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    Wyświetlanie 1-5 z 5
    Tytuł:
    Znaczenie analizy subfosylnych makroszczątków roślinnych i stopnia rozkładu torfu dla rekonstrukcji paleośrodowiska
    The importance of subfossil plant remnants and peat decomposition degree analyses for palaeoenvironment reconstruction
    Autorzy:
    Drzymulska, Danuta
    Powiązania:
    https://bibliotekanauki.pl/articles/1199572.pdf
    Data publikacji:
    2003
    Wydawca:
    Polskie Towarzystwo Przyrodników im. Kopernika
    Opis:
    In this article an attempt was made to explain some aspects of palaeoenvironmental studies. Analyses of plant remnants forming peat are the first described problem. There are two kinds of these analyses: carpological method (recognizing of seeds and fruits) and analysis of vegetative tissues. Their connection with description of the phytosociological rules of plant communities, allows to restore successive sequences of local vegetation. Second characterized problem is decomposition degree of peat. That parametr means proportional relation between humus and full peatmass in a peat sample and it is connected with the peatbog surface humidity. Therefore, knowledge of its value supplies information about past humidity and, on ombrotrophic bogs, also about altitude of precipitations (climatic factor).
    Źródło:
    Kosmos; 2003, 52, 2-3; 299-306
    0023-4249
    Pojawia się w:
    Kosmos
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Development of the Kładkowe Bagno peat-bog in the Late Glacial and Holocene: diversified history of two deposit basins studied with use of macrofossil remains analysis
    Autorzy:
    Drzymulska, Danuta
    Powiązania:
    https://bibliotekanauki.pl/articles/2026058.pdf
    Data publikacji:
    2008
    Wydawca:
    Polska Akademia Nauk. Czytelnia Czasopism PAN
    Tematy:
    Late Glacial
    Holocene
    Puszcza Knyszyńska Forest
    peat
    analysis of plant remains
    subfossil vegetation
    Opis:
    This pa per pres ents re sults of in ves ti ga tion on peat and la cus trine sedi ments from the K³ad kowe Bagno peat- bog located in the Puszcza Knyszyñska For est. Us ing analy sis of plant re mains from sedi ment sam ples, vege ta tive and gen era tive finds were iden ti fied which al lowed de scrib ing peat units. Bas ing on these re sults, re con struc tion of sub fos silvege ta tion and pa laeoen vi ron men tal changes in the mire was made. Al to gether 4 sub as so cia tions of Sphag ne tum mag -el lan ici were de scribed, which de liv ered in for ma tion about hu mid ity of the mire sur face dur ing peat form ing pro -cesses. Stages of de posit de vel op ment were dated by ra dio car bon method. Ac cu mu la tion of the old est sedi ments in thesouth ern ba sin took place in the Late Gla cial. Peat of the north ern ba sin started to ac cu mu late in the At lan tic pe riod.The both parts of the mire ag gre gated proba bly 400 years ago.
    Źródło:
    Studia Quaternaria; 2008, 25; 23-32
    1641-5558
    2300-0384
    Pojawia się w:
    Studia Quaternaria
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Eemian and Early Yi stu lian vegetation at Michałowo (NE Poland)
    Autorzy:
    Kupryjanowicz, Mirosława
    Drzymulska, Danuta
    Powiązania:
    https://bibliotekanauki.pl/articles/2027415.pdf
    Data publikacji:
    2002
    Wydawca:
    Polska Akademia Nauk. Czytelnia Czasopism PAN
    Tematy:
    Eemian Interglacial
    Vistulian
    pollen analysis
    pollen succession
    macrofossil analysis
    Opis:
    This paper presents the results of palaeobotanical studies (pollen and plant macrofossil analyses) of the sediments from sq the profile Michałowo P-3 (Gródek-Michałowo Depression, NE Poland). At this profile the second bed of peat under Holocene peat and the layer of silts and sands was discovered. The pollen succession indicates that they were deposited, with some gaps, from the beginning of Eernian Interglacial to Early Vistulian. The local pollen zones, distinguished in the pollen diagram, correlate with the regional pollen stratigraphy of the Eemian Interglacial, but the pollen record of hornbeam (ES R PAZ) and spruce (E6 R PAZ) regional zones is absent in Michałowo. In the middle part of the Michałowo pine zone (Mi-5 Pinus L PAZ), a cool oscillation of climate is marked by an opening of forests and development of herb plant communities.
    Źródło:
    Studia Quaternaria; 2002; 19-26
    1641-5558
    2300-0384
    Pojawia się w:
    Studia Quaternaria
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Late Glacial and Holocene vegetation changes in the WigryNational Park, NE Poland – new pollen data from three small dystrophic lakes
    Autorzy:
    Fiłoc, Magdalena
    Kupryjanowicz, Mirosława
    Drzymulska, Danuta
    Powiązania:
    https://bibliotekanauki.pl/articles/2027097.pdf
    Data publikacji:
    2014
    Wydawca:
    Polska Akademia Nauk. Czytelnia Czasopism PAN
    Tematy:
    postglacial succession of vegetation
    palaeoecological recon struction
    climate changes
    Late Glacial
    Ho lo cene
    pol len anal y sis
    Wigry Na tional Park
    NE Po land
    Opis:
    The main phases of the Late Gla cial and Ho lo cene de vel op ment of veg e ta tion in the Wigry Na tional Park were re con - structed based on the pol len anal y sis of sed i ments from three small dystrophic lakes (Lake Suchar Wielki, Lake Suchar II and Lake OElepe). At the cur rent stage of re search, the age of the stud ied de pos its was de ter mined by AMS radio car bon dat ing of few sam ples only. This meant that the chro nol ogy of the in ves ti gated pro files had to be es ti mated also in di rectly us ing their palynological cor re la tion with a ra dio met ri cally well-dated pro file from Lake Wigry. The ob tained pol len data con firmed the pic ture of the postglacial veg e ta tion changes of the Wigry Na tional Park, which was based on ear lier stud ies of Lake Wigry. Fur ther more, it doc u mented the ex is tence, mainly in the Preboreal and At - lan tic chronozones, of tem po rary changes in veg e ta tion, which might be a re ac tion to a short-lived cold fluc tu a tions of cli mate.
    Źródło:
    Studia Quaternaria; 2014, 31; 5-16
    1641-5558
    2300-0384
    Pojawia się w:
    Studia Quaternaria
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Palaeobotanical record of the Eemian Interglacial succession at the Jagodne site (Garwolin Plain, central Poland)
    Autorzy:
    Bober, Aleksandra
    Brzozowicz, Dorota
    Drzymulska, Danuta
    Żarski, Marcin
    Suchora, Magdalena
    Powiązania:
    https://bibliotekanauki.pl/articles/2059599.pdf
    Data publikacji:
    2021
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    Eemian Interglacial
    MIS-5e
    Garwolin Plain
    central Poland
    palynology
    plant macrofossils
    Opis:
    Our high-resolution data of pollen and macrofossils from 2 cores taken from the Jagodne site (Garwolin Plain) reveals a pollen succession covering the final part of the Late Saalian (Marine Isotope Stage MIS 6) and embracing the Eemian (MIS 5e). The results correspond to Regional Pollen Assemblage Zones (RPAZ). The hornbeam phase (E5 RPAZ) has been subdivided into subzones and compared to the corresponding division of the key profile of the Garwolin Plain, Kozłów K2-19. The comparison revealed a considerable sedimentary hiatus in the E5 RPAZ at Jagodne. This is attributed to significant palaeohydrological changes occurring widely in this zone, and also seen at other Eemian sites in Poland. Another specific feature of the Jagodne site is the early, rapid terrestrialisation of the palaeolake and its transformation into a raised bog, which occurred already at the end of the hornbeam phase. The Sphagnum dominated peatbog developed for a long time as evidenced by a thick peat layer covering also the Early Vistulian. Both pollen and plant macrofossil data correspond well to observed lithological boundaries, providing a consistent record of palaeoenvironmental and palaeoclimate changes. The results obtained contribute to knowledge of palaeoenvironmental changes and palaeoclimate interpretation of that area.
    Źródło:
    Geological Quarterly; 2021, 65, 2; 65: 34
    1641-7291
    Pojawia się w:
    Geological Quarterly
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
      Wyświetlanie 1-5 z 5

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