{"refrec":{"BRefID":124472,"RR":"<b>Gooday, A.J.; Todo, Y.; Uematsu, K.; Kitazato, H.</b> (2008). New organic-walled Foraminifera (Protista) from the ocean's deepest point, the Challenger Deep (western Pacific Ocean). <i>Zool. J. Linn. Soc. 153(3)</i>: 399-423. <a href=\"https://dx.doi.org/10.1111/j.1096-3642.2008.00393.x\" target=\"_blank\">https://dx.doi.org/10.1111/j.1096-3642.2008.00393.x</a>","BEntID":118663,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":0,"RefStringPartII":". <i>Zool. J. Linn. Soc. 153(3)</i>: 399-423. <a href=\"https://dx.doi.org/10.1111/j.1096-3642.2008.00393.x\" target=\"_blank\">https://dx.doi.org/10.1111/j.1096-3642.2008.00393.x</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Gooday, A.J.; Todo, Y.; Uematsu, K.; Kitazato, H.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Gooday, A.J. <i>et al.</i>","Englishabstract":"We describe four new species and a new genus of very small (< 500 µm) Foraminifera from the Challenger Deep, the deepest point in the world's oceans (10 896 m water depth). All have transparent, mainly organic test walls that incorporate some minute agglutinated mineral particles of various shapes and compositions. <i>Nodellum aculeata</i> sp. nov. has an elongate proloculus with a pointed proximal end followed by a long, tubular section. The genus <i>Resigella</i> is represented by two species: in <i>R. laevis</i> sp. nov., the test comprises 3-4 elongate, oval to cylindrical chambers while <i>R. bilocularis</i> sp. nov. has an oval proloculus followed by a second, larger globular chamber. The fourth species, <i>Conicotheca nigrans</i> gen. et sp. nov., is characterized by a tiny, elongate, conical test filled with dark stercomata. Except in <i>C. nigrans</i>, the test wall has a brownish tinge; energy-dispersive spectroscopy (EDS) suggests the presence of organically bound Fe in all species including <i>C. nigrans</i>. Scanning electron microscopy (SEM) combined with EDS reveals distinctive wall structures. In <i>N. aculeata</i>, the proloculus is strewn with tiny (< 0.7 µm), elongate grains. In this species and in <i>R. laevis</i>, the test surface (except for the proloculus) is covered with a carpet of minute (~0.1 µm) finger-like projections, rather similar to the organic cement of agglutinated Foraminifera. In <i>R. bilocularis</i>, the larger second chamber often has a partial veneer of fine mineral grains of varying composition, as well as organic areas consisting of meshed strands. SEM images of these three species reveal flat, plate-like features that we interpret as clay particles. In <i>C. nigrans</i>, the wall is relatively featureless except where the surface is raised into hummocky mounds and scale-like features, again probably clay particles. We suggest that these species represent a distinctive group of 'agglutinated' Foraminifera in which the test is predominately organic. 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Academic Press: London.  ISSN 0024-4082; e-ISSN 1096-3642","StandardTitleSer":"Zoological Journal of the Linnean Society","ISSN":"0024-4082","AbbrevSer":"Zool. J. Linn. 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