Subfossil chironomids (Diptera,Chironomidae) in three Tatra Mountain lakes (Slovakia) on an acidification gradient

Three lakes were studied in the High Tatra Mountains at altitudes from 2000 to 2157 m a.s.l., which represent three categories of acidity status recognised in the Tatra lakes in the 1980s: non-acidified, acidified, and strongly acidified. Subfossil chironomid remains from dated sediment cores covering ca. throughout 200 years were analysed. The chironomid thanatocoenoses of all cores layers reflected ultra-oligotrophic non-acidified conditions in L’adové pleso. Nevertheless, the finding of the acid-tolerant species Zalutschia tatrica in littoral samples in 1980s indicates that the littoral zone was more influenced by acidification than deeper areas of the lake. Three stages of lake developmental history can be distinguished in the acidified lake Vy?né Wahlenbergovo pleso based on the chironomid subfossil record: the pre-acidification stage before the 1920s, the anthropogenic acidification stage between the 1920–1980s, and the recovery of the lake from the end of the 1980s. The period of acidification was accompanied by a decline in chironomid numbers, while chironomid fauna composition was unchanged during the whole investigated history of the lake. None of the chironomid taxa present prior to the acidification period disappeared during the peak of acidification. The most apparent change in the sediment record taken from the strongly acidified lake Starolesnianske pleso was recognised in the layers corresponding to the period 1960–1980. It is characterised by the disappearance of the dominant acid-sensitive Tanytarsus lugens group and the dominance of acidtolerant Tanytarsus gregarius group. The most recent chironomid assemblage probably benefits from the amount of food resources as a result of increased lake productivity induced by acidification.     

Phytoplankton of a mountain lake (L’adové pleso,the Tatra Mountains,Slovakia): Seasonal development and first indications of a response to decreased acid deposition

A one-year study of the phytoplankton of remote mountain lake L’adové pleso (2057 m. a.s.l.), situated in the High Tatra Mountains, was carried out in 2000–2001. Seasonal development of the species structure and depth distribution of biomass, as well as chlorophyll-a concentrations, and chemical characteristics of the lake water were examined. The phytoplankton was made up of a low number of nanoplanktonic unicellular species, mainly flagellates from Cryptophyceae and Chrysophyceae. Plagioselmis lacustris, Cryptomonas cf. erosa and Ochromonas spp. were the most important with regards to both abundance and biomass. The phytoplankton showed a marked seasonal development. During most of the ice-covered period, abundances of phytoplankton remained very low. In regard to the vertical distribution, both species composition and total biomass were clearly stratified during most sampling dates. The amount of chlorophyll-a per unit biovolume varied considerably, and significantly higher values were found on sampling dates with complete or partial ice cover. Our data on pH and phytoplankton were compared with a previous study in 1990–1991 in order to evaluate possible changes associated with the decrease of acid deposition. The extent of episodic acidification of the lake water has diminished both in time and space, and lake water pH has slightly increased. We observed a shift in species composition, and an important increase of total phytoplankton abundance. This could be considered as a first sign of biological response to changing chemical conditions.     

Macrozoobenthos of two different catchment areas of the tatra mountain lakes with a special reference on the effects of acidification

The structure of macrozoobenthos of two different high-mountain Tatra lakes, namely Starolesnianske pleso (strongly acidified) and Ni?né Terianske pleso (reference site) is described. The latter is characterised by a large catchment and total area, and is relatively deep with strong inlet and outlet. It is not affected by acidification. Univoltine species of mayflies, stoneflies and caddisflies dominate in the littoral, mainly scrapers. Predators are represented by stoneflies. Shredders dominate in the lake outlet. From the zoogeographic point of view, Carpathian endemites and Central European species prevail. Forty percent of species are sensitive to acidification. The former has a smaller catchment and total area, and is relatively shallow, without inlet. It is strongly affected by acidification. Semivoltine species, mainly predators (beetles) and shredders prevail. From the zoogeographic point of view Palaearctic species dominate. Species sensitive to acidification are missing. Emergence of water insects has two peaks during spring and fall circulation.     

Seasonal dynamics of chironomids in the profundal zone of a mountain lake (L’adové pleso,the Tatra Mountains,Slovakia)

The profundal community of L’adové pleso (an oligotrophic high mountain seepage lake at an altitude of 2,057 m with a max. depth of 18 m and an ice-cover period from October–July) was studied from December 2000–October 2001. Chironomidae, the most significant part of the studied community, are represented by four taxa and dominated by Micropsectra radialis Goetghebuer, 1939 and Pseudodiamesa nivosa (Goethgebuer, 1928). These two species showed a 1-year life cycle. The total densities of chironomids varied from 0 to 5,927 ind. m^?2; no chironomids, or very low densities, were found during the winter/spring period, probably due to low oxygen concentrations in the medial part of the lake. These low oxygen concentrations probably caused the relocation of larvae from the medial part of the sedimentary area at the same time.     

Late glacial finds ofPinus cembra L. in the Lubovnianská kotlina Basin

During the palaeobotanical investigation of the Spi?ská kotlina Basin and the neighbouring areas, seeds ofPinus cembra L. were found in limonitized concretions and peat sediment of the Sivárňa mire situated near the village of Vy?né Ru?bachy (east of the High Tatra). The presence of this tree species was also confirmed by pollen analysis. It is the first find of fossil seeds dating from the Late glacial in Czechoslovakia.     

Are they still viable? Physical conditions and abundance of <Emphasis Type="Italic">Daphnia pulicaria</Emphasis> resting eggs in sediment cores from lakes in the Tatra Mountains

All species of Daphnia (Cladocera) produce, at some stage in their life cycle, diapausing eggs, which can remain viable for decades or centuries forming a “seed bank” in lake sediments. Because of their often good preservation in lake sediment, they are useful in paleolimnology and microevolutionary studies. The focus of this study was the analysis of cladoceran resting eggs stored in the sediment in order to examine the ephippial eggs bank of Daphnia pulicaria Forbes in six mountain lakes in the High Tatra Mountains, the Western Carpathians (northern Slovakia and southern Poland). Firstly, we analyzed distribution, abundance and physical condition of resting eggs in the sediment for their later used in historical reconstruction of Daphnia populations by genetic methods. To assess changes in the genetic composition of the population through time, we used two microsatellite markers. Although DNA from resting eggs preserved in the High Tatra Mountain lake sediments was extracted by various protocols modified for small amounts of ancient DNA, DNA from eggs was not of sufficient quality for microsatellite analyses. Distribution curves of resting eggs from sediment cores correspond to the environmental changes that have occurred in the High Tatra Mountains area during last two centuries (atmospheric acid deposition, fish introduction) and demonstrate their influence on natural populations. Evaluation of ephippia physical condition (the most common category was empty ephippial covers) suggests that the majority of resting eggs hatched to produce a new generation of Daphnia or may be due to failed deposition of resting eggs by Daphnia to the chitinous case. In conclusion, age, low quantity and poor physical condition of resting eggs from these Tatra lake sediments proved to be unsuitable not just for use in genetic analyses, but also the possibilities of autogenous restoration of Daphnia populations from the resting egg banks in the Tatra sediments are negligible.     

Pollen and macroscopic analyses of sediments from two lakes in the High Tatra mountains, Slovakia

The paper presents the results of investigations concerning the accumulation processes, sediment composition, pollen and macroscopic analyses of sediments from the lakes Popradské pleso (1513 m) and Štrbské pleso (1345 m) in the High Tatra mountains, western Carpathians, Slovakia. While Popradské pleso is undoubtedly of glacial origin with silts in the Lateglacial layers and algal gyttja in the Holocene layers, Štrbské pleso or its greater part originated recently between the 16th and the beginning of the 18th centuries when the previous bog of Atlantic or early Subboreal age was flooded with water after the dispersed outflow from the bog depression was blocked. Our pollen and macrofossil analyses indicate mountain tundra in the Lateglacial and a continuous presence of coniferous forest with Picea abies with admixture of Pinus cembra, Larix decidua, Juniperus communis and Pinus cf. mugo in the uppermost elevations at the alpine forest limit since the very beginning of the Holocene. No noticeable oscillation of the forest line can be interpreted from our pollen analyses. It seems probable that its position was controlled by geomorphological and edaphic conditions rather than by the Holocene climatic changes. Spruce forests dominated at elevations between ca. 1000–1400 m during the whole Holocene.     

Late Quaternary diatoms in the sediments of Przedni Staw Lake (Polish Tatra Mountains)

The paper presents a diatom succession in the Late Glacial and Holocene sediments of the Przedni Staw lake in the Pie Stawów Polskich Valley High Tatra Mts. Ten diatom phases are distinguished and presented against a pollen diagram from the analyzed core showing continuous sedimentation from the Oldest Dryas to the Subatlantic period. The diatom flora in the Late Glacial sediments is predominantly littoral — Fragilaria, Navicula, Nitzschia, Diploneis, Pinnularia and Amphora species. The Holocene sediments enclose more abundant planktonic species such as Cyclotella quadriiuncta, Asterionella formosa and Melosira distans.     

Identifying century-old long-spined <Emphasis Type="Italic">Daphnia</Emphasis>: species replacement in a mountain lake characterised by paleogenetic methods

Mountain lakes often harbour morphologically or genetically unique populations of zooplankton species, including cladocerans. Daphnia lacustris Sars, predominantly found in Fennoscandia but also known from two Central European lakes in the Tatra Mountains, is one of such taxa. This Daphnia species often forms morphotypes with extremely long tailspines. Historical literature from a century ago documented similar morphs from another lake in the Tatra mountain range, presently inhabited by the phenotypically very different D. galeata. Using a paleogenetic approach (partial sequencing of the mitochondrial gene for 12S rRNA from preserved ephippial eggs in the lake sediment), we tested the hypothesis that Daphnia species composition changed in the lake due to anthropogenic disturbances, and that long-spined morphs were actually another relict population of currently extinct D. lacustris. Ephippia with extremely long spines were successfully retrieved from sediment cores. Despite being morphologically very well preserved, intact eggs were found in less than 2% of analysed ephippia. Genetic analyses, benefiting in most cases from amplification of short 12S fragments using internal primers, proved that long-spined ephippia belonged to D. longispina, which apparently coexisted with D. galeata in the mid-twentieth century. Our results confirm that paleogenetic methods are useful for studying the recent population structures of zooplankton species forming dormant egg banks but lacking reliably identifiable remains in sediments, and show that the extreme development of tailspines in mountain-lake Daphnia is associated with as-yet unclear environmental factors rather than taxonomic status.     

The assessment of 210Pb data from sites with varying sediment accumulation rates

The last few years have seen a dramatic growth in the use of ²¹⁰Pb sediment dating. Despite this, considerable doubt still surrounds the nature of the processes by which ²¹⁰Pb is deposited in lake sediments, and this has lead to a situation where there is a choice of dating models offering different interpretations of ²¹⁰Pb data. In assessing ²¹⁰Pb data it is therefore essential to first of all determine whether data is consistent with the assumptions of the dating model, and to then compare the ²¹⁰Pb chronology with independent dating evidence. We have tested ²¹⁰Pb data from a wide variety of sites, and our calculations indicate that the crs (constant rate of ²¹⁰Pb supply) model provides a reasonably accurate chronology when the total ²¹⁰Pb contents of cores from neighbouring locations are comparable.     

Radiometrically determined dates and sedimentation rates for recent sediments in nine North African wetland lakes (the CASSARINA Project)

Sediment cores were collected from nine wetland lakes in Morocco, Tunisia and Egypt for the CASSARINA project investigating environmental change in Northern African wetlands. The cores were dated radiometrically by using natural (²¹⁰Pb) and artificial (¹³⁷Cs and ²⁴¹Am) radionuclides. At sites in Morocco and Tunisia with mean annual rainfall totals ranging from 500–1000 mm yr^–1, fallout records were generally satisfactory and it was possible to develop independent sediment chronologies based on the radiometric data alone. At the Egyptian sites, rainfall was less than 200 mm yr^–1 and fallout records were much less distinct. At these sites the radiometric data could only be used to give an indication of mean sedimentation rates during the past 30–40 years. By using a combination of fallout radionuclide, pollen, and macrofossil stratigraphic records it was however possible to determine a credible sediment chronology spanning the major part of the 20th century. Applying this chronology to records of spheroidal carbonaceous particles (SCP) from the same sediment cores, the onset of significant levels of atmospheric pollution in the Nile Delta is dated in all three cores to the mid 1950s. Results from a number of lakes (Sidi Bou Rhaba, Ichkeul and Korba) revealed high and accelerating siltation rates, threatening their continued existence beyond the next few decades. In contrast, sedimentation rates at all three Nile Delta sites appear to have declined in recent decades, most probably due to the impact of the Nile barrages.     

A deep dig––hindsight on Holocene vegetation composition from ancient environmental DNA

Want a glimpse at past vegetation? Studying pollen and other plant remains, which are preserved for example in lake sediments or mires for thousands of years, allows us to document regional occurrences of plant species over radiocarbon‐dated time series. Such vegetation reconstructions derived from optical analyses of fossil samples are inherently incomplete because they only comprise taxa that contribute sufficient amounts of pollen, spores, macrofossil or other evidences. To complement optical analyses for paleoecological inference, molecular markers applied to ancient DNA (aDNA) may help in disclosing information hitherto inaccessible to biologists. Parducci et al. (2013) targeted aDNA from sediment cores of two lakes in the Scandes Mountains with generic primers in a meta‐barcoding approach. When compared to palynological records from the same cores, respective taxon lists show remarkable differences in their compositions, but also in quantitative representation and in taxonomic resolution similar to a previous study (Jørgensen et al. 2012). While not free of assumptions that need critical and robust testing, notably the question of possible contamination, this study provides thrilling prospects to improve our knowledge about past vegetation composition, but also other organismic groups, stored as a biological treasure in the ground.     

Paleolimnological studies of annually-laminated sediments in Loe Pool,Cornwall, U.K.

The sediments of Loe Pool, a eutrophic coastal lake in south west England, consist largely of laminated clays and clay-gyttjas. Studies of the diatom microstratigraphy of frozen sediment cores from the Pool indicate that the laminations are annual, and that they contain pairs of light and dark bands formed by seasonal variations in the supply of sediment to the Pool from its catchment. Analysis of the magnetic properties of individual laminations demonstrates the presence of physical and mineralogical microstratigraphic variations, which may also be related to seasonality. A varve chronology, which is confirmed by ¹³⁷Cs analysis and historical records, has been used to provide a timescale for the interpretation of data from other paleolimnological studies. A close agreement between variations in the abundance of sedimentary Sn, and the history of mining in the catchment, has been found. Similarly, analysis of total organic matter, total phosphorus, sedimentary chlorophyll a, sterols, diatoms and Cladocera in the uppermost sediments all indicate eutrophication of the Pool in the period AD 1940 to the present.     

Palynologische Erforschung archäologischer Proben aus dem Komořanské jezero-See bei Most (NW-Böhmen)

From the sediments of the former Komo?anské jezero Lake near Most, pollen analysis of samples linked with archaeological finds has been performed. One reference profile has been pollenanalytically elaborated, followed by pollenanalytical dating of various isolated samples. The samples elaborated were linked with the following cultural periods: of stroked pottery, of funnel beakers, of domestic specimens of Baden pottery, of corded pottery, of the Únětice culture, and of the Middle Ages. A reconstruction of the natural surroundings in various developmental epochs, especially that of the vegetation, has been performed in the locality, in its close vicinity and in more distant neighbourhoods (Komo?anské jezero Lake, the Podkru?nohorská panev Basin, the Kru?né hory Mountains, the ?eské st?edoho?í Mountains). The results refer to the Atlantic, Subboreal and Subatlantic periods. The differentiation of the Subboreal in the area under study is still uncertain.     

Chemical composition of the Tatra Mountain lakes: Response to acidification

Data from two surveys of the Tatra Mountain lakes (Slovakia and Poland) performed in the autumns of 1984 (53 lakes) and 1993 or 1994 (92 lakes) were used to estimate spatial variability in water chemistry in this lake district during the period of maximum European acid deposition. The ionic content of the lakes was generally low, with conductivity (at 20°C) ranging from 1.1 to 4.7 mS m^?1 and 23% of the lakes had a depleted carbonate buffering system. Major factors governing differences in lake-water chemistry were bedrock composition and amount of soil and vegetation in their catchment areas. Compared to lakes in the predominantly granitic central part of the Tatra Mountains, lakes in the West Tatra Mountains had higher concentrations of base cations and alkalinity due to the presence of metamorphic rocks in the bedrock. Concentrations of phosphorus, organic carbon, organic nitrogen, and chlorophyll-a were highest in forest lakes and decreased with decreasing density of vegetation and soil cover in the catchment areas. Concentrations of nitrate showed an opposite trend. Several exceptions to these general patterns in chemical and biological composition were due to exceptional geology or hydrology of the lake catchments.     

The role of pingos in the development of the Dzhangyskol lake–pingo complex,central Altai Mountains,southern Siberia

Dzhangyskol is a small lake of glacial origin in the central part of the Altai Mountains in southern Siberia. Pollen stratigraphies and chronologies of two cores record the vegetational development of the area from the Late Glacial treeless landscape to the forest and steppe of today. The modern lake is a remnant of a much larger ice-dammed lake, which was reduced in size and then temporarily drained after diversion of the inflowing mountain meltwater stream, which had low δ¹⁸O values. The dry lake floor allowed development of permafrost and small pingos (frozen mounds of lake sediments). With the onset of greater climatic humidity in the mid-Holocene, the input of local water with higher δ¹⁸O caused a rise in lake level, drowning the earlier pingos. Growth of a broad fen on the margin of the lake led to formation of a modern pingo complex.     

Qualitative changes in the planktonic Cladocera assemblage of a High Tatra Mountains lake during the last 100 years

During the last roughly 100 years (1881–1989) some noteworthy changes have occurred in the planktonic Cladocera taxocene of the lake Popradské pleso (High Tatra Mts., Czecho-Slovakia). Primarily, in course of the twenties up to the fifties of our century Daphnia pulicaria and Polyphemus pediculus, and later also Holopedium gibberum, disappeared from the plankton of the lake. Conversely, approximately from the mid-seventies, Daphnia longispina has become a constituent of the lake plankton. In spite of lacking data on the principal parameters of the abiotic and biotic environment from the past, the author assumes that probably the most important factor responsible for the changes referred to were fluctuations in the predation pressure of fish. Besides, organic pollution might have played a definite but less important role.     

Alternation of respiratory pathways during the development of wheat leaf

P?i vývoji listu p?enice se zmen?uje stupeň inhibice dýchání fluoridem, monojodacetátem a malonátem a poměr mezi radioaktivitami¹⁴CO₂ uvolněného z glukosy-6-¹⁴C a glukosy-l-¹⁴C (C₆/C₁), co? svěd?í o zvět?ování podílu pentosovího cyklu v celkové respiraci. Tato změna v?ak neni zp?sobena absolutním zvět?ením aktivity pentosového eyklu u star?ích list?, nýbr? p?edev?ím poklesem aktivity glykolytického systému. Naproti tomu u list? oddělených od obilky se pri sní?ení vlhkosti atmosféry méní poměr mezi dýchacími cestami v d?sledku aktivace pentosového cyklu. Na základě disproporce mezi procentem glykolytického podílu respirace vypo?tenym ze sní?ení poměru C₆/C₁ p?i inhibici dýchání fluoridem a procentem inhibice dý chání fluoridem bylo diskutováno o mo?ných p?íoinách vysokých poměr? C₆/C₁ u mladých list?, u nich? byly v některých p?ípadech zji?těny hodnoty těchto poměr? dokonce vy??í ne? jedna.     

Increased sensitivity of the respiratory system of plants grown in gibberellic acid toward fluoride

V souvislosti s d?ívěj?imi údaji (Lu?tinec a Krektjle 1959, Lu?tinec, Krekule a PokornÁ 1960) o silném inhibi?ním ú?inku fluoridu na dychání rostlin pěstovaných v roztoku kyseliny giberelové byl pomocí specificky zna?ené glukosy a respira?ních inhibitor? zji?tován vztah krátko- i dlouhodobého p?sobení kyseliny giberelové k poměru mezi podíly glykolytického a pentosofosfátového odbourání v respiraci list? p?enice. V souhlase s výsledky Fanga a spol. (1960) byIo zji?těno, ?e kyselina giberelová v koncentracích 2 a? 80 mg/l neovlivńuje během několikahodinového p?sobení na roz?ezané listy p?enice poměr radioaktivit¹⁴CO₂ uvolněného z glukosy-6-¹⁴C a -1-¹⁴C (C₆/C₁) ani nemění v koncentraci 10 mg/l stupeń inhibice dýchání fluoridem, monojodacetátem a malonátem a spot?ebu kyslíku. Výdej¹⁴CO₂ z glukosy-l-¹⁴C a -6-¹⁴C kyselina giberelová sni?uje v lineární závislosti na pou?itých koncentracích. U rostlin pěstovaných v roztoku kyseliny giberelové (10–20 mg/l) se rychleji sni?uje poměr C₆C₁ i absolutní hodnoty radioaktivity během několika dní od vyklí?ení, ne? u rostlin pěstovaných ve vodě. To svěd?í o rychlej?ím zvět?ování podílu pentosového cyklu v respiraci pokusných rostlin. Fluorid brzdí p?i stejném nebo men?ím obsahu ve tkáni dýchání list? rostlin pěstovaných v roztoku kyseliny giberelové silněji ne? dýchání rostlin pěstovaných ve vodě, zatimco ûcinek monojodacetátu a malonátu je u stejně starých rostlin (4 dny) obou variant stejný. O mo?ných p?í?inách tohoto jevu bylo diskutováno.     

Nitrogen transformations at the sediment–water interface across redox gradients in the Laurentian Great Lakes

The capacity of a lake to remove reactive nitrogen (N) through denitrification has important implications both for the lake and for downstream ecosystems. In large oligotropic lakes such as Lake Superior, where nitrate (NO₃ ^?) concentrations have increased steadily over the past century, deep oxygen penetration into sediments may limit the denitrification rates. We tested the hypothesis that the position of the redox gradient in lake sediments affects denitrification by measuring net N-fluxes across the sediment–water interface for intact sediment cores collected across a range of sediment oxycline values from nearshore and offshore sites in Lake Superior, as well as sites in Lake Huron and Lake Erie. Across this redox gradient, as the thickness of the oxygenated sediment layer increased from Lake Erie to Lake Superior, fluxes of NH₄ ⁺ and N₂ out of the sediment decreased, and sediments shifted from a net sink to a net source of NO₃ ^?. Denitrification of NO₃ ^? from overlying water decreased with thickness of the oxygenated sediment layer. Our results indicate that, unlike sediments from Lake Erie and Lake Huron, Lake Superior sediments do not remove significant amounts of water column NO₃ ^? through denitrification, likely as a result of the thick oxygenated sediment layer.