Response of benthic foraminiferal communities to changes in
productivity and watermass conditions in the epicontinental
Paratethys during the middle Miocene

J 2019

Response of benthic foraminiferal communities to changes in productivity and watermass conditions in the epicontinental Paratethys during the middle Miocene

SCHEINER, Filip, Katarina HOLCOVÁ, Rastislav MILOVSKÝ, Nela DOLÁKOVÁ, Jana RIGOVÁ et. al.

Základní údaje

Originální název

Response of benthic foraminiferal communities to changes in productivity and watermass conditions in the epicontinental Paratethys during the middle Miocene

Autoři

SCHEINER, Filip (203 Česká republika), Katarina HOLCOVÁ (203 Česká republika), Rastislav MILOVSKÝ (703 Slovensko), Nela DOLÁKOVÁ (203 Česká republika, garant, domácí) a Jana RIGOVÁ (703 Slovensko)

Vydání

Marine Micropaleontology, ELSEVIER, RADARWEG 29, 1043 NX AMSTERDAM, NETHERLANDS, 2019, 0377-8398

Další údaje

Jazyk

angličtina

Typ výsledku

Článek v odborném periodiku

Obor

10506 Paleontology

Stát vydavatele

Nizozemské království

Utajení

není předmětem státního či obchodního tajemství

Odkazy

URL

Impakt faktor

Impact factor: 2.207

Kód RIV

RIV/00216224:14310/19:00112877

Organizační jednotka

Přírodovědecká fakulta

DOI

http://dx.doi.org/10.1016/j.marmicro.2019.101750

UT WoS

000488143600003

Klíčová slova česky

Lang; delta13-C(org); n-alkany; TOC; Centrální Paratethyda; delta13-C; delta O-18

Klíčová slova anglicky

Langhian; delta C-13(org); n-alkanes; TOC; Central Paratethys; delta C-13 and delta O-18

Štítky

rivok

Příznaky

Mezinárodní význam, Recenzováno

Změněno: 27. 3. 2020 17:59, Mgr. Marie Šípková, DiS.

Anotace

V originále

The Langhian epicontinental sea - the Central Paratethys - represented a dynamic environment experiencing many changes, making it an ideal system for testing various geochemical proxies. Here we present a result of a study based on a combination of organic geochemistry (delta 13Corg, n-alkane based indices; TOC/TIC) with benthic foraminiferal stable isotopic (delta 13C; delta 18O) and paleoecological data from the time interval of ~14.4 to 14.36 Ma. Moreover, we evaluated foraminiferal paleoecological data (selected species: Melonis pompilioides; Gyroidinoides spp.; Cibicidoides spp.) together with the delta 13C and delta 18O to interpret the paleoecological consequences at the seafloor. Doing so we assessed the problematics regarding the origin of the organic matter together with changes in productivity and subsequent reaction of benthic foraminiferal assemblages at the seafloor. We used the delta-13Corg, TOC/TIC and the n-alkane based indices to estimate the primary production rate and to determine the origin of the organic matter at the studied locality. The reconstructed paleoenvironment represented an open marine realm without significant freshwater influence, where the primary productivity was generated by marine algae. A gradual decrease of productivity could be observed, linked with shallowing of the basin towards a more carbonate-dominated environment. Changes in nutrient flux and vertical migration of the less oxygenated zone turned out to be the main phenomena responsible for physicochemical and paleoecological changes in the foraminiferal communities within the sediment. In addition we tried to characterize the population dynamics of the studied benthic foraminiferal species under a variety of existing conditions at the seafloor.

Citovat

SCHEINER, Filip, Katarina HOLCOVÁ, Rastislav MILOVSKÝ, Nela DOLÁKOVÁ a Jana RIGOVÁ. Response of benthic foraminiferal communities to changes in productivity and watermass conditions in the epicontinental Paratethys during the middle Miocene. Marine Micropaleontology. ELSEVIER, RADARWEG 29, 1043 NX AMSTERDAM, NETHERLANDS, 2019, roč. 151, AUG 2019, s. 1-12. ISSN 0377-8398. Dostupné z: https://dx.doi.org/10.1016/j.marmicro.2019.101750.

@article{1617296,
   author = {Scheiner, Filip and Holcová, Katarina and Milovský, Rastislav and Doláková, Nela and Rigová, Jana},
   article_number = {AUG 2019},
   doi = {http://dx.doi.org/10.1016/j.marmicro.2019.101750},
   keywords = {Langhian; delta C-13(org); n-alkanes; TOC; Central Paratethys; delta C-13 and delta O-18},
   language = {eng},
   issn = {0377-8398},
   journal = {Marine Micropaleontology},
   title = {Response of benthic foraminiferal communities to changes in productivity and watermass conditions in the epicontinental Paratethys during the middle Miocene},
   url = {https://www.sciencedirect.com/science/article/pii/S0377839819300428?via%3Dihub},
   volume = {151},
   year = {2019}
}

TY  - JOUR
ID  - 1617296
AU  - Scheiner, Filip - Holcová, Katarina - Milovský, Rastislav - Doláková, Nela - Rigová, Jana
PY  - 2019
TI  - Response of benthic foraminiferal communities to changes in productivity and watermass conditions in the epicontinental Paratethys during the middle Miocene
JF  - Marine Micropaleontology
VL  - 151
IS  - AUG 2019
SP  - 1-12
EP  - 1-12
PB  - ELSEVIER, RADARWEG 29, 1043 NX AMSTERDAM, NETHERLANDS
SN  - 03778398
KW  - Langhian
KW  - delta C-13(org)
KW  - n-alkanes
KW  - TOC
KW  - Central Paratethys
KW  - delta C-13 and delta O-18
UR  - https://www.sciencedirect.com/science/article/pii/S0377839819300428?via%3Dihub
L2  - https://www.sciencedirect.com/science/article/pii/S0377839819300428?via%3Dihub
N2  - The Langhian epicontinental sea - the Central Paratethys - represented a dynamic environment experiencing many changes, making it an ideal system for testing various geochemical proxies. Here we present a result of a study based on a combination of organic geochemistry (delta 13Corg, n-alkane based indices; TOC/TIC) with benthic foraminiferal stable isotopic (delta 13C; delta 18O) and paleoecological data from the time interval of ~14.4 to 14.36 Ma. Moreover, we evaluated foraminiferal paleoecological data (selected species: Melonis pompilioides; Gyroidinoides spp.; Cibicidoides spp.) together with the delta 13C and delta 18O to interpret the paleoecological consequences at the seafloor. Doing so we assessed the problematics regarding the origin of the organic matter together with changes in productivity and subsequent reaction of benthic foraminiferal assemblages at the seafloor. We used the delta-13Corg, TOC/TIC and the n-alkane based indices to estimate the primary production rate and to determine the origin of the organic matter at the studied locality. The reconstructed paleoenvironment represented an open marine realm without significant freshwater influence, where the primary productivity was generated by marine algae. A gradual decrease of productivity could be observed, linked with shallowing of the basin towards a more carbonate-dominated environment. Changes in nutrient flux and vertical migration of the less oxygenated zone turned out to be the main phenomena responsible for physicochemical and paleoecological changes in the foraminiferal communities within the sediment. In addition we tried to characterize the population dynamics of the studied benthic foraminiferal species under a variety of existing conditions at the seafloor.
ER  -

SCHEINER, Filip, Katarina HOLCOVÁ, Rastislav MILOVSKÝ, Nela DOLÁKOVÁ a Jana RIGOVÁ. Response of benthic foraminiferal communities to changes in productivity and watermass conditions in the epicontinental Paratethys during the middle Miocene. \textit{Marine Micropaleontology}. ELSEVIER, RADARWEG 29, 1043 NX AMSTERDAM, NETHERLANDS, 2019, roč.~151, AUG 2019, s.~1-12. ISSN~0377-8398. Dostupné z: https://dx.doi.org/10.1016/j.marmicro.2019.101750.

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