2024
Reliability of the Strontium Isotope Stratigraphy approach in marginal seas: Insights from the Miocene Paratethys
HOLCOVÁ, Katarina; Filip SCHEINER; Lukáš ACKERMAN; Rastislav MILOVSKY; Natália HUDÁČKOVÁ et. al.Základní údaje
Originální název
Reliability of the Strontium Isotope Stratigraphy approach in marginal seas: Insights from the Miocene Paratethys
Autoři
HOLCOVÁ, Katarina (203 Česká republika); Filip SCHEINER (203 Česká republika); Lukáš ACKERMAN (203 Česká republika); Rastislav MILOVSKY (703 Slovensko); Natália HUDÁČKOVÁ (703 Slovensko); Šárka HLADILOVÁ (203 Česká republika, domácí); Slavomír NEHYBA (203 Česká republika, domácí) a Danuta PERYT (616 Polsko)
Vydání
PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY, Amsterdam, Elsevier, 2024, 0031-0182
Další údaje
Jazyk
angličtina
Typ výsledku
Článek v odborném periodiku
Obor
10505 Geology
Stát vydavatele
Nizozemské království
Utajení
není předmětem státního či obchodního tajemství
Odkazy
Impakt faktor
Impact factor: 2.700
Kód RIV
RIV/00216224:14310/24:00137669
Organizační jednotka
Přírodovědecká fakulta
UT WoS
001349975300001
EID Scopus
2-s2.0-85207746914
Klíčová slova anglicky
Integrated stratigraphy; Neogene; Foraminifera; Molluscs; Local 87Sr/ 86Sr curve
Štítky
Příznaky
Mezinárodní význam, Recenzováno
Změněno: 30. 1. 2025 11:26, prof. RNDr. Slavomír Nehyba, Dr.
Anotace
V originále
The robustness of the Strontium Isotope Stratigraphy (SIS) as a chemostratigraphic tool was tested in the Miocene epicontinental Central Paratethys using new 87Sr/86Sr results obtained for 129 foraminiferal tests and various marine invertebrate shells that were converted to numerical ages using the global 87Sr/86Sr curve for the Phanerozoic open oceans. These ages were compared with those expected from either magnetostratigraphic, radiometric or biostratigraphic studies applied to selected sections from different Central Paratethys basins. The results from different basins showed variations in 87Sr/86Sr values for specific time intervals; therefore, it is not possible to construct a unique 87Sr/86Sr curve for the Central Paratethys region that can be used for chemostratigraphic purposes. The 87Sr/86Sr signal in semi-enclosed basins tends to reflect the lithology of the source areas. For example, marine basins surrounded by areas of Mesozoic carbonate rock cover are associated with a reduced 87Sr/86Sr signal compared to the global 87Sr/86Sr signal primarily due to the drainage of these Mesozoic carbonate rocks and transfer of their specific Sr signal. By contrast, areas affected by continental runoff from crystalline terrains in combination with limited connection to surrounding marine domains were found to show an elevated 87Sr/86Sr signal compared to the global one. Additionally, it was demonstrated that infaunal, eutrophic and hypoxic species (foraminiferal genus Uvigerina and molluscs) show a shift towards a relatively higher 87Sr/86Sr signal. Therefore, our data show that variable 87Sr/86Sr patterns occur in semi-enclosed domains, primarily reflecting local settings and thus hampering reliable SIS ages. In particular, the best SIS results in the studied Paratethys area occur during periods of maximum marine connectivity, when other (biostratigraphic) methods can be applied, and then become unreliable as connectivity diminishes.
Návaznosti
MUNI/A/1426/2023, interní kód MU |
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