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A quantitative approach for identifying plant ecogroups in the Romanian Early Jurassic terrestrial vegetation
Barbacka, M [Barbacka, Mária (Ősnövénytan), szerző]
;
Popa, ME
;
Mitka, J
;
Bodor, E [Bodor, Emese Réka (Geológia, paleont...), szerző] Őslénytani Tanszék (ELTE / TTK / Ft_K)
;
Püspöki, Z [Püspöki, Zoltán (Földtan), szerző]
;
McIntosh, RW [McIntosh, Richard William (geológia), szerző] Ásvány- és Földtani Tanszék (DE / TTK / FoldtI)
Angol nyelvű Szakcikk (Folyóiratcikk) Tudományos
Megjelent:
PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY 0031-0182 1872-616X
446
pp. 44-54
2016
X. Földtudományok Osztálya: A
SJR Scopus - Paleontology: D1
Azonosítók
MTMT: 3014943
DOI:
10.1016/j.palaeo.2016.01.010
WoS:
000371553000005
DEA:
275959
REAL:
121530
Scopus:
84955244056
Szakterületek:
Biológiai tudományok
Föld- és kapcsolódó környezettudományok
Community level ecology is considered to support significantly the recognition of the ecological status of plant taxa and the identification of plant ecogroups, thus it generally provides extended data sets on the spatial and temporal changes of ecological factors. Since research based exclusively on plant structure and their supposed adaptation to the environment is now considered inadequate, statistical methods can be used. Assuming that co-occurrence of plant fossils on a single hand specimen in the case of autochthonous or parautochthonous floras is the result of their growth in the same phytocenosis, quantitative ecological analysis on Mesozoic materials would yield significant insights. In this paper, statistical and multivariate quantitative analyses of Early Jurassic plant fossil records from the Steierdorf Formation in Anina (South Carpathians, Romania) are presented. Four palaeoecological groups of taxa were distinguished by principal component analysis (PCA) and interpreted as plant assemblages of various palaeobiotopes associated with the sedimentary facies of the enclosing formation. A group of samples was analysed using the principal coordinate (PCO) method and the statistical significance (p {less than or equal to} 0.05) (p ≤ 0.05) of individual binary responses of taxa along the first two PCO ordination axes was tested by general linear model (GLM). They revealed putative palaeoecological gradients: axis 1 - disturbance caused by water level fluctuations, axis 2 - temperature, corresponding with the already assumed environmental and climatic change at the Hettangian/Sinemurian boundary. Multivariate analyses enabled the identification of palaeoecological groups and thus inferring palaeogeographical conditions based on Mesozoic materials. © 2016 Elsevier B.V.
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2024-10-08 05:30
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