Polysaccammina ipohalina Scott, 1976b

Camacho, S, Moura, D, Connor, S, Scott, DB & Boski, T, 2015, Taxonomy, ecology and biogeographical trends of dominant benthic foraminifera species from an Atlantic-Mediterranean estuary (the Guadiana, southeast Portugal), Palaeontologia Electronica 52 (4), pp. 1-37 : 17

publication ID

https://doi.org/ 10.26879/512

persistent identifier

https://treatment.plazi.org/id/6C046402-FF90-FFF3-ED38-FB37780700D8

treatment provided by

Felipe

scientific name

Polysaccammina ipohalina Scott, 1976b
status

 

Polysaccammina ipohalina Scott, 1976b View in CoL

Figure 2.1-3 View FIGURE 2 View FIGURE 3

1976b Polysaccammina ipohalina Scott : p. 316, pl. 2, figs. 1-4, text fig. 4a-c.

1980 Polysaccammina ipohalina Scott ; Scott and Medioli, p. 43, pl. 2, figs. 8-11.

1991 Polysaccammina ipohalina Scott ; Scott, Suter and Kosters, p. 386, pl. 2, fig. 3.

2005 Polysaccammina ipohalina Scott ; Barbosa, Scott, Seoane, and Turcq, p. 40, pl. 1, fig. 12.

Morphological description. Test free, finely arenaceous with pseudochitinous base; globular chambers, irregularly shaped, in uniserial arrangement but sometimes irregularly developed; with terminal aperture; test is flexible at sutures; earlier chambers appear to collapse; sutures distinct and depressed; arenaceous outer layer is not continuous between chambers.

Occurrence. Dominant species along with Jadammina macrescens and Trochammina inflata . Narrow occurrence, recorded only in one site in the Guadiana, in the vegetated margin of a saltworks pond which feeds salt-pans reservoirs, during summer, at 1.96 m above MSL.

Remarks. Its amorphous aspect and similarities with organic matter debris could hinder identification of this taxon as it is rarely mentioned in other works concerning marsh and estuarine foraminiferal analysis. The species was originally described as non-attached; however, many of the species observed in Nova Scotia (Scott and Medioli, 1980) and in the present work were attached to organic debris ( Figure 2.1-3 View FIGURE 2 View FIGURE 3 ).

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