Waernia mirabilis gen. nov., sp. nov. (Dumontiaceae, Gigartinales): A new noncoralline crustose red alga from the northwestern Atlantic Ocean and its relationship to Gainia and Blinksia

Authors: Wilce, R.T., Maggs, C.A. and Sears, J.R.

Journal: Journal of Phycology

Volume: 39

Issue: 1

Pages: 198-212

ISSN: 0022-3646

DOI: 10.1046/j.1529-8817.2003.02037.x

Abstract:

Waernia mirabilis Wilce, Maggs et Sears, gen. et sp. nov., is described for an encrusting red alga endemic to the northeastern North Atlantic Ocean. Its perennial thalli form major understory populations that may outcompete Corallinaceae and Hildenbrandiaceae in some habitats. Crustose red algae with isomorphic gametophytes and tetrasporophytes other than Corallinaceae are poorly known; Waernia differs vegetatively and reproductively from any other such algae. Gametangia are similar to those of the monotypic uncalcified crustose genera Blinksia and Gainia endemic to the Antarctic and central coastal California, respectively. Comparison of Waernia with type material of Blinksia californica Abbott & Hollenberg and Gainia mollis Moe shows that it differs from Blinksia in lacking cohesive crusts in which adjacent cells cohere by direct fusions and by its strongly recurved, rather than straight, carpogonial branches. Gainia and Waernia both have strongly recurved carpogonial branches and laxly constructed crusts that lack secondary pit connections. Gainia differs from Waernia in its considerably larger and thicker crusts, non-nemathecial tetrasporangia, shorter carpogonial branches, and its consistently single gonimoblast initial. We continue to recognize the family Blinksiaceae as a probable member of the Gigartinales with uncertain affinities. Waernia is assigned to the Dumontiaceae (Gigartinales), as its first described isomorphic crustose member. It is also the only genus and one of few algal species endemic to northeastern North America. Waernia either arrived at its present distribution via migration from a Tertiary polar ocean or evolved from an unknown ancestor in a newly formed boreal northwest Atlantic Ocean during post-Oligocene millennia.

Source: Scopus