Enhanced terrestrial carbon uptake in the Northern High Latitudes in the 21st century from the Coupled Carbon Cycle Climate Model Intercomparison Project model projections

The ongoing and projected warming in the northern high latitudes (NHL; poleward of 60 °N) may lead to dramatic changes in the terrestrial carbon cycle. On the one hand, warming and increasing atmospheric CO₂ concentration stimulate vegetation productivity, taking up CO₂. On the other hand, warming accelerates the decomposition of soil organic matter (SOM), releasing carbon into the atmosphere. Here, the NHL terrestrial carbon storage is investigated based on 10 models from the Coupled Carbon Cycle Climate Model Intercomparison Project. Our analysis suggests that the NHL will be a carbon sink of 0.3 ± 0.3 Pg C yr^?1 by 2100. The cumulative land organic carbon storage is modeled to increase by 38 ± 20 Pg C over 1901 levels, of which 17 ± 8 Pg C comes from vegetation (43%) and 21 ± 16 Pg C from the soil (8%). Both CO₂ fertilization and warming enhance vegetation growth in the NHL. Although the intense warming there enhances SOM decomposition, soil organic carbon (SOC) storage continues to increase in the 21st century. This is because higher vegetation productivity leads to more turnover (litterfall) into the soil, a process that has received relatively little attention. However, the projected growth rate of SOC begins to level off after 2060 when SOM decomposition accelerates at high temperature and then catches up with the increasing input from vegetation turnover. Such competing mechanisms may lead to a switch of the NHL SOC pool from a sink to a source after 2100 under more intense warming, but large uncertainty exists due to our incomplete understanding of processes such as the strength of the CO₂ fertilization effect, permafrost, and the role of soil moisture. Unlike the CO₂ fertilization effect that enhances vegetation productivity across the world, global warming increases the productivity at high latitudes but tends to reduce it in the tropics and mid‐latitudes. These effects are further enhanced as a result of positive carbon cycle–climate feedbacks due to additional CO₂ and warming.     

南海北部浮游植物生长对营养盐的响应

2004年夏季作者在南海北部海域研究了浮游植物生长的营养动力学,结合物理-化学过程对浮游植物生物量分布的影响与机制进行了研究,阐明了水平对流和中尺度涡对营养盐分布的影响及浮游植物生长和现存生物量对其的响应。受西南季风和东向沿岸流作用所形成的Ekman输送的影响,南海北部海岸带表层海水作离岸运动,使深层富含营养盐的冷水爬坡涌升到表层来补充,激发浮游植物生物量迅速增长。海区反气旋涡使海水辐聚下沉,造成水体具高温、低盐、高溶解氧浓度、低营养盐浓度和低浮游植物生物量。同时通过现场营养盐加富试验,发现该海域营养盐是浮游植物生长的主要限制因子,而且是多种营养元素共同限制了浮游植物的生长,添加单一的营养盐并不能促进浮游植物的生长。在生物量出现增长的试验组中,营养盐添加不仅促使浮游植物生物量的增长,而且也改变了浮游植物的粒级结构和群落结构。例如,在站S1008,培养前叶绿素a浓度为0.28 mg.m-3,加富培养60 h后浮游植物生物量在NP和NPSi的试验组中有显著的增加,叶绿素a浓度分别达1.07 mg.m-3和1.19 mg.m-3;培养前粒度分级叶绿素a主要以Pico级份占优势,而加富试验结束后,在NP和NPSi的试验组以Nano级份占优势,其它试验组仍以Pico级份占优势;同时,在培养后生物量出现增长的试验组,浮游植物群落的优势类群从甲藻向硅藻演替。     

长江三峡库区堇叶芥属（十字花科）一新种

采于长江三峡库区一个植物新种,属于十字花科堇叶芥属,与大花堇叶芥(Neomartinella grandifloraA l-schehbaz)相比较,其特点为常绿草本,叶两面密被糙伏毛,叶柄密被短柔毛,花序密被短柔毛,长角果略呈镰刀状,长0.9~1.2 cm,命名为兴山堇叶芥(Neomartinella xingshanensisZ.E.Zhao et Z.L.N ing)。     

植物黄酮二氢杨梅素的提纯及结晶形态研究

显齿葡萄属植物富含黄酮物质。研究对显齿葡萄黄酮提取物二氢杨梅素的提纯及结晶态进行了初步探讨。结果表明:以水作为结晶溶剂进行多次重结晶,可有效去除植物黄酮提取物的杂质,总黄酮含量由原来的86%提高至96.5%。二氢杨梅素在水相中的结晶态多为针状结晶,水相保温结晶呈放射性棒状结晶。在pH4.5的条件下,其溶解度最低可获得较高的回收率。     

KK-42对凡纳滨对虾物质储备相关酶类基因表达的影响

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玉米花生间作和磷肥对间作花生光合特性及产量的影响

揭示玉米(Zea mays)和花生(Arachis hypogaea)间作提高花生对弱光利用能力的光合特点及磷(P)肥效应, 对阐明间作花生适应弱光的光合机理和提高间作花生的产量具有重要意义。该试验于2011-2012年在河南科技大学试验农场分析了间作花生功能叶的叶绿素含量与构成、光响应曲线和CO₂响应曲线特点和荧光参数。结果表明: 与单作花生相比, 施P与不施P条件下玉米和花生间作显著(p < 0.01)提高了花生功能叶的叶绿素b含量, 降低了叶绿素a/b, 显著提高了光系统II最大光化学效率(F_v/F_m)、实际光化学效率(Φ_PSII)、光化学猝灭系数(q_P)、表观量子效率(AQY)和弱光时的光合速率, 显著降低了气孔导度、二磷酸核酮糖羧化酶羧化速率(V_cmax)、电子传递速率(J_max)和磷酸丙糖利用速率(TPU); 与不施P相比, 施P有利于提高间作花生功能叶的叶绿素含量, 显著提高了Φ_PSII、q_P、V_cmax、J_max和TPU, 说明间作花生通过提高功能叶的叶绿素b含量, 改变叶绿素构成, 提高了光系统II的F_v/F_m、Φ_PSII和q_P, 增强了对光能的捕获和转化能力, 提高了对弱光的利用能力, 而并非提高了对CO₂的羧化固定能力; 施P有利于提高间作花生对弱光的利用能力和产量, 土地当量比提高了6.2%-9.3%。     

高盐胁迫对罗布麻生长及离子平衡的影响

采用网室盆栽试验,研究了不同浓度NaCl（100～400 mmol·L^-1）胁迫30 d对罗布麻植株生物量积累、生长速率、根系活力、盐分和矿质离子吸收、分布等的影响.结果表明：100 mmol·L^-1 NaCl处理30 d,罗布麻植株鲜质量和生长速率显著下降,但对其干质量没有影响;随着盐度的增加,罗布麻植株干质量、鲜质量和生长速率均显著降低.100～200 mmol·L^-1 NaCl胁迫下,罗布麻根系活力明显高于对照;300～400 mmol·L^-1 NaCl盐胁迫下,其活力显著降低.随着盐浓度的增加,罗布麻根、茎和叶片Na⁺含量逐渐增加、K⁺含量缓慢降低;叶片Ca²⁺、Mg²⁺含量明显降低,茎部Ca²⁺和根部Mg²⁺含量有不同程度的增加.盐胁迫明显降低了罗布麻根、茎和叶片K⁺/Na⁺、Ca²⁺/Na⁺和Mg²⁺/Na⁺的比率,植株选择性吸收和运输K⁺、Ca²⁺的能力显著提高.罗布麻植株很强的拒盐能力,以及对K⁺、Ca²⁺的选择性吸收和运输是其具有高盐适应性的主要原因.     

低浓度哇巴因对负鼠肾小管上皮细胞增殖的影响

目的:用低血清培养液来模拟肾脏供血不足的营养不良状态,研究低浓度哇巴因对低血清培养下OK细胞(负鼠肾小管上皮细胞)增殖的影响。方法:用低浓度哇巴因(1-30n M)处理0.2%血清培养下OK细胞,MTT实验和Brdu掺入法检测哇巴因对OK细胞增殖的影响;Western blot检测Akt和ERK1/2的磷酸化水平;用LY294002和PD98059分别抑制PI3K/Akt和ERK1/2蛋白激酶活性,观察抑制PI3K/Akt和ERK1/2对哇巴因促进OK细胞增殖的影响。结果:低浓度哇巴因(1-30n M)促进OK细胞的增值,上调OK细胞中Akt和ERK1/2磷酸化水平。用LY294002和PD98059特异抑制Akt和ERK1/2的活化能够抑制哇巴因的促增殖作用。结论:低浓度哇巴因(1-10n M)能够促进OK细胞的增值,PI3K/Akt和ERK1/2信号通路参与哇巴因对OK细胞促增殖作用的调节。     

Abscisic acid alleviates iron deficiency by promoting root iron reutilization and transport from root to shoot in Arabidopsis

Abscisic acid (ABA) has been demonstrated to be involved in iron (Fe) homeostasis, but the underlying mechanism is largely unknown. Here, we found that Fe deficiency induced ABA accumulation rapidly (within 6 h) in the roots of Arabidopsis. Exogenous ABA at 0.5 μM decreased the amount of root apoplastic Fe bound to pectin and hemicellulose, and increased the shoot Fe content significantly, thus alleviating Fe deficiency‐induced chlorosis. Exogenous ABA promoted the secretion of phenolics to release apoplastic Fe and up‐regulated the expression of AtNRAMP3 to enhance reutilization of Fe stored in the vacuoles, leading to a higher level of soluble Fe and lower ferric–chelate reductase (FCR) activity in roots. Treatment with ABA also led to increased Fe concentrations in the xylem sap, partially because of the up‐regulation of AtFRD3, AtYSL2 and AtNAS1, genes related to long‐distance transport of Fe. Exogenous ABA could not alleviate the chlorosis of abi5 mutant resulting from the significantly low expression of AtYSL2 and low transport of Fe from root to shoot. Taken together, our data support the conclusion that ABA is involved in the reutilization and transport of Fe from root to shoot under Fe deficiency conditions in Arabidopsis.