sch28 | This vegetation was formerly classified within the Rhynchosporion together with moderately rich minerotrophic fens. I suggest that recognising a separate alliance for ombrotrophic bog hollows is ecologically sensible because all ecological classifications of mires use ombrotrophic and minerotrophic conditions as the leading classification criteria. Dengler et al. (2004) proposed to separate bog hollows from the Scheuchzerio-Caricetea fuscae. Because the Rhynchosporion albae was described from minerotrophic fens, the latter name cannot be used for the vegetation classified here as the Scheuchzerion palustris. (M. Hájek) K. Dierssen disagrees with this solution.
Synonyms
Caricion rotundatae Kalliola 1939
(2b)
– sch30 Kalliola (1939) referred to the Scheuchzerion palustris as a synonym of the Caricion rotundatae Kalliola, hence the latter name become nomen superfluum even though the relevés presented in his paper correspond rather to the Caricion fuscae or to the Stygio-Caricion limosae. (M. Hájek, L. Mucina).
Leuko-Scheuchzerion palustris Nordhagen 1943
(2b)
Molinio caeruleae-Rhynchosporion albae (Koch 1926) de Foucault 1984
(29a)
Rhynchosporion albae sensu auct., non Koch 1926
(pseudonym)
Sphagnion baltici Kustova in Lapshina 2010
(syntax.syn.)
Sphagnion baltici Kustova 1987
(1)
Sphagnion cuspidati Krajina 1933 nom. dubium
(38)
– sch29 Krajina (1933) used extremely large plots (100-800 m2) and besides bog hollows his relevés covered also the surrounding wetland and scrub. Krajina himself synonymised, with question mark, this alliance with the Sphagnion fusci (i.e., the Oxycocco-Sphagnetea hummocks). Although the name characterises bog hollows well, the type relevés are too heterogeneous and therefore the name should be considered as nomen dubium. (M. Hájek).
Sphagnion cuspidati Krajina 1934
(phantom)
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