Informacja

Drogi użytkowniku, aplikacja do prawidłowego działania wymaga obsługi JavaScript. Proszę włącz obsługę JavaScript w Twojej przeglądarce.

English (EN)·Polski (PL)·Yкраїнський (UK)
Przejdź do strony domowej biblioteki Centralna Biblioteka Wojskowa Link otwiera się w nowym oknie Logo biblioteki Prolib Integro - strona głównaCentralna Biblioteka Wojskowa

Wyszukujesz frazę "Cladocera" wg kryterium: Temat

  Lista filtrów
Wyrównaj
Wyświetlanie 1-25 z 39
Tytuł:
Ewolucja środowiska w rynnie jeziora Jasień w obrazie palinologicznym i zmian fauny Cladocera
Environmental change in the Jasień Lake trough as revealed by palynology and Cladocera faunal change
Autorzy:
Miotk-Szpiganowicz, G.
Niska, M.
Powiązania:
https://bibliotekanauki.pl/articles/294308.pdf
Data publikacji:
2008
Wydawca:
Stowarzyszenie Geomorfologów Polskich
Tematy:
paleolimnologia
analiza pyłkowa
analiza Cladocera
palaeolimnology
palynological analysis
Cladocera analysis
Opis:
Na obszarze rynny jeziora Jasień zlokalizowano cztery stanowiska, dla których wykonano analizę palinologiczną i analizę szczątków Cladocera. Celem badań było odtworzenie przemian środowiska przyrodniczego na tym terenie. Rdzenie, z których pobrano próby do analiz, składały się głównie z osadów typu gytia i torf. Próbki do analiz wykonywano według standardowych procedur. Do obróbki danych liczbowych wykorzystywano program POLPAL. Otrzymane wyniki palinologiczne umożliwiły odtworzenie historii roślinności badanego terenu począwszy od okresu borealnego, a analiza szczątków Cladocera dostarczyła informacji o fazach rozwoju części zbiornika jeziornego Obrowo Duże.
In order to reconstruct the environmental history of the Jasień Lake trough, pollen analysis and an analysis of Cladocera remains have been simultaneously carried out. Sediments for pollen research have been collected in the bay section of the Jasień Lake and in the Obrowo Małe peat bog. Cladocera remains have been sampled in two sites within a peat bog adjacent to the Obrowe Duże Lake. Preparation of samples for both analyses followed standard procedures. Numerical data have been elaborated using the POLPAL software. The results of the palynological study have allowed to decipher vegetation history since the Boreal period. The peat bog of Obrowo Małe began to form at the onset of the Atlantic period. Cladocera remains yielded information about phases of water body evolution in the part of the Obrowo Duże Lake, which subject to silting transformed into a low-level valley bog, and then into a transitional peat bog. Pollen and Cladocera analyses have been carried out on material collected at dissimilar sites, which practically excludes the possibility of correlation of results and allowed one only to reconstruct the major hydrological changes, common for the entire region. In the latest Holocene, in the Jasień Lake trough a trend towards water level decrease is observed due to both climatic and human impact. Further changes included the rise of trophic level in the lake and vegetation succession onto the shallower parts of the lake.
Źródło:
Landform Analysis; 2008, 7; 102-112
1429-799X
Pojawia się w:
Landform Analysis
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
The long-lasting resistence of diapausing eggs from Arctic Cladocera frozen at 18°C
Autorzy:
Meijering, Meertinus P.D.
Powiązania:
https://bibliotekanauki.pl/articles/2052078.pdf
Data publikacji:
2003
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
Arctic
Cladocera
diapausing eggs
Źródło:
Polish Polar Research; 2003, 24, 2; 167-172
0138-0338
2081-8262
Pojawia się w:
Polish Polar Research
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Younger Dryas climatic reconstructions in central Poland
Autorzy:
Pawłowski, D.
Powiązania:
https://bibliotekanauki.pl/articles/139212.pdf
Data publikacji:
2017
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
Younger Dryas
cladocera
temperature
oxbow lake
climate
młodszy dryas
Cladocera
temperatura
starorzecze
klimat
Opis:
Cladoceran-based paleotemperature estimates for the Younger Dryas for ten sections of paleo-oxbow lakes, valley mires, and lacustrine sediments from central Poland are presented, and their potential usefulness to climatostratigraphy is described. Most of the changes observed in the cladoceran assemblages are responses to climate changes. The cladoceran-based temperature reconstructions reflect cold conditions during the Younger Dryas (YD) and allow a division of this period into two phases: an older colder phase, between 12,800 and 12,000 cal yrs BP, and a younger, warmer phase, between ca. 12,000 and 11,500 cal yrs BP. The geomorphological features of the study sites and local environmental forces are also taken into consideration. The cladoceran-inferred summer temperature estimates from all of the study sites correspond closely with the available climate reconstruction for the YD in central Europe.
Źródło:
Acta Geologica Polonica; 2017, 67, 4; 567-584
0001-5709
Pojawia się w:
Acta Geologica Polonica
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Description of subfossil post-abdomen and post-abdominal claw of Ceriodaphnia (Cladocera, Daphniidae)
Autorzy:
Nevalainen, Liisa
Powiązania:
https://bibliotekanauki.pl/articles/2026911.pdf
Data publikacji:
2007
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
Cladocera
Ceriodaphnia
subfossil remains
identification
Opis:
Cladoceran remains preserve selectively in lake sediments. Possibly all Cladocera species leave at least some identifiable remains in lake sediments. Exosceletal body parts of families Chydoridae and Bosminidae preserve best but other families are only variably represented in sediments by their outer body parts. Identification of all possible remains helps to achieve more precise palaeolimnological reconstruction of past ecosystems by Cladocera analysis. This article describes, together with photograph and line drawing the subfossil post-abdomen and post-abdominal claw of Ceriodaphnia, previously not widely identified.
Źródło:
Studia Quaternaria; 2007, 24; 65-67
1641-5558
2300-0384
Pojawia się w:
Studia Quaternaria
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Air temperature and water level inferences from northeastern Lapland (69°N) since the Little Ice Age
Autorzy:
Luoto, Tomi P.
Kivilä, E. Henriikka
Kotrys, Bartosz
Płóciennik, Mateusz
Rantala, Marttiina V.
Nevalainen, Liisa
Powiązania:
https://bibliotekanauki.pl/articles/2041809.pdf
Data publikacji:
2020
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
Arctic
paleoclimate
precipitation
temperature
Chironomidae
Cladocera
Źródło:
Polish Polar Research; 2020, 41, 1; 23-40
0138-0338
2081-8262
Pojawia się w:
Polish Polar Research
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Findings of Alona protzi Hartwig 1900 (Branchiopoda: Anomopoda. Chydoridae) in Finland
Autorzy:
Nykänen, Mirva
Sarmaja-Korjonen, Kaarina
Powiązania:
https://bibliotekanauki.pl/articles/2026957.pdf
Data publikacji:
2007
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
Cladocera
Alona protzi
biogeography
ecology
Finland
Opis:
Alona protzi is a rare spe cies of Cla do cera, oc cur ring in lake lit to ral through out Europe. How ever, lit tle is known about this ani mal, and so far it has not been in cluded in pro vi sional lists of spe cies found in Fin land. In this short re port we pres ent our find ings of Alona protzi, both re cent and sub fos sil ma te rial, as well as one pre vi ous, un pub lished finding site of the spe cies in Fin land. We found three sub fos sil shells of this spe cies in the bot tom sedi ments of two lakes. In a third lake we found in tact ani mals, an ephip pial fe male and a male, while sam pling stony bot tom of lake lit to ral.
Źródło:
Studia Quaternaria; 2007, 24; 73-77
1641-5558
2300-0384
Pojawia się w:
Studia Quaternaria
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Cercopagis pengoi (Cladocera) conquered the southern Baltic Sea
Autorzy:
Zmudzinski, L.
Powiązania:
https://bibliotekanauki.pl/articles/85031.pdf
Data publikacji:
1998
Wydawca:
Akademia Pomorska w Słupsku
Tematy:
Cercopagis pengoi
Cladocera
Baltic Sea
water flea
Opis:
The Ponto-Caspian cladocera Cercopagis pengoi invaded the Baltic Sea in 1992. For the first time it was recorded in the Gulf of Riga and three years later it appeared in the Gulf of Finland. In the summer of 1999 it had been also found in huge numbers in shallow areas (0.5 - 10 m) of the Gulf of Gdańsk.
Źródło:
Baltic Coastal Zone. Journal of Ecology and Protection of the Coastline; 1998, 02
1643-0115
Pojawia się w:
Baltic Coastal Zone. Journal of Ecology and Protection of the Coastline
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Palaeohydrological aspect of transformation of lakes into peat bogs during Middle Holocene on the basis of Cladocera analysis in the northern Poland
Autorzy:
Szeroczyńska, Krystyna
Gąsiorowski, Michał
Powiązania:
https://bibliotekanauki.pl/articles/2027409.pdf
Data publikacji:
2002
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
Cladocera remains
fossil lakes
Middle Holocene
palaeohydrology
Opis:
Cladocera are a group of water animals, which are strongly dependent on environmental conditions. The ratio of planktonie to littoral Cladocera species is a widely used tool in palaeohydrological reconstruction of lakes' water level changes. Interpretation of this ratio is still unclear and requires further evidence. The simplest indicator of water level, which can be used in tracing lake-peat bog transitions, is the presence or absence of Cladocera and the character of its disappearance. In general, two models of Cladocera decline are observed. The first model is characterized by a very abrupt disappearance of all species, whereas the second one. with an intermediate stage, is characterized by domination of specific species. These two models are related to different types of terminal history of the water body. Even after a total disappearance of water in the peat bogs, there were episodes of some pioneer cladoceran species presence, correlated with periods of humid climate.
Źródło:
Studia Quaternaria; 2002; 55-60
1641-5558
2300-0384
Pojawia się w:
Studia Quaternaria
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Fossil Cladocera re mains in the Eemian sediments – preservation, frequency and dominant species
Autorzy:
Niska, M.
Powiązania:
https://bibliotekanauki.pl/articles/2027074.pdf
Data publikacji:
2012
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
Cladocera analysis
palaeocology
Eemian Interglacial
Early Vistulian
Polska
Opis:
This pa per pres ents the re sults of fos sil Cladocera anal y sis us ing ma te rial ob tained from seven palaeolakes of the Eemian inter gla cial lo cated in Po land. The main aim of this study was to in ves ti gate the state of pres er va tion and diver sity of spe cies in the Eemian Cladocera. The stud ied Eemian lakes were formed at the end of the Wartanian Gla ciation in tun nel and ket tle holes. They had pre served a con tin u ous re cord of en vi ron men tal changes through out the Eemian inter gla cial, un til the Vistulian Gla ci ation. Cladocera fos sils found in Eemian sed i ments were thin ner and had a more dam aged struc ture than fos sils from the Ho lo cene. Low de gree of fos sil pres er va tion forced to de velop an al terna tive method for prep a ra tion of the fos sils for the mi cro scopic anal y sis. Cladocera spe cies found in the ex am inedpalaeolakes cor re sponded to the pres ent-day spe cies in hab it ing Po land and Cen tral and North ern Eu rope. The changes in species composition resulting from climate changes corresponded to the current geographic distribution of Cladocera. De spite the poor con di tion of the ob tained fos sil re mains, the re sults showed that cladoceran fos sils in sed i ments of palaeolakes may be used in the re con struc tion of en vi ron men tal con di tions from the pe riod pre ced ing the last gla ci ation.
Źródło:
Studia Quaternaria; 2012, 29; 31-43
1641-5558
2300-0384
Pojawia się w:
Studia Quaternaria
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Distribution of Cladocera communities across a climate gradient in shallow lakes from Croatia to Hungary: a preliminary study
Autorzy:
Kövér, Csilla
Korponai, János
Katalinic, Ana
Bereczki, Csaba
Powiązania:
https://bibliotekanauki.pl/articles/2027088.pdf
Data publikacji:
2012
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
Subfossil Cladocera
cli mate change
train ing set
Opis:
Cladocera com mu ni ties in sur face sed i ments of seven lakes were sam pled from the Med i ter ra nean to north Hun gary. Con duc tiv ity, pH, pri mary ions (Ca2+, Mg2+, Na+, K+, Cl–, SO4 2–, HCO3 –, CO3 2–) and macrophyte cov er age were measured as con trib uted en vi ron men tal pa ram e ters for the dis tri bu tion of cladoceran com mu ni ties across the lakes. Thirtytwo cladoceran spe cies were found in the seven lakes. The re corded spe cies have wide tol er ance spec tra, and are able to col o nize very dif fer ent kind of hab i tats. The most com mon and abun dant spe cies were Chydorus sphaericus, Alona rectangula and Bosmina longirostris. Lake area, lat i tude, macrophyte cov er age, pH, con duc tiv ity and hard ness were found to be the most de ter mi nant en vi ron men tal vari ables in the dis tri bu tion of cladoceran spe cies. This study revealed that al though the lakes show a clear sep a ra tion in en vi ron men tal pa ram e ters the com po si tion and dis tri bu tion of Cladoceran com mu ni ties dif fer only slightly across the in ves ti gated geo graph ical gra di ent.
Źródło:
Studia Quaternaria; 2012, 29; 45-52
1641-5558
2300-0384
Pojawia się w:
Studia Quaternaria
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Isotopic and Cladocera records of climate changes of Early Eemian at Besiekierz (Central Poland)
Autorzy:
Mirosław-Grabowska, J.
Niska, M.
Powiązania:
https://bibliotekanauki.pl/articles/2059552.pdf
Data publikacji:
2005
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
Central Poland
palaeoclimate
Eemian Interglacial
cladocera
stable isotopes
Opis:
Results of stable isotope, Cladocera and pollen analyses of lacustrine sediments from Besiekierz (Central Poland) are presented. The Besiekierz palaeolake is located about 25 km north of Łódź (Central Poland) at 130 m a.s.l. The 4 m thick deposits comprise silty sands and clayey silts, overlain by calcareous gyttja and organic silts and peat. Pollen analysis documents that these deposits accumulated during the Eemian Interglacial and the Early Vistulian. Based on the results of stable isotope analyses, nine isotopic horizons (Is) were defined and characterized, and these enabled reconstruction of both climatic and hydrological changes. A positive trend in δ18O values and constant values of δ 13 suggest gradual climatic warming, while constant values of δ 18O and δ 13C indicate stable conditions and/or a fast rate of sedimentation. The fluctuation of isotopic values in the upper part of the succession probably points to a shallowing of the lake due to sedimentary infill. The subfossil cladoceran fauna in the Besiekierz succession is represented by 11 solely littoral species belonging to 3 families. Four zones of Cladocera development were distinguished. The Besiekierz palaeolake was a shallow reservoir. The initial period of its existence probably saw its greatest depth. The Cladocera species present indicate the initial oligotrophic status of the lake and its subsequent increase in trophic status.We compare the results of the isotopic, cladoceran and published palynological analyses, to distinguish and explain the phases of evolution of the lake.
Źródło:
Geological Quarterly; 2005, 49, 1; 67--74
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Description of the subfossil head shield of Alona protzi Hartwig 1900 (Anomopoda, Chydoridae) and the environmental characteristics of its finding sites
Autorzy:
Bjerring, Rikke
Nykänen, Mirva
Sarmaja-Korjonen, Kaarina
Sinev, Artem
Jensen, Karina
Nevalainen, Liisa
Szeroczyńska, Krystyna
Zawisza, Edyta
Powiązania:
https://bibliotekanauki.pl/articles/2026063.pdf
Data publikacji:
2008
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
Subfossil Cladocera
Alona protzi
head shield
description
paleolimnology
Opis:
This pa per gives a de scrip tion of the head shield of Alona protzi, a rare spe cies of Cla do cera (wa ter fleas) whose separated head shield has not yet been de scribed in de tail. Sub fos sil head shields of A. protzi were found in sedi ment cores taken from lakes in Den mark, Swe den, Fin land, Es to nia and Po land. De spite the rar ity of the spe cies this sug gests a wide dis tri bu tion of A. protzi in north ern Europe. The ecol ogy of A. protzi is poorly known. The en vi ron mental spec -trum of the find ing sites was wide and ranged from rela tively nu tri ent poor clear wa ter lakes to eutrophic tur bid wa terlakes, in di cat ing that A. protzi is not nar rowly re stricted. Most of the lakes were, how ever, meso- eutrophic with neu tral to high pH, and with a rela tively low abun dance of sub merged mac ro phytes. How ever, we can not ex clude the pos si bility that A. protzi mainly lives in ground wa ter and is only oc ca sion ally trans ported into lakes.
Źródło:
Studia Quaternaria; 2008, 25; 47-53
1641-5558
2300-0384
Pojawia się w:
Studia Quaternaria
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Unusual stable morphotype of Acroperus harpae (Baird, 1834) from Lake Mývatn, Iceland (Cladocera: Anomopoda: Chydoridae) revealed by palaeolimnological studies
Autorzy:
Sinev, A.Y.
Zawisza, E.
Einarsson, A.
Powiązania:
https://bibliotekanauki.pl/articles/2027090.pdf
Data publikacji:
2012
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
Subfossil Cladocera
Acroperus harpae
new macrophototype description
paleolimnology
Opis:
A new un usual morphotype of Acroperus harpae (Baird, 1834) was found in Lake Mývatn and its neigh bour ing Lake Budlungaflói in Ice land. This form, A. harpae f. multidentata is char ac ter ized by a very large head keel and by 5–9 denticles on the posterovental an gle of the valves in stead of 1–3 com mon for A. harpae. The new form did not dif fer from typ i cal A. harpae in the mor phol ogy of the postabdomen, head pores or any ap pend ages. A study of Lake Mývatn sed i ments rev eled that this form ex isted in the lake for at least two thou sand years.
Źródło:
Studia Quaternaria; 2012, 29; 3-7
1641-5558
2300-0384
Pojawia się w:
Studia Quaternaria
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Palaeogeographical significance of the Eemian biogenic sediments at Bór site (Warta River valley, Central Poland)
Autorzy:
Petera-Zganiacz, J.
Borówka, R.K.
Forysiak, J.
Miotk-Szpiganowicz, G.
Pawłowski, D.
Powiązania:
https://bibliotekanauki.pl/articles/2060307.pdf
Data publikacji:
2013
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
gyttja
palynology
cladocera
geochemistry
Warta River valley deposits
Opis:
An investigated area is located in the middle reach of the WartaRiver valley. During drillings in the Bór site organic deposits such as detritous calcareous gyttja and calcareous detritous gyttja has been documented in a depth between 14,9 and 16,6 m. The organic deposits are covered by mineral, mostly sandy deposits. The accumulation took place in the small lake formed as an abandoned channel. Palynological analysis led to conclusion that biogenic accumulation began at the end of Wartanian and took place at least to the Eemian Interglacial optimum. Results of palynological, Cladocera and geochemical analysis inform about water level changes and increasing of trophy status of the reservoir. Presence of Mesozoic substratum very close to the palaeolake bottom influenced significantly chemical features of the organic deposits. As Eemian organic deposits are uncommon in the Warta River valley, the Bór site seems important for palaeogeographical reconstructions of the Warta River valley during Eemian Interglacial.
Źródło:
Geological Quarterly; 2013, 57, 4; 687--700
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
First records of Alona werestschagini sinev in Finland - subfossil remains from subarctic lakes
Autorzy:
Sarmaja- Korjonen, Kaarina
Sinev, Artem Yu.
Powiązania:
https://bibliotekanauki.pl/articles/2026066.pdf
Data publikacji:
2008
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
Chydorid Cladocera
Alona werestschagini Sinev
palaeolimnology
northern Finnish Lapland
Opis:
Sub fos sil re mains of a new spe cies of Cla do cera (wa ter fleas) of the fam ily Chy do ri dae in Fin land, Alona wer estschagini Si nev, were found in the sedi ments of four lakes above the treeline in north ern most Fin nish Lap land. The remains were found in sur face sedi ments of three lakes and in early Holo cene sedi ments of one lake where the spe cies was a pio neer which soon dis ap peared. The re mains of A. wer est schagini, ex cept the male postab do men, closely re sem ble Alona gut tata. In Eura sia A. wer est schagini has a wide but patchy dis tri bu tion in cold cli mates, sug gest ing that it is a post gla cial rel ict adapted to cold cli mate and oligo trophic lakes. Re cently it has been found also in Nor way and Kola Pen in sula. The early Holo cene finds in di cate that the spe cies spread to north ern most Fin land af ter the re treat of the Scan di na vian Ice Sheet. Since the spe cies has been found in lakes in very se vere con di tions it may be used as a palaeo lim no logi cal in di ca tor in sedi ment stud ies.
Źródło:
Studia Quaternaria; 2008, 25; 43-46
1641-5558
2300-0384
Pojawia się w:
Studia Quaternaria
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Late Holocene water-level changes in Lake Iso Lehmälampi, Southern Finland, reflected in subfossil Cladocerans and Chironomids
Autorzy:
Nevalainen, Liisa
Luoto, Tomi P.
Sarmaja- Korjonen, Kaarina
Powiązania:
https://bibliotekanauki.pl/articles/2026067.pdf
Data publikacji:
2008
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
Chironomidae
Cladocera
climate
Finland
late Holocene
lake-level changes
Opis:
Anal y ses of subfossil cladocerans (Crustacea: Cladocera) and chi rono mids (Diptera: Chironomidae) were ap plied to ex am ine wa ter-level changes in a small and oligotrophic lake in south ern Fin land over the past 2000 years. Ma jor changes in the in ver te brate com mu ni ties oc curred ca. 400 AD on wards when the lit to ral cladoceran Alonella nana started to re place the plank tonic Eubosmina as the dom i nant spe cies and chi rono mids Psectrocladius sordidellus group and Zalutschia zalutschicola in creased. These changes were most likely due to a de creas ing wa ter level and an en larg ing pro por tion of the lit to ral area, pro vid ing suit able veg e ta tive hab i tats, e.g. aquatic bryophytes (mosses), for these taxa. The low er ing wa ter level reached its min i mum just be fore the Me di eval Warm Pe riod, ca. 800–1000 AD, af ter which the lake level rose again and re mained high un til mod ern times. A prom i nent change in the chi rono mid as - sem blages oc curred dur ing the 20th cen tury when Ablabesmyia monilis and Chironomus anthracinus type in creased, pre sum ably due to changes in wa ter chem is try, caused by anthropogenic load of pol lut ants.
Źródło:
Studia Quaternaria; 2008, 25; 33-42
1641-5558
2300-0384
Pojawia się w:
Studia Quaternaria
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
The significance of subfossil Cladocera in stratigraphy of Late Glacial and Holocene
Autorzy:
Szeroczyńska, Krystyna
Powiązania:
https://bibliotekanauki.pl/articles/2027068.pdf
Data publikacji:
2006
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
stratigraphy
“ecostratigraphy” – biostratigraphy
climate
lakes
lacustrine sediments
subfossil Cladocera
Opis:
This pa per pres ents dis cus sion on the re sults of sub fos sil Cla do cera analy ses from five lakes in Po land (Przedni Staw Lake, Per es pilno Lake, Gooeci¹¿ Lake, Imio³ki- fossil lake and Os trow ite Lake). The Cla do cera are rep re sented in sediments by re mains of plank tonic (Bos mini dae, Daph ni dae) and lit to ral (Chy do ri dae) forms. Cla do ceran as sem blage phases (“ecos tra tigra phy”) were de ter mined on the ba sis of changes in domi nance of in di ca tor spe cies and past ecologi cal con di tions were re con structed. The re sults are be ing dis cussed from the view point of cli mate change and anthro po genic ac tiv ity and their role in the lake evo lu tion. Moreo ver, an at tempt to use the cla do ceran phases for stra tigraphic di vi sion of the Late Gla cial and Holo cene was made. Dur ing the Bøl ling/Al lerød in ter sta dial, dis tin guished on the ba sis of pol len analy sis, Cla do cera in di cated short phase of bad con di tion (dry or cold?), proba bly as the Old Dryas cli mate re sults. The be gin ning of Holo cene is char ac ter ized, in moun tain and low land lakes, by high in -crease in the number of spe cies and speci mens of Cla do cera. This de scribed clear warm ing and marked the bound ary Late Gla cial/Holo cene. It was in di cated that the “ecos tra tigra phy” based on Cla do cera can be use ful for cli ma to stratigra phy, if cli mate was the ma jor fac tor con trol ling the de vel op ment of fresh wa ter lakes.
Źródło:
Studia Quaternaria; 2006, 23; 37-45
1641-5558
2300-0384
Pojawia się w:
Studia Quaternaria
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Warunki ekologiczne rozwoju późnovistuliańskiego zbiornika Koźmin Las w świetle analizy Cladocera
Ecological conditions of the small Late Vistulian pond of Koźmin Las site in the light of Cladocera analysis
Autorzy:
Pawłowski, Dominik
Powiązania:
https://bibliotekanauki.pl/articles/578365.pdf
Data publikacji:
2014
Wydawca:
Łódzkie Towarzystwo Naukowe
Tematy:
dolina Warty
subfosylne szczątki Cladocera
młodszy dryas
aktywność fluwialna
powodzie
klimat
Warta River valley
subfossil Cladocera
Younger Dryas
fluvial activity
floods
climate
Opis:
Rezultaty analizy subfosylnych szczątków wioślarek (Cladocera) z profilu osadów organicznych stanowiska Koźmin Las (dolina Warty, Polska Środkowa) pozwoliły przedstawić rekonstrukcję rozwoju opisywanego zbiornika i odnieść je do ak-tywności fluwialnej Warty, szczególnie w okresie młodszego dryasu, pomiędzy 12 900 i 11 600 cal BP. Wyróżniono dwie fazy rozwoju zbiornika. Stwierdzono, że był to płytki zbiornik, o niestabilnych warunkach hydrologicznych. Prawdopodobną przyczyną fluktuacji był zmienny poziom wód gruntowych, powierzchniowych i rzecznych w dolinie Warty. Zmiany we frekwencji Cladocera skorelowano z aktywnością fluwialną rzeki oraz, w szerszym ujęciu, z warunkami klimatycznymi panującymi w młodszym dryasie.
The sediments from small pond infillings located in the Warta River valley in central Poland was studied by Cladocera analysis in order to examine the response of aquatic ecosystems to environmental changes in the Younger Dryas. Lithological and geochemical records were also used to reconstruct fluvial activity of the Warta River. In the Koźmin Las site development, between ca. 12.900 and 11.600 cal BP, prevailed variable hydrological conditions. Cladocera analysis indicates the presence of shallow pool and partly telmatic conditions. The local processes, such as the influence of the Warta River, habitat modification, macrophyte presence, and eutrophication, were important, but these forces were not only major factors that affect the biota diversity in the Younger Dryas. The observation of changes in the composition and concentration of aquatic communities in the studied pool indicates that the changes also occurred in response to climate changes.
Źródło:
Acta Geographica Lodziensia; 2014, 102; 65-70
0065-1249
Pojawia się w:
Acta Geographica Lodziensia
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
New records of Cercopagis pengoi (Ostroumov 1891) in the Southern Baltic
Autorzy:
Olszewska, A.
Powiązania:
https://bibliotekanauki.pl/articles/48054.pdf
Data publikacji:
2006
Wydawca:
Polska Akademia Nauk. Instytut Oceanologii PAN
Tematy:
invasive species
new record
Baltic Sea
Crustacea
Cladocera
Cercopagis pengoi
Opis:
New records of Cercopagis pengoi (Cladocera, Crustacea) are reported for the first time from the central and western part of the Polish zone of the Baltic Sea.
Źródło:
Oceanologia; 2006, 48, 2
0078-3234
Pojawia się w:
Oceanologia
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
500 years of ecological changes recorded in subfossil Cladocera in a high-altitude, tropical lake Lago de la Luna, central Mexico
Autorzy:
Zawisza, E.
Caballero, M.
Ruiz-Fernandez, C.
Powiązania:
https://bibliotekanauki.pl/articles/2027080.pdf
Data publikacji:
2012
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
subfossil Cladocera
crater Nevado de Toluca
lake sed i ment
Opis:
We pres ent the last 500 years of his tory of a high-al ti tude trop i cal lake Lago de la Luna lo cated at Nevado de Toluca crater, Cen tral Mex ico, based on subfossil Cladocera anal y sis. Through the stud ied sed i men tary se quence only five Cladocera spe cies were pres ent. Cladocera com mu nity was dom i nated by lit to ral spe cies (4) and among them one (Ilyocryptus nevadensis) is en demic. The de tailed anal y sis of the sed i ments (ev ery 1 cm) al lowed us to track con tem - po rary cli ma tic and anthropogenic changes. Our re sults showed that Lago de la Luna is a very sen si tive eco sys tem and has strong re sponse to cli ma tic changes. The most re mark able change in the Cladocera com mu nity was ob served between 1683–1780 yr, which was well cor re lated with the Lit tle Ice Age. PCA re sults im plied that mod ern state of the lake Lago de la Luna is very sim i lar to one 400–500 yr ago. Only one pe riod was iden ti fied when hu man im pact was of im por tance. This pe riod seemed to cor re late with changes in the lake eco sys tem due to fish in tro duc tion in the 1950s.
Źródło:
Studia Quaternaria; 2012, 29; 23-29
1641-5558
2300-0384
Pojawia się w:
Studia Quaternaria
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Subfossil Chydorid taxa and assemblages from lake sediments in Poland and Finland with special reference to climate
Autorzy:
Sarmaja-Korjonen, Kaarina
Szeroczyńska, Krystyna
Gąsiorowski, Michał
Powiązania:
https://bibliotekanauki.pl/articles/2027446.pdf
Data publikacji:
2003
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
subfossil Cladocera
chydorids
Finnish lakes
Polish lakes
climate
redundancy analysis
Opis:
In this study we compared chydorid cladoceran (Chydoridae) taxa and assemblages from sediments of 6 Polish and 6 sq Finnish lakes and investigated if the difference in climate of these two countries can be detected in the cladoceran data. The data were analysed in terms of I) average relative proportions of chydorid taxa during the history of each lake and by 2) redundancy analysis (RDA) to explain the present effect of environmental variables (altitude, area, maximum depth, mean annual temperature, mean summer temperature and length of the growing season) on species abundances. The redundancy analysis (RDA) enabled us to distinguish groups of taxa I) with a high thermal preference 2) associated with small, cold-water lakes and 3) associated with shallow lakes. There are clear differences in the dominant chydorid taxa and in the relative proportions of many other chydorid taxa between the two countries since the end of the last glaciation. Although these differences first of all appear to reflect the climatic difference, the influence of many other environmental factors, controlling the living conditions of particular chydorids have been raised and considered. Further studies with larger data are needed before the role of climate can be reliably separated from other elements of environment.
Źródło:
Studia Quaternaria; 2003; 25-34
1641-5558
2300-0384
Pojawia się w:
Studia Quaternaria
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Wioslarki [Cladocera] niektorych okresowych stawow lesnych w okolicach Poddebic, wojewodztwo lodzkie
Cladocera of some periodical forest ponds near Poddebice, Lodz province
Autorzy:
Kaminski, K.Z.
Powiązania:
https://bibliotekanauki.pl/articles/45333.pdf
Data publikacji:
2009
Wydawca:
Instytut Badawczy Leśnictwa
Tematy:
lesnictwo
okolice Poddebic
oczka wodne srodlesne
plankton
wioslarki
Cladocera
sklad gatunkowy
Źródło:
Leśne Prace Badawcze; 2009, 70, 3; 287-292
1732-9442
2082-8926
Pojawia się w:
Leśne Prace Badawcze
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Late-Glacial cladoceran succession in three lakes of the Chełm Hills Region ( Łęczna-Włodawa Lake Group, SE Poland)
Autorzy:
Suchora, M.
Powiązania:
https://bibliotekanauki.pl/articles/2027077.pdf
Data publikacji:
2012
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
Late-Gla cial
subfossil Cladocera
Łęczna-Włodawa Lake Group
Chełm hills
Opis:
High res o lu tion stud ies on subfossil Cladocera from three closely lo cated lakes of the Che³m Hills Re gion – Lake S³one, Syczyñskie, and Pniówno, ev i denced a strong zoo plank ton re sponse to the well-known cli ma tic changes of the Late-Gla cial and early-Ho lo cene. The gen eral changes in the cladoceran com mu nity struc ture re sem ble those de - scribed from other Pol ish and Eu ro pean lakes. Cer tain im por tant dif fer ences were iden ti fied, how ever, which can be at trib uted to the pe cu liar ity of the en vi ron men tal con di tions of the re gion, re gard ing: the deep char ac ter of the lakes stud ied al ready in the ini tial phase of their de vel op ment (Older Dryas), an in ten sive eutrophication pro cess in duced by the Alleröd cli mate warm ing with a pe ri od i cal low er ing of the trophic sta tus, and the char ac ter of the Youn ger Dryas cool ing less se vere than in some other re gions. The chro nol ogy of the palaeoenvironmental changes iden ti fied by means of subfossil Cladocera anal y sis was based on the re sults of palaeobotanical anal y sis, and con firmed by ra diocar bon dat ing avail able for two pro files. Tak ing ad van tage of the close lo ca tion of the study sites, their morphometric and geo log i cal sim i lar i ties, and the high res o lu tion of sam pling, an at tempt was made to use cladoceran suc ces sion in or der to es tab lish the strati graphic di vi sion for Lake Pniówno, lack ing palynological and ra dio car bon data.
Źródło:
Studia Quaternaria; 2012, 29; 9-21
1641-5558
2300-0384
Pojawia się w:
Studia Quaternaria
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Two climatic oscillations during the eemian interglacial : preliminary results of multi-proxy researches of palaeolake at solniki, Ne Poland
Autorzy:
Kupryjanowicz, M.
Ciszek, D.
Morosław-Grabowska, J.
Marciniak, B.
Niska, M.
Powiązania:
https://bibliotekanauki.pl/articles/1186083.pdf
Data publikacji:
2005
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
pyłek
okrzemka
Cladocera
izotopy stabilne
podatność magnetyczna
zmiany klimatu
interglacjał eemski
północno-wschodnia Polska
pollen
diatom
cladocera
stable isotopes
magnetic susceptibility
climate changes
Eemian Interglacial
NE Poland
Opis:
W Solnikach na Wysoczyźnie Białostockiej (północno-wschodnia Polska) odkryto serię osadów jeziornych reprezentujących interglacjał eemski i wczesny vistulian. Wstępne wyniki badań interdyscyplinarnych (analiza pyłkowa, okrzemkowa i Cladocera, pomiary podatności magnetycznej osadów oraz zawartości izotopów stabilnych tlenu i węgla) wykorzystano do zilustrowania zmian klimatu podczas interglacjału eemskiego. Udokumentowano dwie gwałtowne oscylacje klimatu - pierwsza z ciepłym i bardzo wilgotnym klimatem (?opady) miała miejsce w środkowej części poziomu pyłkowego E5 Carpinus, druga z klimatem suchym i bardzo zimnym - w środkowej części poziomu E7 Pinus.
Źródło:
Polish Geological Institute Special Papers; 2005, 16; 53--57
1507-9791
Pojawia się w:
Polish Geological Institute Special Papers
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Spatio-temporal distribution, abundance and diversity of zooplankton community structure in River Shasha, Southwestern Nigeria
Autorzy:
Adedeji, A. A.
Adesakin, T. A.
Oni, T. M.
Oyebamiji, S. P.
Olowogboyega, V. T.
Powiązania:
https://bibliotekanauki.pl/articles/1076780.pdf
Data publikacji:
2019
Wydawca:
Przedsiębiorstwo Wydawnictw Naukowych Darwin / Scientific Publishing House DARWIN
Tematy:
Arthropoda
Cladocera
Copepoda
Ostracoda
Protozoa
Rotifera
Zooplankton
environmental condition and monitoring
eutrophication
Opis:
This study was carried-out to investigate the abundance and diversity of zooplankton in River Shasha, Southwest Nigeria. The zooplankton community constitutes an important component in the faunal composition of the water body. Samples were collected bi-monthly between February 2006 to February 2008, with a mind of capturing various seasons in the period of study, at two sampling stations (Ipetumodu and Edun-abon) established along River Shasha. A total number of 54 zooplankton species were identified, comprising of five classes, namely Rotifera (29 species), Ostracoda (8 species), Arthropoda (5 species), Copepoda (5 species), Protozoa (4 species) and Cladocera (3 species). The most abundant species were Brachionus, Lecane and Keratella recorded the highest distribution among the zooplankton observed during the sampling period. Among the Rotifers, Branchions patulus and Filina opoliensis were found abundant. Holopedium amazonicum and Scapholebris armata were predominant among the Cladoceras. Among the Copepods the dominant species was Ectocyclops phaleratus and Hemicypris ovate and Cypris subglobosa among Ostracoda. Among the Protozoa, Diffugia sp and Vorticella sp were observed. Ceratopogonid sp. was most dominant among Arthropoda. The density of zooplankton population was maximum during dry season (158702 Org/L) and minimum (12402 Org/L) during rainy season due to the different environmental conditions of the water bodies. The overall mean abundance of zooplankton population was in the following order: Rotifera > Protozoan > Arthropoda > Copepoda > Cladocera >Ostracoda. The few species of Zooplankton identified in River Shasha may reflect the moderate level of limit nutrient and there is need for regular monitoring of the waterbody to avoid the excess input of nutrients from domestic and agricultural waste that could lead to eutrophication.
Źródło:
World News of Natural Sciences; 2019, 24; 299-321
2543-5426
Pojawia się w:
World News of Natural Sciences
Dostawca treści:
Biblioteka Nauki
Artykuł
Wyświetlanie 1-25 z 39

Ta witryna wykorzystuje pliki cookies do przechowywania informacji na Twoim komputerze. Pliki cookies stosujemy w celu świadczenia usług na najwyższym poziomie, w tym w sposób dostosowany do indywidualnych potrzeb. Korzystanie z witryny bez zmiany ustawień dotyczących cookies oznacza, że będą one zamieszczane w Twoim komputerze. W każdym momencie możesz dokonać zmiany ustawień dotyczących cookies