Offprint Mass Development of Marine Benthic Sarcinochrysidales

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Offprint Mass Development of Marine Benthic Sarcinochrysidales Offprint Botanica Marina Vol. 43, 2000, pp. 223—231 © 2000 by Walter de Gruyter • Berlin • New York Mass Development of Marine Benthic Sarcinochrysidales (Chrysophyceaes.l .) in Corsica L. Hoffmann3*, C. Billardb, M. Janssens3, M. Leruth3 and V. Demoulin3 a University of Liège, Institute of Botany (B. 22), Sart Tilman, B-4000 Liège, Belgium b University of Caen, Laboratoire de Biologie & Biotechnologies Marines, Esplanade de la Paix, F-14032 Caen, France * Corresponding author A mass development of benthic Sarcinochrysidales (Chrysophyceae s.L), especially of Chrysoreinhardia gi­ raudii comb. nov. (basionym: Tetraspora giraudii) and Nematochrysopsis marina comb. nov. (basionym: Tribonema marinum), is reported from the Corsican coast. Morphology, habitat and seasonal development of these taxa as well as of the less regularly observed Chrysonephos lewisii and of some Chrysophyceae s.l. associated with Chrysoreinhardia giraudii sheaths are presented. Introduction The benthic algal vegetation of the Bay of Calvi (north-western coast of Corsica) has been monitored Large-scale mucilage accumulation events due to dif­ since the late sixties. Since 1987, great changes have ferent types of planktonic or benthic algae have occurred in the structure of this vegetation. Indeed, plagued different seas in recent years (Vollenweider the Cystoseira communities which dominated all the and Rinaldi 1995). Pelagic mucilage formation is well rocky substrates until 1987 have been subject to a known in the North Sea where mucilage from Phaeo­ dramatic regression of their cover and biomass (Hoff­ cystis (Haptophyta) colonies can produce great quan­ m ann et al. 1988, Janssens et al. 1993 and unpub­ tities of foam accumulating along the coasts lished observations by Demoulin and coworkers). At (Lancelot 1995). In the Adriatic Sea several diatom the same time several benthic macroalgae (Janssens species [especially Cylindrotheca closterium (Ehren­ et al. 1993), especially nitrophilous species such as berg) Lewin et Reimann, Chaetoceros affinis Lauder Cladophora prolifera (Roth) Klitzing and Colpomenia and Skeletonema costatum (Greville) Cleve] are re­ sinuosa (Mertens et Roth) Derbès et Solier, as well as sponsible for large-scale pelagic mucilage production epiphytic microalgae (e. g. Bangiophyceae) (Hoff­ (Degobbis et al. 1995, Mingazzini and Thake 1995), m ann et al. 1994) show a clear progression. In addi­ as has also been observed along other European tion, massive development of mucilaginous benthic coasts (e. g. Boalch and H arbour 1977 off the coast microalgae was observed, the most conspicuous com­ of south-west England). Benthic mucilaginous aggre­ ponents of these mucilages are palmelloid and fila­ gates have mainly been described from the Tyrrhen­ mentous Sarcinochrysidales (Chrysophyceae s.l.). ian Sea (Rinaldi et al. 1995, Diviacco 1992, Giaccone The order Sarcinochrysidales was erected by 1992, Cinelli 1992, Rinaldi 1992, Tnnamorati 1992, Gayral and Billard (1977) and included marine Sartoni and Sonni 1992, Tnnamorati 1995). The most Chrysophyceae characterised by having motile cells frequently reported taxa from these benthic commu­ similar to those of brown algae. On ultrastructural nities are Tribonema marinum J. Feldmann (formerly and phytochemical grounds the homogeneity of this considered to be a member of the Tribonematales, group has been questioned (Billard 1984, see also Bil­ Xanthophyceae), Acinetospora crinita (Carmichael ex lard et al. 1990), followed by O ’Kelly (1989) and Sar­ Harv.) Sauvageau (Ectocarpales, Phaeophyceae), toni et al. (1994). Small subunit ribosomal RNA se­ Microcoleus lyngbyaceus (Klitzing) Crouan (Oscilla­ quences confirmed the difference between the Sarci­ toriales, Cyanophyceae; this name usually covers a nochrysidales V str. and the order Chrysomeridales variety of filamentous blue-green algae) and Lopho­ that still lacks formal description (Saunders et al. cladia lallemandii (Montagne) Schmitz (Ceramiales, 1997). A tendency exists to multiply classes among Rhodophyceae) (Giaccone 1992). The causes of these the heterokont algae and the Sarcinochrysidophyceae mucilaginous aggregates are still subject to discus­ has been provisionally introduced by van den Hoek sion. The development of the Phaeocystis blooms in et al. (1995), while Saunders et al. (1997) favour an the N orth Sea (Lancelot 1995) is apparently due to inclusion in the Pelagophyceae which may not con­ the increase of N relative to P and especially silica. vince those who want a strong morphological basis Mucilage development in the Adriatic Sea also seems for taxa. Several taxa have still not been studied for to depend largely on the N/P ratio, the physical envi­ some critical ultrastructural, chemical or molecular ronment and climatic conditions (Rinaldi et al. 1995). characters and a final decision seems premature to Brought to you by | Artesis Hogeschool Antwerpen (Artesls Hogeschool Antwerpen) Authenticated | 172.16.1.226 Download Date | 1/10/12 10:02 AM 224 L. Hoffmann et al us. However, it should be clear that we are referring respectively. In 1989, however, the attention of one here to organisms belonging to the order Sarcinoch­ of the authors (V. D. ) was drawn to their abundance rysidales s. str. within the Chrysophyceae s. I. and possible link to the Cystoseira regression. Besides The purpose of this paper is to give an account of Acinetospora crinita, different diatoms and blue-green the benthic chrysophycean flora of the Corsican algae (especially from the genera Hydrocoleum and coast, especially of the Calvi area, together with an Pseudanabaena), form mucilaginous aggregates outline of the seasonal pattern and habitat of the which, however, are dominated by different species most frequently encountered species. of the order Sarcinochrysidales, the most frequently observed being Chrysoreinhardia giraudii and Nema­ tochrysopsis marina and more locally Chrysonephos Materials and Methods lewisii (Taylor) Taylor. Other Chrysophyceae s.l. are Field observations and collections of specimens were also regularly observed but do not form large aggre­ made by SCUBA diving at several locations on the gates. Corsican coast. Most observations were performed in Revellata Bay near the town of Calvi (north-west Chrysoreinhardia Billard, nom. nov. coast of Corsica) where the benthic algal vegetation Replaced synonym: Pulvinaria Reinhard, Notes de has been regularly monitored since the late sixties, la Société de Chercheurs en Sciences Naturelles de No- and especially since 1988, with repeated samplings at vorosisk, IX, 2: 248, 1885, non Pulvinaria Bonorden, fixed points. The points usually monitored numbered Handb. Mykol.: 272, 1851. 19, regularly distributed along the 12 km shoreline The genus name Pulvinaria used by Reinhard between the harbour of Calvi and the tip of the Punta (1885) is illegitimate because of the earlier homonyms Revellata ( Janssens et al. 1993). Routine observations Pulvinaria Bonorden as well as Pulvinaria Fournier were carried out until the rocky substrates ceased or (Farr et al. 1979, p. 1464). The new name Chrysorein­ down to 15 m depth, deeper on more occasional hardia is therefore proposed. This name has already dives. been suggested several years ago and has provision­ Light microscopical observations were carried out ally been used by some authors but had never been using a Leitz Dialux microscope; photographs, mea­ validly published. surements with a screw micrometer and camera lu­ Type species: Chrysoreinhardia algicola (Reinhard) cida drawings were made from living material. Mate­ Billard comb. nov. rial brought back to Caen was maintained in the en­ Basionym: Pulvinaria algicola Reinhard, Notes de riched seawater medium ES-Tris (Cosson 1973), at la Société de Chercheurs en Sciences Naturelles de No- room temperature under natural daylight illumina­ vorosisk, IX, 2: 248, 1885. tion. Living cells were examined and photographed with a Leitz Orthoplan microscope equipped with in­ In the Calvi area, the genus is represented by the spe­ terference optics. For biomass estimations, the muci­ cies: laginous algae were collected from a 100 cm2 surface. Dry weight was obtained after lyophilisation of the Chrysoreinhardia giraudii (Derbès et Solier) Billard collected material. The organic matter weight (ash- comb. nov. (Figs 3 6) free dry weight) was determined by subtracting from Basionym: Tetraspora giraudii Derbès et Solier, the original dry weight the weight of the ash remain­ Suppl. C. R. Acad. Sei., 8,I: pi. I, figs. 1 -6 , 1856. ing after combustion for 6 h in a muffle furnace at Synonyms: Phaeocystis giraudii (Derbès et Solier) 500 °C. Chlorophyll a concentration was determined Lagerheim, Pulvinaria giraudii (Derbès et Solier) after extraction in 90 % acetone according to Jeffrey Bourrelly (invalid combination: incomplete refer­ and Humphrey (1975). Herbarium specimens are ence). held at the Herbarium of the University of Liège Description: The mucilaginous light brownish colo­ (LG). nies are up to 15 mm in diameter (Fig. 6). Cells are hemispherical to spherical, 7-10 |im in diameter and Results and Discussion are embedded in a homogeneous non-stratified muci- Abundant mucilaginous aggregates have been ob­ served from May to July in different sites on the Cor­ Table I. Observations of macroscopic colonies of Chrysore­ sican coast since 1989. Some of the algae involved inhardia in the Calvi area. were present previously since Nematochrysopsis ma­ rina comb. nov. was already occasionally observed J F M A M J
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