Comparative oxygen and carbon isotopic records of Miocene and recent lacustrine unionid bivalves from Poland

Błażejowski, B.; Racki, G.; Gieszcz, P.; Małkowski, K.; Kin, A.; Krzywiecka, K.

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Tytuł artykułu

Comparative oxygen and carbon isotopic records of Miocene and recent lacustrine unionid bivalves from Poland

Autorzy

Błażejowski B. , Racki G. , Gieszcz P. , Małkowski K. , Kin A. , Krzywiecka K.

Treść / Zawartość

Pełne teksty:

Blazejowski_B_Comprative_Geol. Quart._Vol.57_No 1_2013.pdf

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Abstrakty

The δ¹³C and δ¹⁸O isotope data from both fossil (Miocene) and modern freshwater bivalve shells of family Unionidae from Poland (species Margaritifera flabellatiformis and Unio tumidus, respectively) show a similar, truncated sinusoidal pattern.. The isotopic profiles of the whole shell are visibly marked by three growth stages, linked with a progressive loss of environmental record because of declining intra-annual biocarbonate accretion rate. The juvenile and gerontic phases exhibit generally more positive and stable (plateau) isotopic pattern than the mid-age stage. An increasing δ¹³C trend is typical for the final life stage, likely influenced by nutrient overloading, reversing the tendency towards δ¹³C depletion throughout the individual’s life induced by metabolic processes. Due to the progressive loss of environmental signals through ontogeny, these initial and final isotopic profile segments probably correspond to, respectively, an instant signature of the first season growth, and a multiyear value set of summer maxima during geriatric stage. Vague seasonal cyclic record is the striking feature of the mid-age δ¹⁸O and δ¹³C profile slices. In case of low-amplitude δ¹⁸O curve, this is probably promoted by a sensitivity of the lake ecosystem to many dynamic intra-annual factors affecting water budget balance. This consistent signature mode seems to be typical for lake-dwelling unionid shells at least since Miocene from different climatic zones, as confirmed by coeval lacustrine low-latitude mussels from Amazonia. Thus, this isotope record is relevant to obtain information on the habitat and life cycle of the fossil freshwater bivalves, as well as could help understand modern environmental change.

Słowa kluczowe

sclerochronology stable isotopes fresh water Miocene and recent Unionidae Bełchatów Gil Wielki Lake.

Wydawca

Państwowy Instytut Geologiczny - Państwowy Instytut Badawczy

Czasopismo

Geological Quarterly

Rocznik

2013

Tom

Vol. 57, No. 1

Strony

113–--122

Opis fizyczny

Bibliogr. 64 poz., rys., wykr.

Twórcy

autor

Błażejowski B.

bblazej@twarda.pan.pl

Institute of Paleobiology, Polish Academy of Sciences,Twarda 51/55, 00-818 Warszawa, Poland

autor

Racki G.

Institute of Paleobiology, Polish Academy of Sciences,Twarda 51/55, 00-818 Warszawa, Poland
Faculty of Earth Sciences, University of Silesia, Bedzinska 60, 41-200 Sosnowiec, Poland

autor

Gieszcz P.

Association of Polish Climatologists, Krakowskie Przedmiescie 30, 00-927 Warszawa, Poland

autor

Małkowski K.

Institute of Paleobiology, Polish Academy of Sciences,Twarda 51/55, 00-818 Warszawa, Poland

autor

Kin A.

PHACOPS Association of Friends of Geosciences, Łódz, Poland

autor

Krzywiecka K.

Institute of Paleobiology, Polish Academy of Sciences,Twarda 51/55, 00-818 Warszawa, Poland

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