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Statements

Subject Item
n2:RIV%2F00216208%3A11310%2F09%3A10131791%21RIV13-MSM-11310___
rdf:type
n14:Vysledek skos:Concept
dcterms:description
Million year-scale (3rd-order) depositional sequences (few 10s to ~100 m-thick) are common in the Devonian marine record and are correlated between sedimentary basins and across widely separated continents implying a eustatic origin. Tectonically driven changes in mid-ocean ridge spreading rates/lengths are too slow to account for the calculated 3rd-order rise/fall rates and typical orbital frequencies (~20- 400 ky) are too fast. We analyzed oxygen isotopes from conodont apatite to evaluate if Early-Middle Devonian 3rd-order sea-level changes were controlled by paleoclimatically driven ice volume (glacioeustasy) and seawater temperature change (thermo-eustasy). Two successive depositional sequences in the western U.S. (Nevada) and Czech Republic (Prague Basin) were sampled. The 18O values range from 1.78% to 2.02% (SMOW) and show similar trends across the Emsian-Eifelian boundary. Million year-scale (3rd-order) depositional sequences (few 10s to ~100 m-thick) are common in the Devonian marine record and are correlated between sedimentary basins and across widely separated continents implying a eustatic origin. Tectonically driven changes in mid-ocean ridge spreading rates/lengths are too slow to account for the calculated 3rd-order rise/fall rates and typical orbital frequencies (~20- 400 ky) are too fast. We analyzed oxygen isotopes from conodont apatite to evaluate if Early-Middle Devonian 3rd-order sea-level changes were controlled by paleoclimatically driven ice volume (glacioeustasy) and seawater temperature change (thermo-eustasy). Two successive depositional sequences in the western U.S. (Nevada) and Czech Republic (Prague Basin) were sampled. The 18O values range from 1.78% to 2.02% (SMOW) and show similar trends across the Emsian-Eifelian boundary.
dcterms:title
Stratigraphic and oxygen isotope evidence for My-scale glaciation driving eustasy in the Early-Middle Devonian greenhouse world Stratigraphic and oxygen isotope evidence for My-scale glaciation driving eustasy in the Early-Middle Devonian greenhouse world
skos:prefLabel
Stratigraphic and oxygen isotope evidence for My-scale glaciation driving eustasy in the Early-Middle Devonian greenhouse world Stratigraphic and oxygen isotope evidence for My-scale glaciation driving eustasy in the Early-Middle Devonian greenhouse world
skos:notation
RIV/00216208:11310/09:10131791!RIV13-MSM-11310___
n3:aktivita
n6:S n6:P n6:I n6:Z
n3:aktivity
I, P(KJB307020602), P(ME08011), S, Z(MZP0002579801)
n3:cisloPeriodika
1-4
n3:dodaniDat
n19:2013
n3:domaciTvurceVysledku
n4:4330048
n3:druhVysledku
n18:J
n3:duvernostUdaju
n17:S
n3:entitaPredkladatele
n7:predkladatel
n3:idSjednocenehoVysledku
344006
n3:idVysledku
RIV/00216208:11310/09:10131791
n3:jazykVysledku
n10:eng
n3:klicovaSlova
Glaciation; Conodont apatite; Oxygen isotopes; Greenhouse; Glacio-eustasy; Devonian
n3:klicoveSlovo
n5:Glacio-eustasy n5:Devonian n5:Oxygen%20isotopes n5:Greenhouse n5:Conodont%20apatite n5:Glaciation
n3:kodStatuVydavatele
NL - Nizozemsko
n3:kontrolniKodProRIV
[848A2674E2ED]
n3:nazevZdroje
Palaeogeography, Palaeoclimatology, Palaeoecology
n3:obor
n16:DB
n3:pocetDomacichTvurcuVysledku
1
n3:pocetTvurcuVysledku
6
n3:projekt
n13:KJB307020602 n13:ME08011
n3:rokUplatneniVysledku
n19:2009
n3:svazekPeriodika
276
n3:tvurceVysledku
Berkyová, Stanislava Klapper, Gilbert Sharp, Zachary Joachimski, Michael Frýda, Jiří Elrick, Maya
n3:wos
000266906200015
n3:zamer
n9:MZP0002579801
s:issn
0031-0182
s:numberOfPages
12
n12:doi
10.1016/j.palaeo.2009.03.008
n15:organizacniJednotka
11310