Biostratigraphy of Lower Cretaceous microfossils from the Araripe basin, northeastern Brazil

A biostratigraphic study was carried out in the Lower Cretaceous Araripe basin, northeastern Brazil, allowing the recognition of several chronostratigraphic units: the Dom João (Jurassic?-Lower Cretaceous?), the Rio da Serra (Neocomian) and the Alagoas (Aptian/Albian) local stages. For the first time a large hiatus between the Rio da Serra and Alagoas local stages is carefully documented. The palynomorphs and the ostracode associations throughout the Jurassic?-Aptian/Albian sequence allow the interpretation of the paleoenvironmental evolution of the Araripe basin which otherwise confirms that a polycyclical sedimentation occurred in the basin, being one of the controlling factors on the distribution of ostracodes and palynomorphes.     

Information value of chironomid remains in the uppermost sediment layers of a complex lake basin

The subfossil remains of chironomids were analyzed from four short (35–50 cm) sediment cores in eutrophicated Lake Vanajavesi, southern Finland. The chironomid analysis was found to be a useful palaeolimnological technique for indicating the following aspects: (1) The pollution history of the lake during the last 150 years. A succession from an oligotrophic Micropsectra-Monodiamesa community, through eutrophic Chironomus communities, to the disappearance of the chironomid fauna, was detected. (2) The bottom dynamic conditions at the sampling site. (3) The water level changes of the lake. (4) The significance of bioturbation in the core chronology and stratigraphy. The disappearance of the chironomid remains in the cores was correlated with the occurrence of annually laminated sediment.The most important factor disturbing the interpretation of the cores was the redeposition of head capsules by erosion and transportation. Detailed identification of the remains is necessary to avoid the misinterpretations caused by redeposition. Bioturbation reduces the time resolution of the cores. It is necessary to use dating methods which take the effect of bioturbation into account.     

Age, growth and feeding of the common stingray (Dasyatis pastinaca, L., 1758) in the Cilician coastal basin, northeastern Mediterranean Sea

Growth and feeding of stingray ( Dasyatis pastinaca ) were studied using 346 specimens from the Cilician Basin coastal area (northeastern Mediterranean). Age classes between 0 to XII were found. The total length of all specimens ranged from 14.6 to 100.9 cm, and total weight was between 22.5 and 6800 g. Total length (TL)-weight (W) and disc width (DW)-weight (W) relationships were W = 0.0033*L^3.1429 and W = 0.0039*DW^3.4914, respectively. The age data, derived from central readings, were used to estimate the von Bertalanffy length and weight growth parameters. The results were L_∞ = 294.9 cm, W_∞ = 198690.1 g, K = 0.029 year⁻¹; t₀ = −2.2 year. The D. pastinaca diet was composed mainly of crustaceans.     

On the insect fauna of the Kichiga River basin, northeastern Kamchatka

189 species of insects from 55 families and 9 orders were found in the Kichiga River basin, northeastern Kamchatka Peninsula in 1987–1994: 7 species of Plecoptera, 7 of Odonata, 1 of Orthoptera, 4 of Homoptera, 6 of Heteroptera, 54 of Coleoptera, 73 of Lepidoptera, 15 of Hymenoptera, and 22 species of Diptera. Most of the insect species present in the Kichiga basin have wide ranges: 55 species and subspecies are Holarctic, 52 species have a broad Palaearctic distribution, 10 are Eastern Palaearctic, 8 are Amphi-Pacific, 8 are circumboreal or circumpolar, 4 are Far Eastern or Pacific; 5 species are endemic or subendemic to Kamchatka or some part of the peninsula.     

Phenology of woody species in tropical coastal vegetation, northeastern Brazil

The study was carried out in the Private Nature Reservation Nossa Senhora do Outeiro de Maracaípe, located along the southern coast of Pernambuco state, in the Nossa Senhora do Ó District (08°31′48″S and 35°01′05″W), Ipojuca municipality, northeastern Brazil. The reserve has 76.20 ha of tropical coastal vegetation (Restinga forest). The aims were to determine the existence of seasonal phenological pattern of woody species as a function of rainfall. During the study period, the rainfall was 26.8 mm in the driest month (November 2003) and 538.9 in the wettest (June 2004). Observations on flowering, fruiting, leaf fall, and leaf flushing were recorded monthly, during 16 months (April 2003 to July 2004). All species with a ground level perimeter >10 cm and represented by at least three individuals, were selected and tagged. A total of 51 species represented by 156 individuals were recorded. Leaf flushing and leaf fall did not have seasonal variation and the species continued to gain and loose leaves during the dry (August to February) and rainy (March to July) seasons. Flowering, when evaluated by the Fournier's percentage, varied between 1.9% and 20.2%, with maximum intensity in December 2003 (16.4%) and January 2004 (20.2%). Likewise, fruiting varied between 3.8% and 21.4% with the highest percentages in February (17.2%) and March (21.4%) 2004. The analysis comparing reproductive phenological patterns with monthly rainfall did not show a significant correlation, which may suggest investigations concerning other factors, including biotic ones, as pollination and/or dispersal modes, which can be influencing reproductive events of plants in the studied Restinga forest.     

The chemical character and burial of phosphorus in shallow coastal sediments in the northeastern Baltic Sea

The chemical composition and vertical distribution of sediment phosphorus (P) in shallow coastal sediments of the northeastern Baltic Sea (BS) were characterized by sequential extraction. Different P forms were related to chemical and physical properties of the sediments and the chemistry of pore water and near-bottom water. Sediment P composition varied among the sampling sites located in the Archipelago Sea (AS) and along the northern coast of the Gulf of Finland (GoF): the organic rich sites were high in organic P (OP), while apatite-P dominated in the area affected by sediment transportation. Although the near-bottom water was oxic, the sediments released P. Release of P was most pronounced at the site with high sediment OP and reduced conditions in the sediment-water interface, indicating that P had its origins in organic sources as well as in reducible iron (Fe) oxyhydroxides. The results suggest that even though these coastal areas are shallow enough to lack salinity stratification typical for the brackish BS, they are vulnerable to seasonal oxygen (O₂) depletion and P release because of their patchy bottom topography, which restricts mixing of water. Furthermore, coastal basins accumulate organic matter (OM) and OP, degradation of which further diminishes O₂ and creates the potential for P release from the sediment. In these conditions, an abundance of labile OP may cause marked efflux of P from sediment reserves in the long-term.     

Atmospheric deposition of nutrients in a coastal maquis ecosystem of northeastern Greece

The deposition of nutrients N, P, Ca, Mg, Na and K from the atmosphere on a coastal maquis ecosystem was studied over a 12-month period (1981–1982). The annual precipitation during that period was 1065 mm. Nutrient input was estimated as 5.72, 0.24, 30.31, 3.40, 23.99 and 1616 kg ha^–1 year^–1 for N, P, Ca, Mg, Na and K, respectively. Chemical analysis of throughfall showed enrichment for all the nutrients studied. It was concluded that nutrient input from bulk precipitation is an important contribution to nutrient cycling of the Greek maquis ecosystem.     

Ichthyoplankton of the coastal waters of northeastern shelf of the Black Sea and the Kerch Strait

We study the state of summer ichthyoplankton and dynamics of its taxonomic composition and abundance near large harbor cities (Novorossiysk and Tuapse), as well as in the navigation areas and near transshipment harbor facilities (Taman?? Prichernomor??e and Kerch Strait). We show that temporal-spatial changes in the taxonomic composition and abundance of ichthyoplankton are determined by fluctuations of water temperature, pressure of predatory comb jelly Mnemiopsis leydyi and level of water pollution. High mortality rate and low abundance of fish eggs and larvae in the polluted areas of Novorossiysk, Tuapse, and Kerch Strait indicate unfavorable conditions for the embryonic and postembryonic development of fish in these areas. As judged by the state of ichthyoplankton the most favorable conditions are in the open part of the Novorossiysk Bay and Taman?? Prichernomor??e. Starting from 2002, the spawning populations of pelagophylic fish in the Novorossiysk Bay are gradually recovering to the level of 1980.     

Heterotrophic bacteria,zooflagellates, and ciliates in coastal waters of northeastern Black Sea

According to the parameters of density and biomass of heterotrophic bacterioplankton, waters in the ports of Novorossiysk and Tuapse were eutrophic-hypereutrophic and in the resort cities of Gelendzhik and Anapa they were hypereutrophic. The abundance of heterotrophic bacteria reached maximum values of 12.7–14.2 million cells/mL during the period of abnormally high water temperatures (August 2010) in recreational zones. Chainlike and filamentous forms (57–65%) of bacteria, which were typical for the strong coastal pollution of waters, prevailed. The abundance of zooflagellates (kinetoplastids) in semi-isolated water areas (port of Novorossiysk and Gelendzhik Bay) reached the level of highly eutrophic waters, 6.2–9.7 million ind/m³. However, the biomass of naked ciliates was 1.5 times lower than their maximum values earlier registered in coastal waters of the northeastern shelf. The peak of abundance of alien tintinnids of the genera Eutintinnus, Tintinnopsis, and Amphorellopsis, which were introduced via ballast waters of ships, was recorded in Novorossiysk Bay. The ratio of titinnids to the total abundance of ciliates increased 5 times and reached 25–40%. Protozoans developed poorly in the oil-polluted port of Tuapse and the open Anapa Bay.     

Type of mycorrhizal associations in two coastal nature reserves of the Mediterranean basin

We analysed the mycorrhizal types of two coastal Mediterranean plant communities. Plants belonging to 82 species of 46 families growing in two Mediterranean study sites located within a Regional Natural Park in Italy (Macchia Lucchese) and in a National Park in Croatia (Brijuni) were assessed for the type of their mycorrhizal associations. Mycorrhizas occurred in 83% and 90% of the plant species surveyed in Macchia Lucchese and in Brijuni, respectively. On the basis of macroscopic and microscopic characteristics, six different mycorrhizal types were found, and their co-occurrence in the same plant community showed the large mycorrhizal diversity in Mediterranean vegetation. Different occurrence patterns of mycorrhizal types have been recognised in diverse habitats within Macchia Lucchese, from sand dune plant communities to sclerophyllous woodland. Mycorrhizal type abundance calculated on a floristic basis was very different from that obtained using a vegetation cover index.     

Polychaeta (Annelida) associated with Thalassia testudinum in the northeastern coastal waters of Venezuela

Seasonal variations of polychaetes in a Thalassia testudinum bed were studied from June 2000 to April 2001 in Chacopata, northeastern Venezuela. Eight replicate samples were taken monthly with a 15 cm diameter core and the sediment was passed through a 0.5 mm mesh sieve. A total of 1,013 specimens, belonging to 35 species, was collected. The monthly density ranged from 387 ind/m2 (September) to 1,735 ind/m2 in May (x = 989+/-449 ind/m2). Species richness was lowest in August and September (8) and highest (25) in April (x = 18.00+/-5.29). The shoot density of Thalassia showed an average of 284+/-77.60 shoots/m2, with extreme values in February (164) and May (422). Species diversity ranged from 1.25 in August and 3.33 bits/ind in December (x = 2.47+/-0.64). Significant positive correlations were detected among the number of Thalassia shoots, polychaete abundance and species richness, as well as among species richness, polychaete abundance and species diversity. Species number and average density were found within the intervals of mean values reported in similar studies. The higher number of species and organisms obtained in March-April and June-July can be attributed to the recruitment correlated with the regional up-welling.     

Isotopic signatures and nutrient relations of plants inhabiting brackish wetlands in the northeastern coastal plain of Venezuela

The semi-diurnal tidal regime (≥2 m) in the Paria Gulf on the Atlantic coast of Venezuela, and the flat landscape of the region, allow the penetration for tens of km of marine waters into the rivers draining the northeastern coastal plain of the country. The levels of salinity, tidal flooding, and sedimentation decrease perpendicularly from the river channel toward the back swamps. The vegetation varies sequentially from fringe mangroves along the river margins, to back swamps containing forests dominated by Pterocarpus officinalis, herbaceous communities of Lagenocarpus guianensis, and palm swamps with Mauritia flexuosa, Chrysobalanus icaco, and Tabebuia spp. This environmental structure was used to test the hypotheses that: (a) mangrove distribution is strongly associated with salinity of interstitial water, and (b) they occupy areas where tidal influence and sediment dynamics determine a relatively open N cycle. Analyses of soil, water, and plants along a 1.5 km transect located near the confluence of the Guanoco and San Juan Rivers (Sucre and Monagas States, Venezuela) revealed that: (a) conductivity decreased from 11 to 0.2 mmhos cm⁻¹ from the river fringe to the internal swamp, whereas Na in the same stretch decreased from 100 to 2 μM; (b) average leaf tissue concentrations of Na, P, and N decreased significantly along the transect; (c) P. officinalis showed a large Na-exclusion capacity indicated by positive K/Na ratios from 8 to 200, and Crinum erubescens counteracted Na by accumulating K above 1,000 mmol kg⁻¹; (d) leaves varied widely in δ ¹³C (−25.5 to −32‰) and δ ¹⁵N (4 to −10.5‰) values. Samples were aggregated according to soil carbon content corresponding to those of the mangrove forest belt (5–28 mol C kg⁻¹; 0–650 from river fringe) and those of the back swamps (40–44 mol C kg⁻¹; 700–1,500 m from river fringe). The concentrations of Na, P, and N (in mmol kg⁻¹) and δ ¹⁵N values (in ‰) were significantly higher in the mangrove forest compared to the back swamp (Na 213 vs. 88; P 41 vs. 16; N 1,535 vs. 727; δ ¹⁵N 1.5 vs. −3.7), indicating that the fringe forest was not nutrient limited. These results support the hypotheses that mangroves are restricted to the more-saline sections of the transect, and that the fringe forest has a more open N cycle, favoring ¹⁵N accumulation within the system.     

Taxonomic composition and seasonal dynamics of the meroplankton of the coastal zone of the northeastern Black Sea

The composition and dynamics of the numerical density of meroplankton in the Bays and Seaports of the Northeastern Black Sea, viz., Novorossiysk, Tuapse, Gelendzhik, and Anapa were studied in the long-term aspect. The larvae of the benthic invertebrates of 73 taxa were identified. Meroplankton had their peak abundance period from May to September. Larvae of mollusca Mytilus galloprovincialis and Cardiidae gen sp. (Bivalvia) were dominant in the spring; larvae of mollusca Bittium reticulatum (Gastropoda), Mytilaster lineatus were dominant in the summer, and M. galloprovincialis, Anadara cf. inaequivalvis, Chamelea gallina (Bivalvia) were dominant in the autumn. Polychaete and cirriped larvae occurred in the plankton during the spring-autumn season. Complex species that are tolerant to pollution, such as Amphibalanus improvisus, M. lineatus, B. reticulatum, and the genus Polydora were abundant in Novorossiysk and the Tuapse.     

Zooxanthellae genotypes in the coral Siderastrea stellata from coastal reefs in northeastern Brazil

Siderastrea stellata is a common scleractinian coral that inhabits shallow reefs off the coast of Brazil. This species is considered to be very resistant to temperature and salinity variations and water turbidity, demonstrating great ecological plasticity and adaptability to environmental changes. Samples of S. stellata were taken from the Cabo Branco coastal reefs near João Pessoa, Brazil, every month for two years and analyzed using PCR and Restriction Fragment Length Polymorphisms of SSU rDNA techniques. The data indicated that during the study period S. stellata hosted only one SSU rDNA genotype of Symbiodinium with the RFLP pattern of clade C. The presence of clade C zooxanthellae in S. stellata in northeastern Brazilian reefs shows the wide geographical distribution of this clade, and it may aid bleaching recovery in S. stellata. Furthermore, the association of S. stellata with a zooxanthellae clade considered to be one of most resistant to bleaching may help to explain the high ecological plasticity of this scleractinian species, its capacity to reverse bleaching, and its high resistance and resilience to environmental disturbances.     

Isostatic rebound in the northwestern part of the Lake Agassiz basin: Isobase changes and overflow

Based on new GPS elevation data on the Upper and Lower Campbell strandlines in the northwestern part of the glacial Lake Agassiz basin, the trend of isobases representing differential glacio-isostatic rebound in that region is shown to bend and assume a nearly west-east orientation. This differs from the northwest-southeast orientation to the southeast of the study area, which others had projected into the northwestern corner of the Lake Agassiz basin; this means that there was more isostatic depression than previously thought north of ∼ 53°N. The difference in slopes on reconstructed water planes of the Upper and Lower Campbell beaches is less with these isobases, which better reflects the short period of time between their formation. It is likely that the change in orientation of isobases reflects the presence of a thick Keewatin ice center to the north. Our revised west-east isobase reconstruction indicates that when the lake was at the Campbell beach levels, ∼ 9900-9400 ¹⁴C B.P., Lake Agassiz overflowed across the paleo-divide at Wycherley Lake, Saskatchewan, which controlled flow through the Northwestern Outlet of Lake Agassiz during part of its history; overflow would not have occurred through the Wycherley Lake channels at this time using the old isobase projections.