The phytoplankton of S'Ena Arrubia Lagoon (Centre-Western Sardinia) between 1990 and 1995

Abstract

The phytoplankton study on the S'Ena Arrubia Lagoon started in 1990, after dystrophic events, leading to high fish mortality and consequently great economic losses. This study presents a general picture of the conditions of the lagoon between 1990 and 1995, and reports on the quali-quantitative changes in the phytoplanktonic populations, as well as the trends of temperature, salinity, pH, dissolved oxygen, algal nutrients and chlorophyll a. The lagoon was characterized by great changes in salinity between years and within the same year, by high nutrient contents and by a phytoplankton trend characterized by sudden intense blooms mostly due to the Chlorophyceae and the Bacillariophyceae. The number of species found, decreased from 1990 to 1994, followed by a slight increase in 1995. The same trend was also found for total density and chlorophyll a.     

The flora of the island Piana (Sardinia,Italy)

Abstract

The author reports the results of the herborizations carried out on the island Piana (northeastern Sardinia) located between Cape Ceraso and Cape Coda Cavallo. The flora consists of 250 entities distributed in 154 genera, inclusive of 54 families. The author gives information regarding the mail features of the vegetal coverage, and points out the presence of two species: Limonistrum monopetalum (L.) Boiss. and Omithoga-lum arabicum L., which are extremely rare in the little islands.     

The peopling of Sardinia (Italy): history and effects

Over the last ten years the population of the Mediterranean island of Sardinia has been object of numerous studies in the fields of anthropology and population genetics. Its insularity, central position in the Mediterranean area and rich historical past have made the island a veritable laboratory for the study and understanding of those interacting evolutionary mechanisms which determine a population's genetic structure. Indeed, from work performed at different levels on genetic structure analysis there emerges an extremely complex picture of the relationships between Sardinian and other Italian and Mediterranean populations, but also of relationships within the Sardinian population itself The diversification from Mediterranean and Italian populations can be explained by Sardinia's historical and demographic past. Internal heterogeneity can be attributed, in part, to strict isolation and the accompanying high levels of endogamy and inbreeding, and in part to the endemic presence of malaria which exerted a strong selective pressure on some characteristics; determining, for example, the differentiation between the plains and the mountain areas. Finally, an influence on Sardinia's biological history not to be neglected could be attributed to the demographic events, which triggered off phenomena of genetic drift and to cultural factors.     

The phytoplankton community of a eutrophic reservoir

The dynamics of the phytoplankton community of a eutrophic reservoir are described for a two year period. Fifty-eight species were recorded, 25 of them common. Bacillariophyta dominated during the winter and early spring and Chlorophyta during late spring, to be replaced by a bloom of Cyanophyta. The mean and peak biomass of phytoplankton was 8.6 mg 1^–1 and 40.8 mg 1^–1 in 1981, and 8.3 mg 1^–1 and 37.6 mg 1^–1 in 1982. Temperature accounted for 67.3% and pH for 8% of the variation in total phytoplankton biomass over the two year period, using a multiple regression technique.Both horizontal and vertical patchiness, measured as an index of mean crowding, were recorded in the reservoir. Horizontal aggregations were associated with spring blooms of Chlorophyta and summer blooms of Cyanophyta, while vertical aggregations were most marked during the summer bloom of Cyanophyta. Concentrations of phytoplankton were influenced by wind, the prevailing southwesterly wind accumulating algae in the northeasterly arm of the reservoir during much of the year.     

Flora of the Isle su Cardulinu (Southern Sardinia)

Abstract

The results of two years of collection in a small isle in the southern Sardinia are reported, consisting in a floristic list of 116 entities distributed in 96 genera and 41 families. The biological spectrum of this flora puts in evidence a typical Mediterranean environment, characterized by a marked summer dryness. The ratio: number of entities/surface of the studied site has been compared with that of other small southern Sardinian islands, resulting the highest value. This floristic aspect, as well as differences in the biological spectrum, is interpreted as the result of the presence in the area under study of a desultory link with the mainland, in form of a sandy isthmus. This seems important in breaking the biological balance of the small island.     

The role of periphytes in the shift between macrophyte and phytoplankton dominated systems in a shallow, eutrophic lake (Lake Taihu, China)

Based on experiments of periphyte response to different trophic levels and their impact on macrophyte production, it was found that the periphyte biomass increased with the nutrient concentrations. Increased trophic level and periphyte biomass resulted in decreased macrophyte photosynthesis. It was suggested that the periphytes could cause resilience and hysteresis in the system shifts between macrophyte and phytoplankton domination. Other factors, such as fish farming, storm induced waves and mechanical destruction, and high water levels could be the perturbations during the system shifts, but these are not the key factors. Instead, the nutrient loading and periphyte abundance could determine the shift in lake ecosystem between macrophyte and phytoplankton domination. This finding could theoretically elucidate the mechanism of ecosystem shifts between macrophyte and phytoplankton domination.     

Comparision of historical and recent data on hydrochemistry and phytoplankton in the Rijnland area (The Netherlands)

In two canals and two lakes in the western part of the Netherlands a comparision is made between data on water chemistry and phytoplankton from 1941/1942 with recent data. Orthophosphate in particular, but also inorganic nitrogen, has increased tremendously, especially in the Gouwe canal, where Rhinewater enters the area. The inorganic N/P mass ratio decreased in the last 45 years, indicating that the limiting nutrient has changed from phosphate in 1941 to nitrogen in 1987.The average seston volume, measured by filtering 1001 water through a plankton net (50 µm), has doubled. In the early 1940s the blue-green alga Microcystis aeruginosa regularly formed waterblooms, as it does now. The plankton composition seems to have become impoverished in the last decennia, since several taxa have disappeared. Others are strongly reduced in number. The saprobic index has not changed.Based on the relations between chlorophyll-a and biological oxygen demand (BOD) and between transparency and seston volume, BOD, dry weight and ash free dry weight in 1987 chlorophyll-a and transparency in 1941 are estimated. The average chlorophyll-a concentration in the lakes has doubled or tripled in the last 45 years and the mean transparency in the Gouwe canal declined from 75 to 50 cm. Submerged higher plants at some sites have disappeared in the last decennia. The results can be used to develop ecological objectives for combatting eutrophication in canals and lakes and possibly in the river Rhine.     

Some herborizations on the islet of Pan di Zucchero (Sardinia W-SW)

Abstract

The author reports the results of some floristic research carried out on the islet of Pan di Zucchero (W-SW Sardinia). The presence of endemism and of a low and creeping Artemisia arborescens coverage have been pointed out, as well as a natural unviolated state unique among the Sardinian microinsular habitats, due to the inacessibility of the area.     

On the annual variation of phytoplankton biomass in Finnish inland waters

Annual variations in phytoplankton biomass in 63 lakes in Southern and Central Finland are discussed. Biomass is rather small during winter (January–April), usually <0.05 mg l^–1 (fresh weight) and there are no differences between oligotrophic and eutrophic lakes. In early spring and in autumn biomass varies widely, depending mainly on water temperature. Phytoplankton biomass is smaller in July than in June and August in oligotrophic lakes (biomass <0.20 mg l^–1 fresh weight) and mesotrophic (biomass 1.0–2.5 mg l^–1) lakes, but greater in eutrophic (biomass 2.5–10.0 mg l^–1) and hypereutrophic (biomass >10.0 mg l^–1) lakes. The standard deviation of phytoplankton biomass in Finnish inland waters is usually smallest in July, which facilitates the comparison of phytoplankton between different kinds of lakes.     

A comparison of phytoplankton biomass parameters and their interrelation with nutrients in Saronicos Gulf (Greece)

The relationship between total phytoplankton cell number, chlorophyll a, cell volume, and the response of these parameters to reactive phosphorus and nitrate in surface waters of Saronicos Gulf (Greece) was examined using simple and partial correlation statistics. Different conclusions could be drawn as to the comparability between biomass parameters and their interrelation with nutrients. Partial correlation analysis is considered to be a better method for comparing ecological data. The analysis of phytoplankton abundance should include determinations of as many biomass characteristics as possible since each has its own specificity.     

An updated inventory of the non-native flora of Sardinia (Italy)

We provide an updated inventory of the non-native flora of the Italian island of Sardinia, including accepted names, family, synonyms, biological form, fruit type, introduction pathway and native origin. This inventory was performed by reviewing the available literature and conducting dedicated field surveys across the entire island. The inventory catalogues 931 non-native taxa, including 31 cryptogenic species, 901 species, 14 subspecies, 13 varieties, two forms and one cultivar. We utilised the position on the introduction–invasion continuum concept and meta-population criterion to further label each species. Based on these frameworks, the non-native flora of Sardinia can be divided into 274 casual, 169 naturalised, 19 invasive, 440 exclusively planted and 29 unobserved after 1950. There are 204 archaeophytes and 727 neophytes. The majority of the non-native species (791) were introduced to the island voluntarily, and 140 species were introduced accidentally. The present inventory identifies 72 additional non-native taxa not previously reported in the literature.     

Microcystin production by cyanobacteria in the Mwanza Gulf (Lake Victoria,Tanzania)

In order to investigate the potential for microcystin (MC) production by cyanobacteria in the Mwanza Gulf (Lake Victoria, Tanzania), nutrients, phytoplankton and microcystins were sampled inshore (3 m depth) and offshore (18 m depth) from May to August 2002. Significant differences in soluble reactive phosphorus (SRP) and nitrate concentrations between offshore and inshore indicated eutrophication via terrestrial run-off. Though the concentrations of SRP and nitrate ranged between 36–127 and 35–726 μg l ⁻¹ each, the phytoplankton biovolume was generally low. The phytoplankton community was dominated by diatoms (Nitzschia acicularis), a number of cyanobacterial species (Aphanocapsa sp., Anabaena sp., Planktolyngbya spp., Microcystis sp.) and cryptomonads. The water column was completely mixed and Nitzschiapeaked in abundance during July. All cyanobacteria were low in abundance during the entire study period (0.1–1.6 mm ³ l ⁻¹). Microcystins were analysed using high performance liquid chromatography coupled with diode array detection High Performance Liquid Chromatography with Diode Array Detection (HPLC-DAD) and in most samples no microcystins were detected. The highest concentration of [Asp ³]-MC-RR was found in open water at the surface on July 2nd, 2002 (1 μg l ⁻¹). MC concentrations did not pose a potential health risk in the Mwanza Gulf during the study period, however, it is possible that the period of higher cyanobacterial biovolumes has been missed during the sampling period of this study.     

Group-specific phytoplankton biomass/dissolved carbohydrate relationships in the Gulf of Trieste (Northern Adriatic)

Distribution of carbohydrates (CHO) and photosynthetic pigments werestudied in the Gulf of Trieste, northern Adriatic Sea, during the period ofsummer stratification with a special emphasis on determining the impact ofthe taxonomic composition and concentration of phytoplankton biomass on thecarbohydrate levels in the water column. Dissolved total carbohydrates(DTCHO), dissolved monosaccharides (DMCHO) as well as particulatecarbohydrates (PTCHO) were determined using the colorimetric MBTH-method,while pigment biomarkers of the phytoplankton biomass were determined byreversed-phase HPLC. Concentrations of the total CHO (dissolved+particulate) varied in a wide range from 173 μg Cl^™1 to 1552 μg C l^™1. The percentage ofPTCHO in the total CHO concentration was relatively low(4–25%), indicating that the main pool of CHO was in thedissolved phase. The contribution of DTCHO to the total dissolved organiccarbon (DOC) in late summeontribution r was highly variable(10–65%) with an average value of 20 ± 14%, whilein early summer this percentage was somewhat lower and less variable (range11–23%; average 17± 3%). Analyses of biomarkerpigments revealed a very high diversity and a rather heterogenous verticaland spatial distribution of the phytoplankton biomass during the period ofsummer stratification. In September 1994, the predominant taxonomic groupsof phytoplankton were prymnesiophytes, diatoms, silicoflagellates,cyanobacteria and, especially in the bottom layer, dinoflagellates. Arelatively good correlation (r² =0.51) found betweenDTCHO and chl a suggested that DTCHO were mainly of phytoplankton origin.Furthermore, a concomitant increase of DTCHO with peridinin and fucoxanthinindicated that dinoflagellates and diatoms had a decisive impact on CHOlevels in the water column. By contrast, early summer phytoplankton (June),which was dominated by prymnesiophytes, exhibited a comparatively lowerimpact on the CHO distribution. This revised version was published online in July 2006 with corrections to the Cover Date.     

Long term study on the influence of eutrophication, restoration and biomanipulation on the structure and development of phytoplankton communities in Feldberger Haussee (Baltic Lake District, Germany)

Feldberger Haussee provides a classic example of eutrophication history of hardwater lakes in the Baltic Lake District (Germany) and of changes in their algal flora during the 20th century. The lake originally was regarded as slightly eutrophic. A process of drastic eutrophication from the 1950s until the end of the 1970s caused mass developments of blue-green and green algae. A restoration program was started in the 1980s to improve the water quality of the lake using both diversion of sewage outside the catchment area, and biomanipulation by altering the fish community. This restoration program led to positive changes in the lake ecosystem. Direct effects of biomanipulation resulted in an increase of herbivorous zooplankton, a decrease of phytoplankton biomass, and an increase of water transparency. The recovery of Feldberger Haussee also may have been indirectly enhanced by an increase in nutrient sedimentation as a consequence of intensified calcite precipitation, decrease in phosphorus remobilization due to a pH-decrease, increased NIP-ratio, and recolonization of the littoral zone by macrophytes. This paper concentrates on the long term development of the phytoplankton community as a response to changes in the food web structure as well as to alterations in the chemical environment of the algae. Both are reflected in four major stages passed by the algal assemblage between 1980 and 1994: (1) From 1980-summer 1985 dense green algal populations were found indicating similar conditions as in the 1970s during the period of maximum eutrophication. (2) A diverse phytoplankton community during summer 1985–1989 showed the first effects of a recovery. (3) From 1990–1992 the phytoplankton was characterized by ungrazeable filamentous blue-green algae first of all as a response to increased herbivory of zooplankton on edible species and to increasing N/P-ratios. (4) Finally, the algal species diversity increased in 1993 and 1994 whereas the phytoplankton biomass decreased showing the success of the combined restoration measures.     

Analysis of 31 STR loci in the genetic isolate of Carloforte (Sardinia, Italy)

The genotypes of 31 autosomal short tandem repeat loci in the population of Carloforte were analyzed, these representing a linguistic and genetic isolate located on the island of Sardinia (Italy). The markers span the entire length of chromosomes 19, 20, 21 and 22. Allele frequencies and statistical parameters were presented for all loci. Observed heterozygosity ranged from 0.279 to 0.884, and polymorphism information content from 0.552 to 0.886. All but two loci showed Hardy-Weinberg equilibrium after Bonferroni correction. The 31 short tandem repeat loci examined in the present work provide additional data on the genetic structure of the Carloforte population.     

Miocene carbonate factories in the syn-rift Sardinia Graben Subbasins (Italy)

Summary Miocene syn-rift carbonate production areas are exposed in south-eastern Sardinia (Italy) along the eastern side of the Plio-Pleistocene Campidano Graben. Here the downfaulted margins of the Oligo-Miocene Sardinia rift-basin crop out with a complex alignment of smaller subbasins. Carbonate factories developed during the Aquitanian times in these tectonically controlled small depositional subbasins, where terrigenous input might be high due to the erosion of the uplifted pre-Neogene substrata. Terrigenous deposits generally acted as passive substratum for pioneer communities of rhodalgal-type (red algae, ostreids, bryozoans) and locally evolved into coral-dominated assemblages. Carbonate production areas occur on tilted, uplifted blocks as well as along basement margins. These have varying organic communities and facies characteristics strongly dependent on different environmental conditions. In footwall areas, devoid of (or with a very reduced) terrigenous supply, open foramol carbonate factories occur with aggradational-progradational stratigraphic geometries. The resulting pure calcareous successions are organized in sequences, bounded by tectonically driven discontinuity surfaces. In sectors close to the hinterland area, with a higher freshwater input and a consequent significant clastic input, coral-dominated assemblages grew during long periods of quiescence between flash floods. Repeated coral-rich communities developed on thick wedges of terrigenous debris. Carbonate facies composition and distribution were mainly controlled by local syn-sedimentary tectonics and eustasy as well as by climate. However, although the inception of the carbonate factories was presumably not synchronous, their growth represented the response to a relative regional sea level rise subsequent to episodes of significant clastic supply: the expression of an early syn-rift stage. During the Burdigalian (N6 zone) a hemipelagic cover uniformly sealed the neritic successions. This basin wide drowning event appears to correspond to the transgressive system tract of the TB2.1 cycle ofHaq et al. (1987) but it can also be interpreted as the expression of an evolved syn-rift stage passing to late syn-rift and quiescence stages. Beneath the hemipelagic cover in some areas, ?late Aquitanian-early Burdigalian deep erosive surfaces, terrigenous clastics and paleosoils have been recognized. These suggest a relative sea level fall and may relate to the global sea level drop at the TB1-TB2 boundary (seeHaq et al., 1987) or to diacronous uplift of different fault blocks.     

Ecological interactions between Nile tilapia (Oreochromis niloticus, L.) and the phytoplanktonic community of the Furnas Reservoir (Brazil)

1. Exotic invasive species modify natural food webs in a way frequently hard to predict. In several aquatic environments in Brazil the introduction of Oreochromis niloticus (tilapia) was followed by changes in water quality. Yet, because of its rapid and easy growth, this fish has been used in many aquaculture programmes around the country. 2. To measure the effects of tilapia on the phytoplankton community and on water conditions of a large tropical reservoir in south‐eastern Brazil (Furnas Reservoir), we performed two in situ experiments using three controls (no fish) and three tilapia enclosures (high fish density). Abiotic and biotic parameters were measured at 4 day intervals for 28 days. 3. Fish presence increased nitrogen (N) and phosphorus (P) availability (ammonium 260 and 70% mean increase – first and second experiment; and total phosphorus 540 and 270% mean increase) via excretion. Nutrient recycling by fish can thus be significant in the nutrient dynamics of the reservoir. The higher chlorophyll a concentration in the experimental fish tanks (86 and 34 μg L^?1, first and second experiment, respectively) was the result of a positive bottom‐up effect on the phytoplankton community (approximately 2 μg L^?1 in the reservoir and control tank). 4. Because tilapia feed selectively on large algae (mainly cyanobacteria and diatoms), several small‐sized or mucilaginous colonial chlorophyceans proliferated at the end of the experiments. Thus, the trophic cascade revealed strong influences on algal composition as well as on biomass. 5. Tilapia can contribute to the eutrophication of a waterbody by both top‐down and bottom‐up forces. In particular, by supplying considerable amount of nutrients it promotes the increase of fast growing algae. Tilapia must be used cautiously in aquaculture to avoid unexpected environmental degradation.     

Changes in phytoplankton biomass and primary production between 1991 and 2001 in the Westerschelde estuary (Belgium/The Netherlands)

The Westerschelde estuary is a very polluted and turbid estuary, but the last decade the waterquality improved. Dredging activity also increased in 1997 to allow bigger ships to enter the port of Antwerpen. This could potentially decrease the light conditions for the phytoplankton. Because of all these recent changes in the estuary we studied primary productivity in 2001 and compared it to values in 1991. The results show that due to a decrease in discharge in particulate and dissolved organic carbon the oxygen concentrations in general have increased in the upstream region, although in spring and summer low oxygen concentrations (10–30% saturation) can still be found. Phosphate and ammonia concentrations have decreased and the zone of nitrification which was very large in 1991 has become very small and is now located in the uppermost upstream region of the estuary. Si-concentrations have remained the same. All nutrient concentrations are still high enough not to limit phytoplankton growth. Turbidity remained unaltered as a result of the dredging works, and as a result phytoplankton biomass in most of the estuary did not show a decrease, although there were signs that in the upstream region phytoplankton biomass decreased, possible caused by increased grazing pressure. The relationship between phytoplankton biomass and primary productivity did not change, and from the data it can be concluded that the dredging activity will not influence the gross and net primary productivity of the phytoplankton.     

Effects of aquatic macrophytes on water quality and phytoplankton communities in shallow lakes

We investigated aquatic macrophytes, water quality, and phytoplankton biomass and species composition in three shallow lakes with different levels of vegetation cover and nutrient concentration in Kushiro Moor, during August 2000. Trapa japonica can live in a wide range of nutrient levels. This species forms an environment with a steeper extinction of light, higher concentrations of dissolved organic carbon (DOC), lower concentrations of dissolved oxygen (DO) near the bottom, and lower concentrations of nitrate+nitrite and soluble reactive phosphorus (SRP) than other vegetation types. The pH was much higher in a Polygonum amphibium community, and the DO near the bottom did not decrease compared to a T.japonica community in the summer. The relationship between chlorophyll a and the limiting nutrient (total phosphorus (TP) when total nitrogen (TN):TPis 10 and TN/10 when TN:TP is <10) significantly differed between lakes with and without submerged vegetation. The chlorophyll a concentrations at a given nutrient level were significantly lower in water with submerged macrophytes than in water without them. Correspondence analysis showed that the difference in phytoplankton community structure across sites was largely due to the presence or absence of submerged macrophytes, and the ordination of phytoplankton species in the lakes with submerged macrophytes is best explained by environmental gradients of TN, chlorophyll, pH and SRP.