Salt stress is a major abiotic stress limiting plant growth and yield. In the present study, the effects of exogenous H_(2)O_(2) on the reactive oxygen species(ROS) metabolism and the antioxidant system in leaves of N...Salt stress is a major abiotic stress limiting plant growth and yield. In the present study, the effects of exogenous H_(2)O_(2) on the reactive oxygen species(ROS) metabolism and the antioxidant system in leaves of Nitralia tangutorum Bobr. under salt stress were studied. N. tangutorum seedlings were subjected to 200 mmol·L^(-1) NaCl treatment with or without the exogenous application of H_(2)O_(2) for 7 days. The results showed that NaCl stress significantly increased the relative conductivity, the contents of thiobarbituric acid reactive substances(TBARS) and ROS(H_(2)O_(2) and O_(2)^(·-)), as well as promoted the activities of antioxidant enzymes including superoxide dismutase(SOD), peroxidase(POD), catalase(CAT), and ascorbate peroxidase(APX) in N. tangutorum leaves. In addition, exogenous H_(2)O_(2) decreased the relative conductivity, the contents of TBARS, H_(2)O_(2) and O_(2)^(·-), while further enhanced the activities of antioxidant enzymes. These results indicated that H_(2)O_(2) effectively alleviated the adverse effects of NaCl stress on N. tangutorum through the regulation of ROS metabolism.展开更多
榴辉岩中单斜辉石和石榴子石之间显著的镁同位素平衡分馏,使其成为一种具有潜力的高精度地质温度计。为此,本文选取文献中已报道的来自西南天山洋壳冷俯冲造山带、大别-苏鲁陆壳碰撞造山带和南非卡普瓦尔克拉通三种构造环境中的64对单...榴辉岩中单斜辉石和石榴子石之间显著的镁同位素平衡分馏,使其成为一种具有潜力的高精度地质温度计。为此,本文选取文献中已报道的来自西南天山洋壳冷俯冲造山带、大别-苏鲁陆壳碰撞造山带和南非卡普瓦尔克拉通三种构造环境中的64对单斜辉石-石榴子石矿物对镁同位素数据,利用δ26MgCpx-δ26MgGrt图解筛选出50对达到镁同位素平衡分馏的数据,采用Huang et al.(2013)通过第一性原理计算和Wang et al.(2012)、Li et al.(2016)分别通过经验估计得出的镁同位素温度计计算榴辉岩的峰期温度,并与前人研究结果进行对比。通过分析计算结果,发现对于造山带榴辉岩,Huang et al.(2013)的温度计计算结果与前人通过传统温度计和相平衡模拟研究结果较一致,较好地重现了榴辉岩的峰期温度,而Wang et al.(2012)和Li et al.(2016)的温度计计算结果明显低于前人获得的峰期温度;对于克拉通榴辉岩,三种镁同位素温度计的计算结果与前人通过传统温度计获得的研究结果大多数相差在50℃以上,很可能是早期退变质过程中镁同位素在高温条件下再平衡导致的,这表明三种镁同位素温度计均不适用于克拉通榴辉岩。同时,基于这些榴辉岩样品数据,本文利用经验估计的方法进行校准,得到了新的单斜辉石-石榴子石镁同位素公式Δ26MgCpx-Grt=1.11×10^6/[T(K)]2(R2=0.92)。此外,本文也对单斜辉石-石榴子石镁同位素地质温度计的应用前景及应用时应当注意的问题进行了简单的探讨。展开更多
Recent progress in the study of the UHP metamorphic belt in southwestern Tianshan,China,is summarized in this paper.This about 80-km-long and over 10-km-wide UHP belt has been recognized by the discovery of coesite,co...Recent progress in the study of the UHP metamorphic belt in southwestern Tianshan,China,is summarized in this paper.This about 80-km-long and over 10-km-wide UHP belt has been recognized by the discovery of coesite,coesite pseudomorphs and other UHP minerals.It is the largest oceanic-type UHP metamorphic belt reported so far.It has formed due to northward subduction of the Tianshan Paleo-Ocean.U-Pb dating of metamorphic rims of zircons from a coesite-bearing garnet-phengite schist yields a peak UHP metamorphic ages of 320±3.7 Ma.Combined with ages of 233–226 Ma obtained from rims of zircons from retrograded eclogites,a long retrograde metamorphic evolution(>70 Ma)has been revealed.According to phase equilibria modeling,the P-T paths of both coesite-bearing eclogites and garnet-phengite schists are characterized by thermal relaxation,i.e.,the metamorphic temperature peak lags behind the pressure peak,indicating that the UHP rocks experienced slow and long heating and decompression during exhumation in the subduction channel.On the basis of the field observation that a small amount of eclogite lenses is wrapped in large volumes of metapelites,and the similar P-T paths of both rock types,we propose that the exhumation of the UHP eclogites from southwestern Tianshan,China,may have resulted from the exhumation of large volumes of low-density metapelites,which carried the denser eclogites to the Earth’s surface.展开更多
基金Supported by the Natural Science Foundation of Heilongjiang Province(LH2019C021)。
文摘Salt stress is a major abiotic stress limiting plant growth and yield. In the present study, the effects of exogenous H_(2)O_(2) on the reactive oxygen species(ROS) metabolism and the antioxidant system in leaves of Nitralia tangutorum Bobr. under salt stress were studied. N. tangutorum seedlings were subjected to 200 mmol·L^(-1) NaCl treatment with or without the exogenous application of H_(2)O_(2) for 7 days. The results showed that NaCl stress significantly increased the relative conductivity, the contents of thiobarbituric acid reactive substances(TBARS) and ROS(H_(2)O_(2) and O_(2)^(·-)), as well as promoted the activities of antioxidant enzymes including superoxide dismutase(SOD), peroxidase(POD), catalase(CAT), and ascorbate peroxidase(APX) in N. tangutorum leaves. In addition, exogenous H_(2)O_(2) decreased the relative conductivity, the contents of TBARS, H_(2)O_(2) and O_(2)^(·-), while further enhanced the activities of antioxidant enzymes. These results indicated that H_(2)O_(2) effectively alleviated the adverse effects of NaCl stress on N. tangutorum through the regulation of ROS metabolism.
文摘榴辉岩中单斜辉石和石榴子石之间显著的镁同位素平衡分馏,使其成为一种具有潜力的高精度地质温度计。为此,本文选取文献中已报道的来自西南天山洋壳冷俯冲造山带、大别-苏鲁陆壳碰撞造山带和南非卡普瓦尔克拉通三种构造环境中的64对单斜辉石-石榴子石矿物对镁同位素数据,利用δ26MgCpx-δ26MgGrt图解筛选出50对达到镁同位素平衡分馏的数据,采用Huang et al.(2013)通过第一性原理计算和Wang et al.(2012)、Li et al.(2016)分别通过经验估计得出的镁同位素温度计计算榴辉岩的峰期温度,并与前人研究结果进行对比。通过分析计算结果,发现对于造山带榴辉岩,Huang et al.(2013)的温度计计算结果与前人通过传统温度计和相平衡模拟研究结果较一致,较好地重现了榴辉岩的峰期温度,而Wang et al.(2012)和Li et al.(2016)的温度计计算结果明显低于前人获得的峰期温度;对于克拉通榴辉岩,三种镁同位素温度计的计算结果与前人通过传统温度计获得的研究结果大多数相差在50℃以上,很可能是早期退变质过程中镁同位素在高温条件下再平衡导致的,这表明三种镁同位素温度计均不适用于克拉通榴辉岩。同时,基于这些榴辉岩样品数据,本文利用经验估计的方法进行校准,得到了新的单斜辉石-石榴子石镁同位素公式Δ26MgCpx-Grt=1.11×10^6/[T(K)]2(R2=0.92)。此外,本文也对单斜辉石-石榴子石镁同位素地质温度计的应用前景及应用时应当注意的问题进行了简单的探讨。
基金supported by the National Basic Research Program of China(2009CB825007)the National Natural Science Foundation of China(41121062 and41272069)
文摘Recent progress in the study of the UHP metamorphic belt in southwestern Tianshan,China,is summarized in this paper.This about 80-km-long and over 10-km-wide UHP belt has been recognized by the discovery of coesite,coesite pseudomorphs and other UHP minerals.It is the largest oceanic-type UHP metamorphic belt reported so far.It has formed due to northward subduction of the Tianshan Paleo-Ocean.U-Pb dating of metamorphic rims of zircons from a coesite-bearing garnet-phengite schist yields a peak UHP metamorphic ages of 320±3.7 Ma.Combined with ages of 233–226 Ma obtained from rims of zircons from retrograded eclogites,a long retrograde metamorphic evolution(>70 Ma)has been revealed.According to phase equilibria modeling,the P-T paths of both coesite-bearing eclogites and garnet-phengite schists are characterized by thermal relaxation,i.e.,the metamorphic temperature peak lags behind the pressure peak,indicating that the UHP rocks experienced slow and long heating and decompression during exhumation in the subduction channel.On the basis of the field observation that a small amount of eclogite lenses is wrapped in large volumes of metapelites,and the similar P-T paths of both rock types,we propose that the exhumation of the UHP eclogites from southwestern Tianshan,China,may have resulted from the exhumation of large volumes of low-density metapelites,which carried the denser eclogites to the Earth’s surface.
