Alluvial and volcanic pathways to silicified plant stems (Upper
Carboniferous-Triassic) and their taphonomic and
palaeoenvironmental meaning

J 2010

Alluvial and volcanic pathways to silicified plant stems (Upper Carboniferous-Triassic) and their taphonomic and palaeoenvironmental meaning

MATYSOVÁ, Petra, Ronny ROESLLER, Jens GOETZE, Jaromír LEICHMANN, Gordon FORBES et. al.

Základní údaje

Originální název

Alluvial and volcanic pathways to silicified plant stems (Upper Carboniferous-Triassic) and their taphonomic and palaeoenvironmental meaning

Název česky

Aluviální a vulkanický mechanismus silicifikace rostliných kmenů.

Autoři

MATYSOVÁ, Petra (203 Česká republika), Ronny ROESLLER (276 Německo), Jens GOETZE (276 Německo), Jaromír LEICHMANN (203 Česká republika, garant, domácí), Gordon FORBES (826 Velká Británie a Severní Irsko), Edith TAYLOR (826 Velká Británie a Severní Irsko), Jakub SAKALA (203 Česká republika) a Tomas GRYGAR (203 Česká republika)

Vydání

Palaeogeography, Palaeoclimatology, Palaeoecology, 2010, 0031-0182

Další údaje

Jazyk

angličtina

Typ výsledku

Článek v odborném periodiku

Obor

10500 1.5. Earth and related environmental sciences

Stát vydavatele

Nizozemské království

Utajení

není předmětem státního či obchodního tajemství

Impakt faktor

Impact factor: 2.390

Kód RIV

RIV/00216224:14310/10:00047191

Organizační jednotka

Přírodovědecká fakulta

UT WoS

000279489200010

Klíčová slova česky

Křemen;moganit;prostřědí;fosilní dřevo;katodová luminiscence;provenience

Klíčová slova anglicky

Quartz; Moganite; Environment; Fossil wood; Cathodoluminescence; Provenance analysis

Změněno: 28. 4. 2011 14:24, prof. RNDr. Jaromír Leichmann, Dr. rer. nat.

Anotace

ORIG CZ

V originále

: Petrographic imaging, in combination with qualitative and quantitative instrumental analyses of mineral mass, allow us to obtain material signatures of silicified plant stems that are relatively common in sediments of continental basins since the late Palaeozoic. These fossils can be found in their original strata but commonly have been removed from their environmental and stratigraphic context, redeposited, and scattered on the recent land surface after erosion of the parent rocks Analytical data gathered from X-ray diffraction analysis, hot cathodoluminescence (CL) imaging and spectroscopy. electron microprobe analysis, Raman spectrometry, and polarised light microscopy serve to characterise material signatures of samples from basins in Brazil. Germany, the Czech Republic, Sultanate of Oman, Mongolia, Antarctica, France, and the USA This collection includes silicified Pennsylvanian and Permian plant taxa (and a few from the Triassic) found in fluvial environments and sites influenced by volcanism with the purpose to discern fundamental material characteristics formed under particular environmental circumstances. Late Pennsylvanian and Permian silicified stems in fluvial rocks include the presence of well-crystalline quartz (alpha-SiO2), sometimes with a trace of kaolinite, showing weak CL (mostly blue or dark reddish), occasional mosaic or patchy preservation of anatomical details, and other signs of pressure distortion of wet trunks in fluvial deposits and subsequent diagenetic recrystallisation The presumed silica source for the initial stage of silicification was weathering of labile minerals, mostly feldspars in the alluvium. In wood from aeolian deposits, moganite in combination with goethite was detected Based on our results, we propose that the stems were silicified in sandy or gravelly fluvial deposits, most frequently in arkoses and arkosic sands, indicators of relatively warns climate with pronounced seasonal distribution of precipitation Excluded from this interpretation are steins silicified primarily by volcanic material, these are distinguished by a higher species diversity, silicification close to the site of growth, miscellaneous mineralogy, usually with very colourful CL shades, and the presence of metastable forms of SiO2. opal-CT or moganite This volcanic influence on silicification mode is less clearly controlled by seasonality of precipitation or palaeoclimate

Česky

Křemen;moganit;prostřědí;fosilní dřevo;katodová luminiscence;provenience, studium prostředí fosilizace dřev jak je reflektováno v CL

Návaznosti

MSM0021622412, záměr

Název: Interakce mezi chemickými látkami, prostředím a biologickými systémy a jejich důsledky na globální, regionální a lokální úrovni (INCHEMBIOL) (Akronym: INCHEMBIOL)

Investor: Ministerstvo školství, mládeže a tělovýchovy ČR, Interakce mezi chemickými látkami, prostředím a biologickými systémy a jejich důsledky na globální , regionální a lokální úrovni

Citovat

MATYSOVÁ, Petra, Ronny ROESLLER, Jens GOETZE, Jaromír LEICHMANN, Gordon FORBES, Edith TAYLOR, Jakub SAKALA a Tomas GRYGAR. Alluvial and volcanic pathways to silicified plant stems (Upper Carboniferous-Triassic) and their taphonomic and palaeoenvironmental meaning. Palaeogeography, Palaeoclimatology, Palaeoecology. 2010, roč. 292, 1-2, s. 127-143, 16 s. ISSN 0031-0182.

@article{924536,
   author = {Matysová, Petra and Roesller, Ronny and Goetze, Jens and Leichmann, Jaromír and Forbes, Gordon and Taylor, Edith and Sakala, Jakub and Grygar, Tomas},
   article_number = {1-2},
   keywords = {Quartz; Moganite; Environment; Fossil wood; Cathodoluminescence; Provenance analysis},
   language = {eng},
   issn = {0031-0182},
   journal = {Palaeogeography, Palaeoclimatology, Palaeoecology},
   title = {Alluvial and volcanic pathways to silicified plant stems (Upper Carboniferous-Triassic) and their taphonomic and palaeoenvironmental meaning},
   volume = {292},
   year = {2010}
}

TY  - JOUR
ID  - 924536
AU  - Matysová, Petra - Roesller, Ronny - Goetze, Jens - Leichmann, Jaromír - Forbes, Gordon - Taylor, Edith - Sakala, Jakub - Grygar, Tomas
PY  - 2010
TI  - Alluvial and volcanic pathways to silicified plant stems (Upper Carboniferous-Triassic) and their taphonomic and palaeoenvironmental meaning
JF  - Palaeogeography, Palaeoclimatology, Palaeoecology
VL  - 292
IS  - 1-2
SP  - 127-143
EP  - 127-143
SN  - 00310182
KW  - Quartz
KW  - Moganite
KW  - Environment
KW  - Fossil wood
KW  - Cathodoluminescence
KW  - Provenance analysis
N2  - : Petrographic imaging, in combination with qualitative and quantitative instrumental analyses of mineral mass, allow us to obtain material signatures of silicified plant stems that are relatively common in sediments of continental basins since the late Palaeozoic. These fossils can be found in their original strata but commonly have been removed from their environmental and stratigraphic context, redeposited, and scattered on the recent land surface after erosion of the parent rocks Analytical data gathered from X-ray diffraction analysis, hot cathodoluminescence (CL) imaging and spectroscopy. electron microprobe analysis, Raman spectrometry, and polarised light microscopy serve to characterise material signatures of samples from basins in Brazil. Germany, the Czech Republic, Sultanate of Oman, Mongolia, Antarctica, France, and the USA This collection includes silicified Pennsylvanian and Permian plant taxa (and a few from the Triassic) found in fluvial environments and sites influenced by volcanism with the purpose to discern fundamental material characteristics formed under particular environmental circumstances. Late Pennsylvanian and Permian silicified stems in fluvial rocks include the presence of well-crystalline quartz (alpha-SiO2), sometimes with a trace of kaolinite, showing weak CL (mostly blue or dark reddish), occasional mosaic or patchy preservation of anatomical details, and other signs of pressure distortion of wet trunks in fluvial deposits and subsequent diagenetic recrystallisation The presumed silica source for the initial stage of silicification was weathering of labile minerals, mostly feldspars in the alluvium. In wood from aeolian deposits, moganite in combination with goethite was detected Based on our results, we propose that the stems were silicified in sandy or gravelly fluvial deposits, most frequently in arkoses and arkosic sands, indicators of relatively warns climate with pronounced seasonal distribution of precipitation Excluded from this interpretation are steins silicified primarily by volcanic material, these are distinguished by a higher species diversity, silicification close to the site of growth, miscellaneous mineralogy, usually with very colourful CL shades, and the presence of metastable forms of SiO2. opal-CT or moganite This volcanic influence on silicification mode is less clearly controlled by seasonality of precipitation or palaeoclimate
ER  -

MATYSOVÁ, Petra, Ronny ROESLLER, Jens GOETZE, Jaromír LEICHMANN, Gordon FORBES, Edith TAYLOR, Jakub SAKALA a Tomas GRYGAR. Alluvial and volcanic pathways to silicified plant stems (Upper Carboniferous-Triassic) and their taphonomic and palaeoenvironmental meaning. \textit{Palaeogeography, Palaeoclimatology, Palaeoecology}. 2010, roč.~292, 1-2, s.~127-143, 16 s. ISSN~0031-0182.

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