Genetic evidence for the identity of Caulerpa racemosa (Forsskål) J. Agardh (Caulerpales,Chlorophyta) in the Adriatic Sea

Three taxa of Caulerpa racemosa that differ morphologically and genetically have been reported in the Mediterranean Sea. The ‘invasive variety’ was recorded for the first time in the early 1990s in Libya. In less than 10 years, it was found in almost all parts of the Mediterranean. The first record of C. racemosa in the Croatian part of the Adriatic Sea was in 2000 and as many as 35 different localities were established by the end of 2004. In terms of morphology, the specimens from the Adriatic Sea resemble the ‘invasive variety’. To confirm this, we analysed populations from two different localities (the island of Mljet and the peninsula of Pelje?ac) using the ITS1-5.8S-ITS2 region of 18S-5.8S-26S rDNA unit as a molecular marker. The ITS1-5.8S-ITS2 region from nine individual plants was amplified by PCR, cloned in a pCR 2.1 vector and sequenced. Phylogenetic comparison of sequences from specimens found in the Adriatic Sea with specimens of the same and similar taxa, found both inside and outside the Mediterranean, provided genetic evidence that C. racemosa populating the Adriatic Sea corresponds to the Mediterranean C. racemosa var. cylindracea (Sonder) Verlaque, Huisman?&?Boudouresque, i.e. to the ‘invasive variety’.     

Diatom distribution in the Southern Adriatic Coastal waters

Abstract

Data on the horizontal and vertical distribution of diatom species, collected between April 1995 and March 1996 in coastal waters of the Apulian Adriatic Sea are presented. A total number of 120 species belonging to 51 genera were identified. Diatoms were dominant in the major part of the examined samples, constituting up to 90% of the total cell numbers during the spring period.     

Plant species diversity of Adriatic islands: An introductory survey

Abstract

The European Mediterranean region is one of the world's major centres of biodiversity. Research on plant species diversity in this region has neglected the area along the eastern part of the Adriatic basin in comparison to the other Mediterranean areas. The main aim of this study was to focus on this neglected area, by supplying data which is at present lacking in order to discuss the species-area relationship (SAR), floristic richness and endemism of the Adriatic islands and coast. Floristic data for 106 Croatian islands collected by different authors were integrated, systematised and presented in a form usable by other researchers worldwide. The Power (Arrhenius) function was used for modelling (by non-linear regression) the SAR. Residuals around the regression curve (as indicators of floristic diversity without the influence of island area) were calculated for each island. The proportion of endemics in the total island flora varies from 0% up to 28.6%, and 17.5% for narrow endemics. Floristic richness of the broader region was estimated (on the basis of SAR extrapolation) on 1807 species for all Croatian islands, and on 2797 species for the entire Mediterranean area in Croatia.     

Vanneaugobius dollfusi Brownell, 1978 a rare fish new to the Adriatic Sea

Two specimens of Vanneaugobius dollfusi found among ichthyological material of the Institute of Oceanography and Fisheries, Split and two specimens donated to the Natural History Museum Rijeka provide the first positive records of this species in the Adriatic Sea, and the second record ever for this species.     

Hyperbenthic gobies in the Kvarner area, Adriatic Sea

By the aid of SCUBA diving in the Kvarner area (northern Adriatic) from 1993 to 2002 five gobiid species were found to be hyperbenthic. These findings provided specific data on their ecology.     

The Mechanism Controlling Plant Nutrient Concentrations in the Northern Adriatic Sea

A 20 year data set for the northern Adriatic was analyzed and the factors establishing the nutrient environment identified. Concentrations ranged widely (TIN 0.0–78, PO₂ 0.01–1.1, and SiO₄ 0.0–59 mmol m⁻³). In early winter remineralization increased concentrations. Characteristic winter, late spring and fall phytoplankton blooms alternately decreased and increased concentrations, as modified by river input. In summer nutrients were minimal under a semi-closed circulation pattern and high vertical stability, due to closely coupled nitrogen and phosphorus assimilation-regeneration processes and biogenic silica sedimentation. “New” primary production supported mainly by river input of “new” nutrients approximated “regenerated” primary production supported by regenerated nutrients, making the ecosystem especially sensitive to eutrophication pressure from anthropogenic increases in the Po River nutrient load.     

The halophilous vegetation of the Po Delta (northern Italy)

The halophilous vegetation in the Po Delta region (north Adriatic) has been studied with the Braun-Blanquet method. Vegetation types have been defined by numerical classification of vegetation data. Their ecology has been studied by indirect gradient analysis. The following three main groups of phytocoena have been recognized. (1) Perennial halophytic vegetation (class Puccinellio-Salicornietea) including 7 associations: Spartinetum maritimae, Puccinellietum palustris, Salicornietum radicantis, Salicornietum fruticosae, Agropyro-Inuletum crithmoidis, Halimionetum portulacoidis, are quoted according to an approximate gradient of decreasing soil moisture. The Juncetum maritimi is conditioned by soil erosion. (2) Therophytic vegetation settled on soils subject to natural or artificial disturbance (class Thero-Salicornietea), including 3 associations: Suaedo-Kochietum hirsutae, Salicornietum herbaceae s.1. and the Aster tripolium-Suaeda maritima community. (3) Halotolerant vegetation (class Artemisietea vulgaris), including only the Atripliceto-Elytrigietum pungentis settled on soils with a low salt content.Nomenclature of species follows Pignatti (1982).The research was supported by a grant of the Istituto per i Beni Artistici, Culturali e Naturali, Regione Emilia-Romagna (Italy) and by a grant of the Italian C.N.R. (Research Group for Naturalistic Biology).     

Plankton and hydrography in a moderately eastern Adratic bay (Gruž Bay)

Gruž Bay (south-eastern Adriatic) is moderately eutrophicated, mostly by discharge from the karst river Ombla. Input of inorganic nitrogen might be attributed to enrichment from the open sea during strong and continuous north winds in winter 1988/89. Annual succession of primary producers, herbivores and decomposers was defined by seven stages and induced by specific physical-chemical characteristics. In the period April–August, biological production was mostly due to small size fractions of phytoplankton and zooplankton. Recycling of planktonic biomass occurred in September, of allochtonous organic matter in February and March.     

Sedimentary anaerobic microbial biogeochemistry in the Gulf of Trieste, northern Adriatic Sea: Influences of bottom water oxygen depletion

Sediment samples from two locationsin the Gulf of Trieste (northern Adriatic Sea) werecollected during periods of maximum and minimumtemperatures for two years. Both sites were rich incarbonate material and inhabited by a diverse benthicinfaunal community. However, Site F exhibited adeeper dwelling faunal community, higher content ofcarbonate minerals, and larger grained sediments thanat site MA, which was closer to shore. Depth profilesof sulfate reduction and potential rates of iron andmanganese reduction were determined together withmeasurements of pore water and solid phase chemistry. Bottom waters at all sites were nearly saturated withoxygen for all of the dates sampled except forSeptember 1993 when bottom waters at site F were lessthan 50% saturated. Sulfate reduction rates were ashigh as 400 nmol ml^-1 day^-1 during latesummer and fall when temperatures were >20 °C,while rates during March (8 °C) were <30 nmolml^-1 day^-1. Potential rates of ironreduction, as determined by the accumulation of bothdissolved and acid-soluble reduced iron, were high insurficial sediments at each site except at site F whenbottom waters were partially depleted in oxygen. In the latter instance, sulfate reduction overwhelmedmetal reduction. Although the portion of metalreduction due directly to enzymatic use by bacteriawas not determined, the potential rate data suggestedthat Fe and perhaps Mn reduction were significantcomponents of anaerobic carbon degradation in thesesediments during much of the year. Both sitesappeared to support active metal-reducing bacterialcommunities. However, occasional depletion of oxygenin bottom waters appeared to cause a decrease inirrigation/reworking activity by infauna whichdepressed redox cycling of elements enhancing theimportance of sulfate reduction. A shift from metalreduction to sulfate reduction potentially exacerbatestoxic effects of oxygen depletion on fauna byincreasing the accumulation of toxic sulfide.     

Possible cryptic speciationwithin the sea anemone Actinia equina complex detected byAFLP markers

The population genetic profiles of 60 specimens of thecommon intertidal sea anemone Actinia equina taken from foursampling sites (Peroj, Barbariga and the north and south shoresof the Limski Canal), along a 25 km strip of the coastof the Istra Peninsula, Croatia, were evaluated by AFLP markers(144 loci). All populations were characterized by aggregates ofspecimens confined within a few square meters. One of the populations(on the north shore of the canal) contained both large and small-sizedindividuals. Results revealed high within-aggregate genetic heterogeneity(36.1–55.6%). With respect to interpopulationprofiles, geographically remote populations from Peroj, Barbarigaand the south shore of the canal were more closely related geneticallythan those on the north and south shores of the canal. The small-sizedsubpopulation from the north shore exhibits a distinct AFLP pattern,suggesting that it warrants recognition as a cryptic species.  © 2002The Linnean Society of London, Zoological Journal of the LinneanSociety , 2002, 136 , 315−320