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Foraminifera
Sign in to saveForaminifera ( ; Latin for "hole bearers"; informally called "forams") are single-celled organisms, members of a phylum or class of Rhizarian protists characterized by streaming granular ectoplasm for catching food and other uses; and commonly an external shell called a test of diverse forms and materials. Tests of chitin (found in some simple genera, and Textularia in particular) are believed to be the most primitive type. Most foraminifera are marine, the majority of which live on or within the seafloor sediment (i.e., are benthic, with different sized species playing a role within the macro
Foraminifera are single-celled ocean organisms with streaming cytoplasm for feeding and typically an external shell, making them among the most abundant life forms in marine sediments. They matter because they play important ecological roles on the seafloor and their shells are commonly used by scientists to study ocean history and conditions.
AI-generated from the Wikipedia summary — may contain errors.
Species
foraminiferans
Foraminifera
PHYLUM
- KingdomChromista
- PhylumForaminifera
via GBIF
Museum specimens
- Specimen records
- 16,471
- With media
- 7,835
- Collections
- LACM, NHMUK, USNM
- Recorded in
- United States, United Kingdom
Research
1,295 papers- Foraminifera as bioindicators of water quality: The FoRAM Index revisited.ReviewEnvironmental pollution (Barking, Essex : 1987) · 2020Prazeres M, Martínez-Colón M, Hallock PDOI: 10.1016/j.envpol.2019.113612
- Foraminifera and plastic pollution: Knowledge gaps and research opportunities.ReviewEnvironmental pollution (Barking, Essex : 1987) · 2023Bouchet VMP, Seuront L, Tsujimoto A et al.DOI: 10.1016/j.envpol.2023.121365
- Insights from Fossil-Bound Nitrogen Isotopes in Diatoms, Foraminifera, and Corals.ReviewAnnual review of marine science · 2023Robinson RS, Smart SM, Cybulski JD et al.DOI: 10.1146/annurev-marine-032122-104001
- Foraminifera as a model of eukaryotic genome dynamism.mBio · 2024Timmons C, Le K, Rappaport HB et al.DOI: 10.1128/mbio.03379-23
- Biocalcification in porcelaneous foraminifera.eLife · 2024Dubicka Z, Tyszka J, Pałczyńska A et al.DOI: 10.7554/eLife.91568
- Are physiological responses in foraminifera reliable environmental stress bioindicators? A systematic review.Environmental research · 2023Tavera Martínez L, Marchant M, Urbina MDOI: 10.1016/j.envres.2022.114515
- Global diversity patterns of larger benthic foraminifera under future climate change.ReviewGlobal change biology · 2023Förderer EM, Rödder D, Langer MRDOI: 10.1111/gcb.16535
- Benthic Foraminifera as Pollution Biomarkers: a Morphological Approach.Microbial ecology · 2023Martínez LT, Marchant M, Díaz RTA et al.DOI: 10.1007/s00248-023-02282-y
via PubMed
~41 min read
Encyclopedic overview
13 sectionsContents
- History of study
- Taxonomy
- Anatomy
- Ecology
- Reproduction
- Variations in reproductive mode
- Tests
- Evolutionary history
- Paleontological applications
- Modern uses
- Gallery
- See also
- External links
Foraminifera ( ; Latin for "hole bearers"; informally called "forams") are single-celled organisms, members of a phylum or class of Rhizarian protists characterized by streaming granular ectoplasm for catching food and other uses; and commonly an external shell called a test of diverse forms and materials. Tests of chitin (found in some simple genera, and Textularia in particular) are believed to be the most primitive type. Most foraminifera are marine, the majority of which live on or within the seafloor sediment (i.e., are benthic, with different sized species playing a role within the macrobenthos, meiobenthos, and microbenthos), while a smaller number float in the water column at various depths (i.e., are planktonic), which belong to the suborder Globigerinina. Fewer are known from freshwater or brackish conditions, and some very few (nonaquatic) soil species have been identified through molecular analysis of small subunit ribosomal DNA.
Foraminifera typically produce a foraminifera test, or shell, which can have either one or multiple chambers, some becoming quite elaborate in structure. These shells are commonly made of calcium carbonate () or agglutinated sediment particles. Over 50,000 species are recognized, both living (6,700–10,000) and fossil (40,000). They are usually less than 1 mm in size, but some are much larger, the largest species reaching up to 20 cm.
Excerpted from Wikipedia’s “Foraminifera” article, available under the CC BY-SA 4.0 licence.