Trochammina inflata ( Montagu, 1808 )

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 : 21

publication ID

https://doi.org/ 10.26879/512

persistent identifier

https://treatment.plazi.org/id/6C046402-FF94-FFF7-EFAF-F8707ECC022E

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Felipe

scientific name

Trochammina inflata ( Montagu, 1808 )
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Trochammina inflata ( Montagu, 1808) View in CoL

Figure 3.17-3.21 View FIGURE 3

1808 Nautilus inflatus Montagu : p. 81, pl. 18, fig. 3.

1858 Rotalina inflata (Montagu) ; Williamson, p. 50, pl. 4, figs. 93, 94.

1952 Trochammina inflata (Montagu) ; Parker, p. 459, pl. 3, fig. 1.

1957 Siphotrochammina lobata Saunders : p. 9, pl. 3, figs. 1, 2.

1977 Siphotrochammina elegans Zaninetti, Brönnimann, Beurlen and Moura : pl. 2, figs. 8, 10, 11.

1990 Trochammina inflata (Montagu) ; Scott, Schnack, Ferrero, Espinosa and Barbosa, p. 733, pl. 1, fig. 3.

2005 Trochammina inflata (Montagu) ; Horton, Whittaker, Thomson, Hardbattle, Kemp, Woodroffe and Wright, p. 3, pl. 1, fig 4.

Morphological description. Agglutinated test, trochospirally enrolled, chambers rather inflated, increasing in size gradually; aperture a low arch with a bordering lip; smoothly agglutinated.

Occurrence. Dominant in the living assemblages of the modern estuary; closely related to J. macrescens , occurring together in almost all the samples, although it has higher abundances in middle elevations (0.2 to 0.8 m above MSL at samples E1, LG2 and FB2) where J. macrescens abundance starts to decrease and species diversity starts to increase; like J. macrescens , it is more common in winter.

Remarks. This taxon is the type species of the genus Trochammina ; perhaps the best known and most distinctive of all the endemic marsh species, as well as being one of the earliest species ever described (Scott et al., 2001); the specimens found in Guadiana often present a proteinaceous umbilical tube ( Figure 3.18 View FIGURE 3 ), covered with fine sediment, the purpose of which is unknown.

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