Lithology and chemical composition of a Neoholocene palaeochannel infill within the Białka River valley, Kraków-Częstochowa Upland

Artykuł - publikacja recenzowana


Tytuł
Lithology and chemical composition of a Neoholocene palaeochannel infill within the Białka River valley, Kraków-Częstochowa Upland
Odpowiedzialność
Piotr Cybul, Daniel Okupny
Twórcy
Sumy twórców
2 autorów
Punktacja publikacji
Osoba Dysc. Pc k m P U Pu Opis
0000-0002-8836-6044 6.7 70 1 2 49,50 0,7071 49,4970 Art.
Gł. język publikacji
Angielski (English)
Data publikacji
2021
Objętość
2 (arkuszy wydawniczych), 14 (stron).
Identyfikator DOI
10.26485/AGL/2021/111/8
Adres URL
http://czasopisma.ltn.lodz.pl/index.php/Acta-Geographica-Lodziensia/article/view/1587/1437
Uwaga ogólna
Czasopismo wydawane jest na zasadach Open Access. Wszystkie artykuły udostępniane są na licencji Creative Commons: Uznanie autorstwa - Użycie niekomercyjne - Bez utworów zależnych (CC BY-NC-ND).
Uwaga ogólna
Opublikowano: 2021-12-23.
Finansowanie
Acta Geographica Lodziensia - zadanie finansowane ze środków Ministra Nauki i Szkolnictwa Wyższego w ramach umowy 704/P-DUN/2019 przeznaczonych na działalność upowszechniającą naukę.
Cechy publikacji
  • Oryginalny artykuł naukowy
  • OpenAccess
Dane OpenAccess
CC_BY_NC_ND - Licencja,
FINAL_PUBLISHED - Wersja tekstu,
OTHER - Sposób publikacji,
AT_PUBLICATION - Moment udostępnienia,
[brak danych] - Data udostępnienia
Słowa kluczowe
Czasopismo
Acta Geographica Lodziensia
( ISSN 0065-1249 eISSN 2451-0319 )
Kraj wydania: Polska
Zeszyt: t. 111
Strony: 109-122
Pobierz opis jako:
BibTeX, RIS
Data zgłoszenia do bazy Publi
2021-12-18
PBN
Wyświetl
WorkId
29083

Abstrakt

en

Mires are common in the landscape of the Kraków-Częstochowa Upland, but they are rarely explored by Earth scientists. In addition to numerous morphological depressions filled with biogenic sediments, mires also occur within river valley, usually upstream from gaps. The intensification of marsh formation within the Białka River valley (left-side tributary of Krztynia, upper Pilica catchment) may have been influenced by the occurrence of poorly permeable, fluvial silty sands in the bedrock. Infilling of the studied depression at Młyny was accomplished via fluvial sedimentation characterised by local aggradation interrupted by carbonate precipitation, and sedentation of autochthonous organic matter. The former sediment type is represented mostly by mineral-organic aggraded silt with a dominant fine fraction, occurring mostly in the basal part of the studied core, and sand fraction in the top interval of the core, superjacent to calcareous-clay gyttja. Ash content reaches up to 87% and Fe concentrations are periodically elevated (30–48 mg/g). Calcium carbonate (CaCO3) also occurs in the studied oxbow mire deposit, exceeding 40% in some intervals, which indicates that a more important part was played by groundwaters in the water balance of the Białka valley. This periods were periodically interrupted due to higher flooding activity and recorded by mineral sediments characterised by specific granulometric composition, and an elevated percentage of organic matter deposited as rhythmists. Elevated concentrations of trace elements noted in a horizon dated at 1885±105 BP by means of radiocarbon dating may point to human impact on the environment due to the adaptation of economy to local conditions. The geochemical record of human activity is corroborated by archaeological data from various parts of the Białka valley catchment. The reason for the concentration of trace elements being highest in the top interval of the studied core is the intense economic development of Silesia-Kraków region, and the associated deforestation, mining and metallurgy.

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