The chinese upright stone tablets started building early inQindynasty which were called stone-carving in the Initial stage.After the Eastern Han Dynasty, they were gradually changed name as"tablets" or "...The chinese upright stone tablets started building early inQindynasty which were called stone-carving in the Initial stage.After the Eastern Han Dynasty, they were gradually changed name as"tablets" or "steles" with the increasing of carved stones. Greatnumbers of stone tablets standing like trees in forest, were later展开更多
The cortex(i.e.,absorptive tissue)and stele(transportive vascular tissue)are fundamental to the function of plant roots.Unraveling how these anatomical structures are assembled in absorptive roots is essential for our...The cortex(i.e.,absorptive tissue)and stele(transportive vascular tissue)are fundamental to the function of plant roots.Unraveling how these anatomical structures are assembled in absorptive roots is essential for our understanding of plant ecology,physiology,and plant responses to global environmental changes.In this review,we first compile a large data set on anatomical traits in absorptive roots,including cortex thickness and stele radius,across 698 observations and 512 species.Using this data set,we reveal a common root allometry in absorptive root structures,i.e.,cortex thickness increases much faster than stele radius with increasing root diameter(hereafter,root allometry).Root allometry is further validated within and across plant growth forms(woody,grass,and liana species),mycorrhiza types(arbuscular mycorrhiza,ectomycorrhiza,and orchid mycorrhizas),phylogenetic gradients(from ferns to Orchidaceae),and environmental change scenarios(e.g.,elevation of atmospheric CO_(2)concentration and nitrogen fertilization).These findings indicate that root allometry is common in plants.Importantly,root allometry varies greatly across species.We then summarize recent research on the mechanisms of root allometry and potential issues regarding these mechanisms.We further discuss ecological and evolutionary implications of root allometry.Finally,we propose several important research directions that should be pursued regarding root allometry.展开更多
Although post-mortem apotheosis and secular honor in temples have received more attention,shrines to living men were also ordinary institutions from Han times onwards in Chinese history.Previous scholarship so far on ...Although post-mortem apotheosis and secular honor in temples have received more attention,shrines to living men were also ordinary institutions from Han times onwards in Chinese history.Previous scholarship so far on pre-mortem shrines in Tang and Song relates them to pre-mortem commemoration in inscribed records of local commendation on the one hand and Neo-Confucian Daoxue Shrines to Local Worthies on the other.That scholarly work suggests that Tang and Song premortem shrines when political were basically elite institutions;and that when common people were involved their motivations were religious rather than political.In Ming times,by contrast,premortem shrines were normatively established by commoners and const^uted a venue for popular political participation,while the steles commemorating the shrines explicitly argued that non-el让e people had the right to political speech.This article speculates,as a hypothesis awaiting further research,that both Yuan modes of government generally,and creative uses of premortem enshrinement in Yuan times specifically,may have contributed to Ming populism.展开更多
Iron (Fe) migration in soil-plants is a critical part of Fe biogeochemical cycling in the earth surface system. Fe isotope fractionation analysis in the soil-rice system is promising for quantitatively assessing vario...Iron (Fe) migration in soil-plants is a critical part of Fe biogeochemical cycling in the earth surface system. Fe isotope fractionation analysis in the soil-rice system is promising for quantitatively assessing various pathways and clarifying Fe transformation processes. However, the mechanisms of Fe isotope fractionation in the soil-rice system are not well understood. In this study, the Fe isotopic compositions (δ^(56)Fe) of rhizosphere soils, pore water, Fe plaque, and rice plant tissues at the jointing and mature stages of the plants were determined. The rice plants were slightly enriched in heavier δ^(56)Fe by 0.3‰ relative to the soil, and the stele and cortex showed similar δ^(56)Fe values, indicating that the uptake of Fe by rice plants predominantly occurred via Fe(III)-phytosiderophores (Fe(III)-PS) chelation, but not Fe(III) reduction. Additionally, at both the jointing and mature stages, the rice plant tissues showed similar δ^(56)Fe values. However, the Fe isotope fractionation between the roots and stems (Δ56Feroot−stem) was 1.39 ± 0.13‰, which is similar to the previously Ab initio-calculated values between Fe(III)-citrate and Fe(III)- 2-deoxymugineic acid (DMA), indicating that both the phloem and xylem have similar δ^(56)Fe values, and the major Fe-chelating substances in the phloem of the rice plants are Fe(III)-DMA and Fe(II)- Nicotianamine (NA). Therefore, this study demonstrates that Fe isotope fractionation can be used as a signature for interpreting the Fe uptake and translocation mechanism in the soil-rice system.展开更多
文摘The chinese upright stone tablets started building early inQindynasty which were called stone-carving in the Initial stage.After the Eastern Han Dynasty, they were gradually changed name as"tablets" or "steles" with the increasing of carved stones. Greatnumbers of stone tablets standing like trees in forest, were later
基金This study was funded by the National Natural Science Foundation of China(32171746,42077450,31870522 and 31670550)Funding for Characteristic and Backbone Forestry Discipline Group of Henan Province,and the Scientific Research Foundation of Henan Agricultural University(30500854),Research Funds for overseas returnee in Henan Province,China.
文摘The cortex(i.e.,absorptive tissue)and stele(transportive vascular tissue)are fundamental to the function of plant roots.Unraveling how these anatomical structures are assembled in absorptive roots is essential for our understanding of plant ecology,physiology,and plant responses to global environmental changes.In this review,we first compile a large data set on anatomical traits in absorptive roots,including cortex thickness and stele radius,across 698 observations and 512 species.Using this data set,we reveal a common root allometry in absorptive root structures,i.e.,cortex thickness increases much faster than stele radius with increasing root diameter(hereafter,root allometry).Root allometry is further validated within and across plant growth forms(woody,grass,and liana species),mycorrhiza types(arbuscular mycorrhiza,ectomycorrhiza,and orchid mycorrhizas),phylogenetic gradients(from ferns to Orchidaceae),and environmental change scenarios(e.g.,elevation of atmospheric CO_(2)concentration and nitrogen fertilization).These findings indicate that root allometry is common in plants.Importantly,root allometry varies greatly across species.We then summarize recent research on the mechanisms of root allometry and potential issues regarding these mechanisms.We further discuss ecological and evolutionary implications of root allometry.Finally,we propose several important research directions that should be pursued regarding root allometry.
文摘Although post-mortem apotheosis and secular honor in temples have received more attention,shrines to living men were also ordinary institutions from Han times onwards in Chinese history.Previous scholarship so far on pre-mortem shrines in Tang and Song relates them to pre-mortem commemoration in inscribed records of local commendation on the one hand and Neo-Confucian Daoxue Shrines to Local Worthies on the other.That scholarly work suggests that Tang and Song premortem shrines when political were basically elite institutions;and that when common people were involved their motivations were religious rather than political.In Ming times,by contrast,premortem shrines were normatively established by commoners and const^uted a venue for popular political participation,while the steles commemorating the shrines explicitly argued that non-el让e people had the right to political speech.This article speculates,as a hypothesis awaiting further research,that both Yuan modes of government generally,and creative uses of premortem enshrinement in Yuan times specifically,may have contributed to Ming populism.
基金This work was supported by the National Natural Science Foundation of China(Grant Nos.41807026,42030702,and U20A20109)China Postdoctoral Science Foundation(Grant Nos.2020T130126 and 2019M662820)+3 种基金Guangdong Key Research and Development Project(Grant Nos.2019B110207002)Local Innovative and Research Teams Project of Guangdong Pearl River Talents Program(Grant Nos.2017BT01Z176)projects of Science and Technology Development in Guangdong Academy of Sciences(Grant Nos.2020GDASYL-20200104022 and 2019GDASYL-0103054)Guangdong Special Support Plan for High-Level Talents(Grant Nos.2017TX04Z175).
文摘Iron (Fe) migration in soil-plants is a critical part of Fe biogeochemical cycling in the earth surface system. Fe isotope fractionation analysis in the soil-rice system is promising for quantitatively assessing various pathways and clarifying Fe transformation processes. However, the mechanisms of Fe isotope fractionation in the soil-rice system are not well understood. In this study, the Fe isotopic compositions (δ^(56)Fe) of rhizosphere soils, pore water, Fe plaque, and rice plant tissues at the jointing and mature stages of the plants were determined. The rice plants were slightly enriched in heavier δ^(56)Fe by 0.3‰ relative to the soil, and the stele and cortex showed similar δ^(56)Fe values, indicating that the uptake of Fe by rice plants predominantly occurred via Fe(III)-phytosiderophores (Fe(III)-PS) chelation, but not Fe(III) reduction. Additionally, at both the jointing and mature stages, the rice plant tissues showed similar δ^(56)Fe values. However, the Fe isotope fractionation between the roots and stems (Δ56Feroot−stem) was 1.39 ± 0.13‰, which is similar to the previously Ab initio-calculated values between Fe(III)-citrate and Fe(III)- 2-deoxymugineic acid (DMA), indicating that both the phloem and xylem have similar δ^(56)Fe values, and the major Fe-chelating substances in the phloem of the rice plants are Fe(III)-DMA and Fe(II)- Nicotianamine (NA). Therefore, this study demonstrates that Fe isotope fractionation can be used as a signature for interpreting the Fe uptake and translocation mechanism in the soil-rice system.