Bol. Soc. Esp. Briol. 46-47: 5-10 (2016)
CINCLIDIUM STYGIUM SW. (MNIACEAE, BRYOPSIDA) IN EASTERN
PYRENEES
Vincent Hugonnot
Le bourg, 43380 Blassac, France. E-mail: vincent.hugonnot@wanadoo.fr
Abstract: Cinclidium stygium Sw. is recorded for the first time in the Pyrenees (PyrénéesOrientales, France) which is a significant south-western extension of its known range,
approximately 400 km. The new locality is described, and recommendations are made for
conservation of the species.
Resumen: Se cita Cinclidium stygium Sw. por primera vez en los Pirineos (Pyrénées-Orientales,
Francia), lo que supone una extensión significativa de su área de distribución hacia el suroeste
de aproximadamente 400 km. Se describe la nueva localidad y se dan recomendaciones para la
conservación de la especie.
Keywords: Mosses, Cinclidium stygium, rich-fen relict, Pyrenees, ecology, Madres.
INTRODUCTION
In the course of bryological surveys in the eastern part of the Pyrenees, several bryophytes
of phytogeographical interest were found. Among them, Cinclidium stygium Sw. deserves to be
mentioned because it had not been previously recorded south of the Alps, which means a
significant southwards extension of its known range.
The worldwide distribution of Cinclidium stygium was reviewed by Mogensen (1973). This
species has a circumpolar distribution in boreal and low-arctic regions in the northern
hemisphere, and a remarkable disjunction in South America. In the Holarctic, its range extends
farther south than the other species of Cinclidium, none of which has been recorded in southern
Europe. Conversely, it is rare or absent in high-arctic regions. In North America, it is widespread
in Canada (Koponen, 1974), from Yukon to Quebec. It is locally frequent in Alaska and
Greenland. The species is widespread in Fennoscandia (Koponen, 1969), in Altaï Mountains
(Ignatov, 1994), and Kamtschatka (Czernyadjeva & Ignatova, 2008), in Switzerland
(http://www.nism.uzh.ch/map/map_en.php), of local occurrence in the north of the British Isles
and Ireland (Blockeel et al., 2014), in Denmark and Germany (Meinunger & Schröder, 2007),
as well as in Poland (Karczmarz, 1962). Its southwestern limit lies in French Alps, where it is
very rare (Sarrassat, 1939). In this country the most important populations are in the Jura (Hétier,
1896; Hillier, 1954).
Cinclidium stygium is experiencing a gradual decline, particularly in the southern part of its
range. It has disappeared from several countries (Netherlands, Belgium), and is hence of
conservation concern. It is for example VU in Ireland, CR in Slovakia, EN in Romania (Hodgetts,
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Boletín de la Sociedad Española de Briología 46–47 (2016)
2015). In France it is protected under the law in the region of Franche-Comté (Arrêté of 22 June
1992, Journal Officiel of 4 August 1992).
This paper intends to report the presence of an isolated population of Cinclidium stygium in
the Pyrenees, as well as to describe its ecology and discuss conservation issues.
STUDY AREA
Madres-Coronat massif occupies a position between the Mediterranean Sea and the first high
summits of the Pyrenean range. The Pic Madres culminates at 2469 m. It is settled less than 60
km from the Mediterranean Sea. The geologic bedrock is mostly composed of schists and granite,
with veins of granodiorite and other magmatic rocks very rich in Ca, Mg, K, etc. The summit
plateau has been carved by glaciers which formed typical U-shaped valleys, where horizontal
sections and drops in elevation alternate. The plateau has been fractured by erosion, and the
cracks are filled with detritic granitic sand that plays the role of an aquifer restituting slowly
accumulated large quantities of water. This may account for the particular abundance of peaty
habitats on the slopes of the massif.
The climate is marked by oceanic influence but strongly modified by altitude. The annual
mean precipitation is 1500-1900 mm at Madres summit. The summer may experience violent
storms. The mean annual temperature is low (around 3°C at 2300 m). Snow is abundant in winter
and may last from November to April in alpine habitats. Cold and dry winds are very frequent.
MATERIAL AND METHODS
This study is based upon examination of fresh and dry collections of plants referable to
Cinclidium stygium from France. The material collected in Pyrénées-Orientales was studied
immediatly after collecting while still fresh. Dry material previously collected by the author in
Southern Alps and Jura was used for morphological comparison.
The new locality is as follows:
FRANCE: Pyrénées Orientales, Mosset, Madrès range, La Balmette d’Avall, 2150 m, in alpine
fens, 42º39’027'‘N; 2º12’013'‘W. Leg. V. Hugonnot, 21 October 2015, Herbarium PyrénéesOrientales 7598, without reproductive organs.
The morphological characters have been assessed in the course of our study from traditional
examination of both dry and fresh plants.
The voucher specimens are deposited in the author’s private herbarium.
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HUGONNOT: CINCLIDIUM STYGIUM SW. (MNIACEAE, BRYOPSIDA) IN EASTERN PYRENEES
Nomenclature of liverworts and mosses follows, respectively, Ros et al. (2007) and Ros et al.
(2013).
RESULTS
The studied material has been confirmed to belong to Cinclidium stygium. However, it has
been found rather variable as far as gametophytes are concerned. Frequently, the plants appeared
with the vegetative parts depauperate, with small leaves, from 1.5 to 2 mm, of ovate to elliptical
outline and an acute apex. The largest leaves (from 3 to 4.5 mm) were oblong to obovate-elliptic,
longer than wide and sharply apiculate. The best developed ones were distinctly petiol-like at
base and had an elongated areolation. The margin was uniformly unistratose. Old portions of
stem were densely tomentose. Macronemata were initiated as indistinct longitudinal lines at the
apex of shoots. No gametangia were observed. At 2 cm deep in the colony, the leaves were
mostly damaged and reduced to their thick nerves, the lamina cells being destroyed.
The colony was composed of an extensive red-blackish mat of densely interwoven stems,
packed into a dense tomentum. The mat was strikingly superficial, not deep, as it is often the
case in floating fens. Here, it did not exceed 2 cm deep, and grew upon a dense and black peat
where no fragments of plants were recognizable.
Cinclidium stygium grew on a very gentle slope (less than 5 deg. of inclination) in a
subalpine Trichophorum cespitosum (L.) Hartm. fen, attributable to Caricion davallianae Klika
1934. Associated bryophytes were not abundant, with Scorpidium cossonii (Schimp.) Hedenäs,
Ptychostomum pseudotriquetrum (Hedw.) J.R.Spence & H.P.Ramsay (C. sp.), Imbribryum
muehlenbeckii (Bruch & Schimp.) N. Pedersen, Campylium stellatum (Hedw.) Lange &
C.E.O.Jensen, Palustriella falcata (Brid.) Hedenäs, Sphagnum teres (Schimp.) Ångstr., and
Calliergon richardsonii (Mitt.) Kindb.
Fifteen square meters were occupied by Cinclidium stygium. Three main colonies were
observed in distinct small similar fens. Several hundred meters of unoccupied fens were also
present in the surroundings.
DISCUSION
Determination of material
The genus Cinclidium includes 4 species (Mogensen, 1973). The distinction between them
is generally straighforward taking into consideration sexual condition, leaf shape and capsule
characters. Then, difficulties may arise when only sterile material is at hand, which is the case
here. In particular, the distinction of Cinclidium stygium and C. articum (Bruch & Schimp.)
Schimp. may raise serious problems. The areolation of Cinclidium stygium is longer (lamina
cells more than two times as long as wide) than that of C. arcticum (less than two times as long
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Boletín de la Sociedad Española de Briología 46–47 (2016)
as wide). The leaf apiculum is long squarrose-pointed in Cinclidium stygium while being shortly
acuminate in C. arcticum, which is a northern species that has been reported from Germany in
recent times (Meinunger & Schröder, 2007).
Reproduction and Ecology
Cinclidium stygium is a synoicous species whose sporophytes are occasional. They are
frequent in Jura or Southern Alps (pers. obs.), where they were considered frequent in the past
(Hétier, 1896; Hillier, 1954). Absence of sporophytes in monoicous taxa may relate to the
absence of gametangia, inefficient fertilization or abortion of sporophytes at early stages of
development. In the case of Cinclidium stygium in the Pyrenees, it is clearly linked to the total
absence of gametangia. The harsh climatic conditions could be responsible for a depleted
fertility, which is common at the margin of plants distribution areas.
Cinclidium stygium is a fen indicator included in many types of “eutrophic” communities
(see review in Koponen, 1969), mostly Caricion lasiocarpae (Braun, 1968; Paul & Lutz, 1941).
There is a great deal of confusion about fen nomenclature, deriving from the phytosociological
approach to this vegetation type. Calcareous fens are widely considered eutrophic systems even
though detailed chemical characteristic of water or soil are mostly lacking. Though admittedly
rich in Ca++ solutes, or other minerals, they are mostly poor in biogenous elements (mostly P
and N compounds), and then clearly oligotrophic (Braun, 1968; Lamentowicz et al. 2013;
Kooijman et al., 2015). This is likely the case in the Pyrenees where no natural source of nutrient
enrichment is known.
Cinclidium stygium may extend into thinly wooded stands, which is the case in Alps or Jura,
where it is occasionally found in wooded carr. It is generally observed in habitats where water
trickles, as in the Pyrenees, or by springs or along rivulets (Mogensen, 1973; Sauer, 1990;
Blockeel et al., 2014). In Europe, the habitat requirements appear to be much narrower in the
southern regions than in the northern ones.
It is frequently associated with Calliergon giganteum (Schimp.) Kindb., Meesia triquetra
(L. ex Jolycl.) Ångstr., Scorpidium cossonii, S. scorpioides (Hedw.) Limpr., Hamatocaulis
vernicosus (Mitt.) Hedenäs, Drepanocladus trifarius (F.Weber & D.Mohr) Broth. ex Paris (Paul
& Lutz, 1941; Braun, 1970). By contrast, the community in the Pyrenees appears rather speciespoor. Calliergon richardsonii is perhaps a rarer associate which is mentioned from small spring
mounds at sites of calcium-rich ground water outflow (Antipin et al., 2003). Cinclidium stygium
is more frequent and achieves dominance in intermediate floating fens (along with Hamatocaulis
vernicosus, Meesia longiseta Hedw., Sphagnum teres) than in aquatic hollows
(Pseudocalliergon trifarium, Scorpidium scorpioides) (Braun, 1968). In the Pyrenees no
topographic heterogeneity was detectable.
Conservation
Fen bryophytes are very sensitive to overgrazing, which results in trampling and
eutrophication (Stammel et al., 2003; McBride et al., 2011). Grazing by cattle may well not be
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HUGONNOT: CINCLIDIUM STYGIUM SW. (MNIACEAE, BRYOPSIDA) IN EASTERN PYRENEES
appropriate in the case of relictual fens, and the dynamics of such stands are far from well
understood. They may be stable on the long run and may not need anthropogenic action.
Monitoring of the populations should be undertaken to unravel the vegetation trajectories.
Climate warming is certainly of concern because it could enhance development of tall
vegetation and overturn water balance on the long run.
Additionally, taking advantage of the wide vegetative regeneration of mosses, the capacity
of Cinclidium stygium for regrowth should be tested in adequate fen stands in the field. Target
stands could be habitats where competition has been lowered, deteriorated, but where water
feeding remains intact both from the point of views of quality and amounts. Clonal growth of
dispersed gametophores fragments is to be expected and could represent an innovating device of
conserving asexually reproducing relict bryophytes in isolated situation, far from their main
range.
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Recepción del manuscrito: 31-03-2016
Aceptación: 17-06-2016
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