foraminifer

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for·a·min·i·fer

 (fôr′ə-mĭn′ə-fər, fŏr′-) also fo·ram·i·nif·er·an (fə-răm′ə-nĭf′ər-ən)
n.
Any of numerous chiefly marine protozoans of the order (or phylum) Foraminifera, characteristically having a calcareous shell with perforations through which numerous pseudopods protrude. The shells accumulate on the ocean floor as sediment.

[From New Latin Forāminifera, order name : Latin forāmen, forāmin-, an opening + Latin -fer, -fer.]

fo·ram′i·nif′er·al adj.

foraminifer

(ˌfɒrəˈmɪnɪfə)
n
(Biology) any marine protozoan of the phylum Foraminifera, having a shell with numerous openings through which cytoplasmic processes protrude. Often shortened to: foram See also globigerina, nummulite
[C19: from New Latin, from foramen + -fer]
foraminiferal, foˌramiˈniferous adj

for•a•min•i•fer

(ˌfɔr əˈmɪn ə fər, ˌfɒr-)

n.
any chiefly marine protozoan of the order Foraminifera, typically having a linear, spiral, or concentric shell perforated by small holes or pores through which pseudopodia extend.
[1835–45; < New Latin Foraminifera < Latin foramen]
ThesaurusAntonymsRelated WordsSynonymsLegend:
Noun1.foraminifer - marine microorganism having a calcareous shell with openings where pseudopods protrudeforaminifer - marine microorganism having a calcareous shell with openings where pseudopods protrude
rhizopod, rhizopodan - protozoa characterized by a pseudopod
globigerina - marine protozoan having a rounded shell with spiny processes
nummulite - large fossil protozoan of the Tertiary period
References in periodicals archive ?
The presence of reef forming organisms (bryozoans, foraminifers, echinoderms, and bivalves) support this model.
The UE consists of greenish marlaceous clays with silicon sandstone inter-layers, foraminifers, shales of ostracordes.
Reillustration and Revised Taxonomy for Selected Deepsea Benthic Foraminifers.
The foraminifers are abundant and benthic foraminifera strongly dominate the assemblages, the P/B ratio being 11%.
The Sakesar Limestone is rich in fossil assemblage including foraminifers, mollusks and ostracodes, (Davies and Pinfold, 1937) carried out the pioneering work on the foraminiferal biostratigraphy of the marine lower tertiary succession in the Salt Range.
The distribution of different larger foraminifers species from Kalarwahan Gorge is shown in (Fig.
Molecular evidence of cryptic speciation in planktonic foraminifers and their relation to oceanic provinces.
Also, there are rarely planktonic foraminifers including non-keeled Globigerinids.
Late Pliocene to Holocene benthic foraminifers of the Guaymas Basin, Gulf of California: Sites 477 through 481.