1995
DOI: 10.1073/pnas.92.1.141
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Origin of the foraminifera.

Abstract: We report nuclear small-subunit rDNA sequences for two species of the benthic foraminifer Ammonia. Because of their abundance in present and past seas, the foraminifera are a very important group of organisms used in a wide range of geologic studies; however, the ancestry of this group was, until now, unknown. Difficulties in purifying foraminiferal DNA and avoiding PCR contamination led us to develop DNA.DNA in situ hybridization techniques to verify our sequence data. Phylogenetic analysis of verified forami… Show more

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Cited by 29 publications
(5 citation statements)
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“…Geographical mapping of the polyrhabdinid environmental samples reveals their worldwide distribution: deep sea sediment from the East Sea ( Park et al, 2008 ), sediment from seashores of Denmark ( Karst et al, 2018 ), sediment of mangrove system in Brazil ( Santos et al, 2010 ), methane cold seep in Sagami Bay in Japan, the tidal flat on Disko Island near Greenland, Cariaco basin in the Caribbean Sea near Venezuela, marine stromatolites near the Bahamas ( Baumgartner et al, 2009 ; Stoeck, Taylor & Epstein, 2003 ; Stoeck et al, 2007 ; Takishita et al, 2007 ), and a clone derived from the foraminiferan Ammonia beccarii ( Wray et al, 1995 ). The identification of the latter sequence as a foraminiferan was refuted ( Pawlowski et al, 1996 ), and it probably originated by either pseudoparasitism, occasional ingestion of a gregarine oocysts by the foraminiferan (see Rueckert et al (2011) for similar cases of misidentification).…”
Section: Discussionmentioning
confidence: 99%
“…Geographical mapping of the polyrhabdinid environmental samples reveals their worldwide distribution: deep sea sediment from the East Sea ( Park et al, 2008 ), sediment from seashores of Denmark ( Karst et al, 2018 ), sediment of mangrove system in Brazil ( Santos et al, 2010 ), methane cold seep in Sagami Bay in Japan, the tidal flat on Disko Island near Greenland, Cariaco basin in the Caribbean Sea near Venezuela, marine stromatolites near the Bahamas ( Baumgartner et al, 2009 ; Stoeck, Taylor & Epstein, 2003 ; Stoeck et al, 2007 ; Takishita et al, 2007 ), and a clone derived from the foraminiferan Ammonia beccarii ( Wray et al, 1995 ). The identification of the latter sequence as a foraminiferan was refuted ( Pawlowski et al, 1996 ), and it probably originated by either pseudoparasitism, occasional ingestion of a gregarine oocysts by the foraminiferan (see Rueckert et al (2011) for similar cases of misidentification).…”
Section: Discussionmentioning
confidence: 99%
“…This feature of the method is highly relevant to studies of systematics as well as the ecological studies addressed here. Species‐specific oligonucleotides can also be coupled to a fluorophore or radioisotope and used as a probe for in situ hybridization (Wray et al 1995). By this method, a DNA sequence can be used to identify a morphological type of foraminiferan that corresponds to a particular molecular type.…”
Section: Discussionmentioning
confidence: 99%
“…The new sequence from S. serpulae was aligned with 51 other alveolate SSU rDNA sequences using MacClade 4 (D. R. Maddison & W. P. Maddison 2000) and visual fine‐tuning. The apicomplexan sequence misattributed to the foraminiferan Ammonia beccarii (U07937) was omitted from the analyses because this sequence is missing data (Wray et al . 1995; Leander et al .…”
Section: Methodsmentioning
confidence: 99%