Wood decay of Xenoxylon yunnanensis Feng sp nov from the Middle Jurassic of Yunnan Province, China

A permineralised gymnosperm wood, Xenoxylon yunnanensis Feng sp. nov., is described from the Middle Jurassic Shaximiao Formation in Huize County, Yunnan Province, Southwest China. The pycnoxylic wood consists of thick-walled tracheids and thin-walled rays. It is characterised by uniseriate, contiguo...

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Published in:Palaeogeography, Palaeoclimatology, Palaeoecology
Main Authors: Feng, Zhuo, Wei, Hai-Bo, Wang, Chun-Ling, Chen, Yu-Xuan, Shen, Jia-Jia, Yang, Ji-Yuan
Format: Report
Language:English
Published: ELSEVIER SCIENCE BV 2015
Subjects:
Online Access:http://ir.nigpas.ac.cn/handle/332004/11972
https://doi.org/10.1016/j.palaeo.2015.05.021
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spelling ftchinacscnigpas:oai:ir.nigpas.ac.cn:332004/11972 2023-05-15T13:15:21+02:00 Wood decay of Xenoxylon yunnanensis Feng sp nov from the Middle Jurassic of Yunnan Province, China Feng, Zhuo Wei, Hai-Bo Wang, Chun-Ling Chen, Yu-Xuan Shen, Jia-Jia Yang, Ji-Yuan 2015-09-01 http://ir.nigpas.ac.cn/handle/332004/11972 https://doi.org/10.1016/j.palaeo.2015.05.021 英语 eng ELSEVIER SCIENCE BV PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY Feng, Z . Wood decay of Xenoxylon yunnanensis Feng sp nov from the Middle Jurassic of Yunnan Province, China[J]. Palaeogeography, Palaeoclimatology, Palaeoecology,2015,433(?):60-70. http://ir.nigpas.ac.cn/handle/332004/11972 doi:10.1016/j.palaeo.2015.05.021 Fossil wood Saprophytic Xenoxylon yunnanensis Feng Plant-fungal interaction Jurassic GENUS XENOXYLON PALEOCLIMATIC IMPLICATIONS CLAMP CONNECTIONS LIAONING PROVINCE ALEXANDER ISLAND PALEOZOIC FUNGI GROWTH RINGS TREE GROWTH ANTARCTICA Physical Geography Geology Paleontology Geography Physical Geosciences Multidisciplinary 期刊论文 2015 ftchinacscnigpas https://doi.org/10.1016/j.palaeo.2015.05.021 2019-10-11T00:03:18Z A permineralised gymnosperm wood, Xenoxylon yunnanensis Feng sp. nov., is described from the Middle Jurassic Shaximiao Formation in Huize County, Yunnan Province, Southwest China. The pycnoxylic wood consists of thick-walled tracheids and thin-walled rays. It is characterised by uniseriate, contiguous, compressed bordered pits on the radial walls of tracheids, and one large simple pit in each cross-field. Growth rings exhibit narrow late-wood. The mean sensitivity of analysis of 25 growth rings is 0.2, suggesting that a climate with abundant rainfall and weak seasonality could have prevailed in Yunnan, at least locally, during the Middle Jurassic. The outer portion of the wood is largely decayed, and shows poorly preserved cells lacking details. Decayed tracheids displaying various features, including removal of middle lamellae, separations of secondary walls, presence of thickened corners and appositions, are recognised as cell reactions to fungal activity. Irregularly distributed micro-cavities are formed by complete decomposition of tracheids and rays in the wood. Abundant fungal remains occurring in the wood generally consist of multiple branched hyphae. These fungal hyphae are either confined to individual cell lumens or extend through adjacent cells. Although the probable reproductive structure and typical clamp connection are very rarely observed with few septate hyphae, the affinities of these fungal hyphae are somewhat obscure. Nevertheless, our study sheds light on the palaeoecology of Middle Jurassic terrestrial ecosystems of Southwest China. (C) 2015 Elsevier B.V. All rights reserved. Report Alexander Island Antarc* Antarctica Nanjing Institute of Geology and Palaeontology: NIGPAS OpenIR (Chinese Academy of Sciences) Alexander Island ENVELOPE(-69.895,-69.895,-71.287,-71.287) Palaeogeography, Palaeoclimatology, Palaeoecology 433 60 70
institution Open Polar
collection Nanjing Institute of Geology and Palaeontology: NIGPAS OpenIR (Chinese Academy of Sciences)
op_collection_id ftchinacscnigpas
language English
topic Fossil wood
Saprophytic
Xenoxylon yunnanensis Feng
Plant-fungal interaction
Jurassic
GENUS XENOXYLON
PALEOCLIMATIC IMPLICATIONS
CLAMP CONNECTIONS
LIAONING PROVINCE
ALEXANDER ISLAND
PALEOZOIC FUNGI
GROWTH RINGS
TREE GROWTH
ANTARCTICA
Physical Geography
Geology
Paleontology
Geography
Physical
Geosciences
Multidisciplinary
spellingShingle Fossil wood
Saprophytic
Xenoxylon yunnanensis Feng
Plant-fungal interaction
Jurassic
GENUS XENOXYLON
PALEOCLIMATIC IMPLICATIONS
CLAMP CONNECTIONS
LIAONING PROVINCE
ALEXANDER ISLAND
PALEOZOIC FUNGI
GROWTH RINGS
TREE GROWTH
ANTARCTICA
Physical Geography
Geology
Paleontology
Geography
Physical
Geosciences
Multidisciplinary
Feng, Zhuo
Wei, Hai-Bo
Wang, Chun-Ling
Chen, Yu-Xuan
Shen, Jia-Jia
Yang, Ji-Yuan
Wood decay of Xenoxylon yunnanensis Feng sp nov from the Middle Jurassic of Yunnan Province, China
topic_facet Fossil wood
Saprophytic
Xenoxylon yunnanensis Feng
Plant-fungal interaction
Jurassic
GENUS XENOXYLON
PALEOCLIMATIC IMPLICATIONS
CLAMP CONNECTIONS
LIAONING PROVINCE
ALEXANDER ISLAND
PALEOZOIC FUNGI
GROWTH RINGS
TREE GROWTH
ANTARCTICA
Physical Geography
Geology
Paleontology
Geography
Physical
Geosciences
Multidisciplinary
description A permineralised gymnosperm wood, Xenoxylon yunnanensis Feng sp. nov., is described from the Middle Jurassic Shaximiao Formation in Huize County, Yunnan Province, Southwest China. The pycnoxylic wood consists of thick-walled tracheids and thin-walled rays. It is characterised by uniseriate, contiguous, compressed bordered pits on the radial walls of tracheids, and one large simple pit in each cross-field. Growth rings exhibit narrow late-wood. The mean sensitivity of analysis of 25 growth rings is 0.2, suggesting that a climate with abundant rainfall and weak seasonality could have prevailed in Yunnan, at least locally, during the Middle Jurassic. The outer portion of the wood is largely decayed, and shows poorly preserved cells lacking details. Decayed tracheids displaying various features, including removal of middle lamellae, separations of secondary walls, presence of thickened corners and appositions, are recognised as cell reactions to fungal activity. Irregularly distributed micro-cavities are formed by complete decomposition of tracheids and rays in the wood. Abundant fungal remains occurring in the wood generally consist of multiple branched hyphae. These fungal hyphae are either confined to individual cell lumens or extend through adjacent cells. Although the probable reproductive structure and typical clamp connection are very rarely observed with few septate hyphae, the affinities of these fungal hyphae are somewhat obscure. Nevertheless, our study sheds light on the palaeoecology of Middle Jurassic terrestrial ecosystems of Southwest China. (C) 2015 Elsevier B.V. All rights reserved.
format Report
author Feng, Zhuo
Wei, Hai-Bo
Wang, Chun-Ling
Chen, Yu-Xuan
Shen, Jia-Jia
Yang, Ji-Yuan
author_facet Feng, Zhuo
Wei, Hai-Bo
Wang, Chun-Ling
Chen, Yu-Xuan
Shen, Jia-Jia
Yang, Ji-Yuan
author_sort Feng, Zhuo
title Wood decay of Xenoxylon yunnanensis Feng sp nov from the Middle Jurassic of Yunnan Province, China
title_short Wood decay of Xenoxylon yunnanensis Feng sp nov from the Middle Jurassic of Yunnan Province, China
title_full Wood decay of Xenoxylon yunnanensis Feng sp nov from the Middle Jurassic of Yunnan Province, China
title_fullStr Wood decay of Xenoxylon yunnanensis Feng sp nov from the Middle Jurassic of Yunnan Province, China
title_full_unstemmed Wood decay of Xenoxylon yunnanensis Feng sp nov from the Middle Jurassic of Yunnan Province, China
title_sort wood decay of xenoxylon yunnanensis feng sp nov from the middle jurassic of yunnan province, china
publisher ELSEVIER SCIENCE BV
publishDate 2015
url http://ir.nigpas.ac.cn/handle/332004/11972
https://doi.org/10.1016/j.palaeo.2015.05.021
long_lat ENVELOPE(-69.895,-69.895,-71.287,-71.287)
geographic Alexander Island
geographic_facet Alexander Island
genre Alexander Island
Antarc*
Antarctica
genre_facet Alexander Island
Antarc*
Antarctica
op_relation PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY
Feng, Z . Wood decay of Xenoxylon yunnanensis Feng sp nov from the Middle Jurassic of Yunnan Province, China[J]. Palaeogeography, Palaeoclimatology, Palaeoecology,2015,433(?):60-70.
http://ir.nigpas.ac.cn/handle/332004/11972
doi:10.1016/j.palaeo.2015.05.021
op_doi https://doi.org/10.1016/j.palaeo.2015.05.021
container_title Palaeogeography, Palaeoclimatology, Palaeoecology
container_volume 433
container_start_page 60
op_container_end_page 70
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