.
The tests are usually less than 0.5 mm in size, but the largest can be up to 20 cm across. Foraminifera are among the most abundant and scientifically important groups of organisms.
The tests of recently dead planktic foraminifera are so abundant that they form a thick blanket over one third of the surface of the Earth (as Globigerina ooze on the ocean floor).
Foraminifera are essentially marine and estuarine-dwelling protozoans living in all environments from the greatest depths right up to highest astronomical tide level and from the equator to the poles.
The importance of foraminifera comes from the use of their fossil tests in biostratigraphy, paleoenvironment studies, and isotope geochemistry. Their ubiquity in most marine sedimentary rocks,
often as large, well-preserved, diverse assemblages, has resulted in their being the most studied group of fossils worldwide. Because recent foraminifera have attracted little interest from biologists,
paleontologists have been forced to undertake most studies, including genetic research, on the living fauna.
This site has the following aims:
- to provide a catalogue of the world's foraminiferal species
- to promote stability in foraminiferal nomenclature
- to act as a tool for higher taxonomic revisions and regional monographs
The list of currently accepted species-group names is at least 90% complete for recent species, but the taxonomy of many taxa still
needs revision and newly described species will be added as soon as possible after publication, a task that will be undertaken continuously by the editors.
Fossil genera and higher taxa are mostly complete but fossil species will take many years to add in. There is currently no broad consensus available for the higher classification of the Foraminifera.
Here, the classification given in Loeblich and Tappan (1987 and 1992) is mostly used for calcareous taxa and Kaminski (2004) is followed for agglutinated taxa, but the higher level classification of
Foraminifera is in a state of revision and has been updated to comply with the genetic sequence-based results to date of Pawlowski et al. (2013) and Holzmann and Pawlowski (2017). Further results of ongoing molecular phylogenetic
investigations will hopefully help to stabilise the taxonomic system in the future.
- Holzmann, M. and Pawlowski, J. (2017). An updated classification of rotaliid foraminifera based on ribosomal DNA phylogeny. Marine Micropaleontology 132, 18-34.
- Kaminski, M. A. (2004). The Year 2000 Classification of the Agglutinated Foraminifera. In: M. K. Bubik, Ma. (ed). Proceedings of the Sixth International Workshop on Agglutinated Foraminifera. Grzybowski Foundation Special Publication. Pp. 237-255.
- Loeblich, A. R., and Tappan, H. (1987). "Foraminiferal genera and their classification." Van Nostrand Reinhold, New York.
- Loeblich, A. R., and Tappan, H. (1992). Present status of foraminiferal classification. In "Studies in Benthic foraminifera. Proceedings of the Fourth Symposium on benthic foraminifera, Sendai, 1990." (Y. Takayanagi, and T. Saito, Eds.), pp. 93-102. Tokai University Press, Tokyo.
- Pawlowski, J., Holzmann, M., Tyszka, J. (2013). New supraordinal classification of Foraminifera: Molecules meet morphology. Marine Micropaleontology 100, 1-10
A steering committee provides international oversight and fosters the compilation and rationalisation of the World Foraminifera Database.
The Steering Committee members are:
Enter data and make taxonomic decisions in the groups they have responsibility for:
Editors are responsible for entries, decision on validity of names. Corrections and omissions may be addressed to either editor.
Acceptance of a species in the database is an editorial decision, but we acknowledge such decisions need to be re-examined frequently in the light of new information. If you disagree with senior synonymy decisions or genus assignments, please let us have your well-argued-corrected assignment. Only the editors can add or modify the data, but anybody can upload images with identifications and location information, although this will be checked and can be modified by the editors
History of the World Foraminifera Database
The World Foraminifera Database began as the European recent species list compiled by Tomas Cedhagen and Onno Gross. Added to this in 2010 were the Gulf of Mexico recent species list compiled by Barun Sen Gupta and colleagues and the New Zealand modern species list compiled by Bruce Hayward and colleagues.
- Gross, O. (2001). Foraminifera, in: Costello, M.J. et al. (Ed.) (2001). European register of marine species: a check-list of the marine species in Europe and a bibliography of guides to their identification. Collection Patrimoines Naturels, 50: 60-75.
- Hayward, B.W., Tendal, O.S., Carter, R., Grenfell, H.R., Morgans, H.E.G., Scott, G.H., Strong, C.P., Hayward, J.J. (2012). Phylum Foraminifera. Foraminifera and Xenophyophores. In: Gordon, D.P. (ed.). New Zealand Inventory of biodiversity: A Species 2000 Symposium Review. Canterbury University Press,. Christchurch. Pp. 242-287
- Sen Gupta, B.K., Smith, L.E., Machain-Castillo, M.L. (2009). Foraminifera of the Gulf of Mexico, Pp. 87–129 in Felder, D.L. and D.K. Camp (eds.), Gulf of Mexico–Origins, Waters, and Biota. Biodiversity. Texas A&M Press, College Station, Texas.
Since then records have been added from Johannes Pignatti’s catalogue of recent foraminifera, many major atlases of Recent foraminifera and output from Ellis and Messina Catalogue of Foraminifera. We are aware that many taxa described since 1980 have yet to be found and added
Who described the largest number of recent Foraminiferal species?
- McCulloch – 2429
- Cushman – 1134
- D’Orbigny – 691
- Brady – 398
- Saidova – 394
- Earland - 306
The literature library currently contains ~9000 references, many of the older works are available as scanned PDFs.
The Photogallery currently contains ~6000 images linked to species records, mostly entered by Tomas Cedhagen from Brady’s Challenger volume and Cushman monographs, but also some other monographs.
Links to other Foriminiferal sites
To assist the beginner or the non-specialist we provide here a selection of links to foraminiferal websites for further information.
By downloading or consulting data from this website, the visitor acknowledges that he/she agrees to the following:
If data are extracted from this website for secondary analysis resulting in a publication, the website should be cited as follows:
- Hayward, B.W.; Le Coze, F.; Gross, O. (2017). World Foraminifera Database. Accessed at http://www.marinespecies.org/foraminifera on 2017-09-21
If any data constitutes a substantial proportion of the records used in secondary analyses (i.e. more than 25% of the data are derived from this source, or the data are essential to arrive at the conclusion of the analysis), the authors/managers of the database should be contacted. It may be useful to contact us directly in case there are additional data that may strengthen the analysis or there are features of the data that are important to consider but may not have been apparent from the metadata.
The World List is a searchable catalogue of species and higher taxa names.
Navigating this catalogue starts with clicking on one of the choices in the menu, which you find on the top of each page
- Introduction will lead you this introductory section
- Search taxa will lead to a query page through which all taxon pages can be accessed
- Browse taxa will lead to a taxonomic tree
- Checklist will lead to a query page in which a geounit can directly be picked if the exact name of the unit is already known. This way a list of taxa for a given area can be found quickly.
- Attributes will lead to a page to query (mainly) fossil ranges
- Stats some statistics about the World Foraminifera Database
- Sources will lead to a query page for References of Foraminifera literature.
- Images will lead to photogallery with images
- Login only available to editors.
For each foraminiferal species or infraspecific taxon, accepted or not, there may be the following entries:
- genus name
- the subgenus name, if applicable,
N.B. subgenus names do not need to be cited at all times according to the ICZN; acceptance of combinations without subgenus names is considered ‘alternative representation’ in the database.
- the species name
- the infraspecific name, if applicable
- the author and year of the species name, without or with brackets depending on whether it is the original combination or not
- The AphiaID (a unique numerical database identifier)
- The higher classification (according to Loeblich and Tappan, 1990, 1992)
- The status as ‘accepted’ or ‘unaccepted’ (if applicable; junior synonymy is usually based on published revision)
- Record status (indicates who checked the record)
- Rank of taxon, e.g. species
- Parent: immediately higher taxon, e.g. genus, to which the present taxon belongs
- Synonymized taxa: the list of junior synonyms linked to the present name
- Sources: literature reference of the original description and if applicable to a recent revision (as the ‘basis of the record’).
- Child taxa: all immediate subordinate taxa, e.g. subspecies
- Environment: marine or brackish
- Fossil range: recent only or also known as fossil (soon epoch ranges will be available)
- Distribution: indication of the recent geographic distribution of the taxon, at least based on the origin of the holotype,
Different geounits may be indicated, preferably the Marine Ecoregion (see Spalding et al. 2007), but frequently also the country’s Exclusive Economic Zone. The distribution areas of the junior synonyms are automatically shown with each ‘accepted species’
- Specimen: type specimen information, or published specimen information
- Links: to other foraminiferal resources, to images and other information on specific servers. Current general links are: Genbank, etc.
- Notes: any further relevant information, including descriptions, comments, explanations, etc.
- Images: photos or other images uploaded to the site
We prefer ‘objective’ images of the taxa, such as photos or illustrations of type specimens. We do not encourage photos of unidentified foraminifera, but reliably identified copyright free images are welcome.
- LSID notation: (similar to ISBN in publications)
- Edit history: date of entry and changes made, name of editor
- Links to a Taxonomic tree, Google, Google Scholar and Google images.
The records on higher taxa generally have the same structure as those of the species records. Not all of the above items already exist for all taxa entered in the database, but they will be added as time permits.
What you can do with this database at this time is find out what the currently accepted combination is of your subject foraminifer, what its currently accepted higher taxon affiliation is, and from where it was originally described. You can also check which accepted species occur in a higher taxon. What you cannot (yet) do is find every published combination of genus and species name, as we have given priority so far to the original and the currently accepted combinations (so non-original non-accepted combinations are frequently still lacking). What you also cannot do comprehensively is trace the distributions of species and higher taxa or extract regional lists of species, because there is as yet no consistency in the data entered from around the world.