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Statements

Subject Item
n2:RIV%2F00025798%3A_____%2F10%3A00000383%21RIV11-MZP-00025798
rdf:type
n17:Vysledek skos:Concept
dcterms:description
Recurvoides infernus sp. nov., one of the oldest representatives of the superfamily Recurvoidacea (Foraminiferida), is described in a thin black claystone overlaying the manganese deposits of the Krížna Unit in the Tatra Mountains (Poland). These manganese carbonates/silicates were laid down around a shallow exhalative submarine vent, active in the Early Toarcian. The microfossils are possibly the first described Jurassic foraminifera associated with hydrothermal vents. The assemblage is dominated by a high abundance and dominance of this new species. The primary lamination of the claystone, the lack of any macrofauna, and an elevated TOC content point to oxygen-deficient conditions during sedimentation of these deposits. The nearly exclusive occurrence of agglutinated foraminifers suggests a low pH level. It is likely that foraminifers colonized vent-related bacterial mats that acted as a rich and stable food source. Modern shallow- and deep-water hydrothermal vents may represent similar habitats. Recurvoides infernus sp. nov., one of the oldest representatives of the superfamily Recurvoidacea (Foraminiferida), is described in a thin black claystone overlaying the manganese deposits of the Krížna Unit in the Tatra Mountains (Poland). These manganese carbonates/silicates were laid down around a shallow exhalative submarine vent, active in the Early Toarcian. The microfossils are possibly the first described Jurassic foraminifera associated with hydrothermal vents. The assemblage is dominated by a high abundance and dominance of this new species. The primary lamination of the claystone, the lack of any macrofauna, and an elevated TOC content point to oxygen-deficient conditions during sedimentation of these deposits. The nearly exclusive occurrence of agglutinated foraminifers suggests a low pH level. It is likely that foraminifers colonized vent-related bacterial mats that acted as a rich and stable food source. Modern shallow- and deep-water hydrothermal vents may represent similar habitats.
dcterms:title
A new vent-related foraminifer from the lower Toarcian black claystone of the Tatra Mountains, Poland A new vent-related foraminifer from the lower Toarcian black claystone of the Tatra Mountains, Poland
skos:prefLabel
A new vent-related foraminifer from the lower Toarcian black claystone of the Tatra Mountains, Poland A new vent-related foraminifer from the lower Toarcian black claystone of the Tatra Mountains, Poland
skos:notation
RIV/00025798:_____/10:00000383!RIV11-MZP-00025798
n3:aktivita
n10:Z n10:I
n3:aktivity
I, Z(MZP0002579801)
n3:cisloPeriodika
2
n3:dodaniDat
n5:2011
n3:domaciTvurceVysledku
n11:5048125
n3:druhVysledku
n14:J
n3:duvernostUdaju
n12:S
n3:entitaPredkladatele
n16:predkladatel
n3:idSjednocenehoVysledku
244785
n3:idVysledku
RIV/00025798:_____/10:00000383
n3:jazykVysledku
n15:eng
n3:klicovaSlova
Foraminifera, Ammosphaeroidinidae, agglutinated foraminifera, hydrothermal vent, black claystone, suboxia, The Carpathians, Tethys, Jurassic
n3:klicoveSlovo
n6:suboxia n6:Foraminifera n6:Tethys n6:agglutinated%20foraminifera n6:Jurassic n6:The%20Carpathians n6:black%20claystone n6:Ammosphaeroidinidae n6:hydrothermal%20vent
n3:kodStatuVydavatele
PL - Polská republika
n3:kontrolniKodProRIV
[CD10078387E2]
n3:nazevZdroje
Acta Palaeontologica Polonica
n3:obor
n8:DB
n3:pocetDomacichTvurcuVysledku
1
n3:pocetTvurcuVysledku
3
n3:rokUplatneniVysledku
n5:2010
n3:svazekPeriodika
55
n3:tvurceVysledku
Jach, Renata Bubík, Miroslav Tyszka, Jarosław
n3:wos
000278409700012
n3:zamer
n7:MZP0002579801
s:issn
0567-7920
s:numberOfPages
9