ACTA BIOLOGICA SLOVENICA LJUBLJANA 2008 Vol. 51, [t. 1: 13–20 Sprejeto (accepted): 27.10.2008 Competitive advantages of Najas marina L. in a process of littoral colonization in the lake Velenjsko jezero (Slovenija) Tekmovalne prednosti vrste Najas marina L. pri kolonizaciji litorala Velenjskega jezera (Slovenia) Zdenka MAZEJ1*, Mateja GERM2 1 ERICo d.o.o., Environmental Research and Industrial Co-operation, Koroška 58, 3320 Velenje, Slovenia; E-mail address: zdenka.mazej@erico.si (*corresponding author) 2 Biotechnical Faculty, Department of Biology, Večna pot 111, 1000 Ljubljana, Slovenia Abstract. Najas marina is the dominant macrophyte species in Velenjsko jezero. It appeared in the lake in 1997 and soon prevailed over the species Myriophyllum spicatum L. and Pota- mogeton crispus L., which used to be the two most abundant species in the lake in the past. The physico-chemical and geomorphological characteristics of the lake are discussed in relation to the attributes of Najas marina, presenting competitive advantages in this environment. Conditions in the lake such as warm water and unstable sediment enabled successful growth and life strategy of Najas marina, which is a summer-annual plant with short life cycle, quick propagation from seeds and a very extensive root system. Key words: artificial lake, physico-chemical and geomorphological characteristics of the lake, plant invasion, aquatic macrophytes, Najas marina L. Izvleček. Najas marina je prevladujoča makrofitska vrsta v Velenjskem jezeru. V jezeru se je pojavila leta 1997 in kmalu prevladala nad vrstama Myriophyllum spicatum L. in Potamogeton crispus L., ki sta do takrat prevladovali v jezeru. V članku so izpostavljene fizikalno kemijske in geomorfološke značilnosti jezera, ki so ene izmed pomembnih dejavnikov, ki vplivajo na kompeticijske lastnosti določene vrste. Razmere v jezeru, kot so topla voda in nestabilen sediment, omogočajo uspešen razvoj in rast vrste Najas marina, ki je toploljubna enoletnica s kratkim življenjskim ciklom, hitrim načinom razmnoževanja iz semen in z zelo ekstenzivnim koreninskim sistemom. Ključne besede: umetno jezero, fizikalno kemijske in geomorfološke značilnosti jezera, invazivnost rastlin, vodni makrofiti, Najas marina L. Introduction The ability of a plant species to invade a region depends not only on the attributes of the plant, but also on the physico-chemical characteristics of the lake habitat invaded (Ali & SoltAn 2006). Besides penetration of radiation and temperature, the key factor determining the composition and vertical distribution of submersed macrophyte communities is substrate composition (average grain size, sorting level, silt fraction, organic matter). Sediments influence vegetation in two ways, i.e. by serving as an anchor for roots and rhizoids (HAndley & dAvy 2002) and as potential nutrient reservoir 14 Acta Biologica Slovenica, 51 (1), 2008 (PerAltA & al. 2003). ScultHorPe (1967) pointed out that the principal influence of the substrate on the distribution of rooted aquatic plants is due to its physical texture rather than chemical composition. The sediment texture is a very important characteristic, which has very great influence on the physical, chemical and, indirectly, on the biological properties of the sediment. The mechanical properties and instability of the substrate in aquatic habitats might prevent seedling establishment and increase the chances of dislodgement (tituS & Hoover 1991) in many species. In contrast seedlings of Najas marina L. can not colonize on firm sediments (HAndley & dAvy 2002). Authors who have investigated the interaction between vegetation and sediment (lindner 1978, Selig & al. 2007) clearly distinguished between plant communities’ characteristic for mineral sediments with low nutrient content and plant communities’ characteristic for muddy sediments with high nutrient content. Najas marina is a rare species in Slovenia, registered in only six locations (Vreš & Kaligarič 1999, germ & al. 2008) beside Velenjsko jezero, where Najas marina is the dominant species. It appeared in the lake in 1997 (mAzej 1998) and outcompeted both Myriophyllum spicatum L. and Potamogeton crispus L., which used to be abundant in previous years. However, they had never occurred in the lake to such an extent as Najas marina. Myriophyllum spicatum and Potamogeton crispus are known as very competitive species, which establish large monospecific weed beds in many lakes (nicHolS & SHow 1986; BolduAn & al. 1994), including some Slovenian meso-eutrophic lakes (mAzej 1998; Mazej & gaberščiK 1999). We hypothesize that physico-chemical and geomorphological characteristics of the lake are the main factors, which allow the broad expansion of Najas marina. Species composition was related to environmental characteristics in order to point out the reasons for the successful growth of Najas marina, which prevailed over other macrophytes. Some of the attributes of Najas marina were also stressed. Materials and methods Study Area Velenjsko jezero is situated in the Šalek valley, in the Sub-alpine part of Slovenia near the Aus- trian border at an altitude of 366 m, with a surface area of 135000 m2 and a maximum depth of 54 m. Huge lignite-coal reserves, which are dug in Velenje Colliery are the crucial factor of human caused changes and pollution of the Šalek valley. The most remarkable consequences of coal mining are three subsidence lakes, Škalsko, Velenjsko and Družmirsko jezero. Velenjsko jezero came into existence after the World War II. At the beginning of its existence it was used as a reservoir for ash transport water from the Šoštanj thermal plant. The pH of transport water is around 12. The pH of lake was the same so any sorts of organism could not survive in such an alkaline environment. Up to early eighties ash slurry had run into lake, but afterwards the building of the ash landfill was begun. Ash reminded on the landfill and only transport water ran to lake. The pH remained 12 because the only reason for high alkinity was transport water. The closed loop system for the ash was built in 1994 and this has an impact on the lake quality. In only three years the lake pH has almost been normalized and biota appeared in the lake again (ŠterBenk, 1999). It was recolonized by phyto- and zooplankton, fish, macrophytes and other organisms. The pH-value of the lake is now around 8. Sampling Three sampling locations (L1, L2, L3) with highest species richness and similar morphometric characteristics of littoral on the south-eastern part of the lake, were chosen. Samples of water and sedi- ment were taken adjacent to vegetation from three sampling locations monthly from June to September 2004. Samples of water were taken at 0.5 m depth in plastic bottles, while sediment was sampled by a 15Z. Mazej, M. Germ: Competitive advantages of Najas marina L. in a process of littoral colonization … handled plastic scoop. Water transparency was measured in the middle of the lake with a Secchi disk. Temperature at 30 cm and pH at all three locations were measured with a MultiLine P4. Presence and abundance of macrophytes At the same time the distribution of macrophyte species at the three sampling locations was assessed using a boat, a depth meter, a viewing box and a sampling rake. Species abundance was evaluated according to koHler (1978) on a five level descriptor scale (1 – very rare, 2 – infrequent, 3 – common, 4 – frequent, 5 – abundant, predominant). Water and sediment analysis The samples of water and sediment were brought to the laboratory and stored at 4 oC. The contents of total nitrogen (TN), total phosphorus (TP) and soluble reactive phosphate (SRP) in sediment were analysed by the standard methods: ISO 11261:1995, ISO 11263:1995 and ÖNORM L 1088:2005, while TN and TP in the water were determined according to the standard methods ISO 10304-2:1995 and ISO 6878:2004. Soil texture, sorting level and the content of organic matter were also determined in the sedi- ment. Soil texture was determined by mechanical analysis – the sedimentation stactometer method with American classification according to Hodnik (1988). The percentages of four fractions were determined: sand (grain size > 0.2 mm), coarse silt (grain size 0.05