Enhanced regional terrestrial carbon uptake over Korea revealed by atmospheric CO2 measurements from 1999 to 2017

Understanding changes in terrestrial carbon balance is important to improve our knowledge of the regional carbon cycle and climate change. However, evaluating regional changes in the terrestrial carbon balance is challenging due to the lack of surface flux measurements. This study reveals that the terrestrial carbon uptake over the Republic of Korea has been enhanced from 1999 to 2017 by analyzing long‐term atmospheric CO₂ concentration measurements at the Anmyeondo Station (36.53°N, 126.32°E) located in the western coast. The influence of terrestrial carbon flux on atmospheric CO₂ concentrations (ΔCO₂) is estimated from the difference of CO₂ concentrations that were influenced by the land sector (through easterly winds) and the Yellow Sea sector (through westerly winds). We find a significant trend in ΔCO₂ of ?4.75 ppm per decade (p < .05) during the vegetation growing season (May through October), suggesting that the regional terrestrial carbon uptake has increased relative to the surrounding ocean areas. Combined analysis with satellite measured normalized difference vegetation index and gross primary production shows that the enhanced carbon uptake is associated with significant nationwide increases in vegetation and its production. Process‐based terrestrial model and inverse model simulations estimate that regional terrestrial carbon uptake increases by up to 18.9 and 8.0 Tg C for the study period, accounting for 13.4% and 5.7% of the average annual domestic carbon emissions, respectively. Atmospheric chemical transport model simulations indicate that the enhanced terrestrial carbon sink is the primary reason for the observed ΔCO₂ trend rather than anthropogenic emissions and atmospheric circulation changes. Our results highlight the fact that atmospheric CO₂ measurements could open up the possibility of detecting regional changes in the terrestrial carbon cycle even where anthropogenic emissions are not negligible.     

Variation in the phenology of photosynthesis among eastern white pine provenances in response to warming

In higher‐latitude trees, temperature and photoperiod control the beginning and end of the photosynthetically active season. Elevated temperature (ET) has advanced spring warming and delayed autumn cooling while photoperiod remains unchanged. We assessed the effects of warming on the length of the photosynthetically active season of three provenances of Pinus strobus L. seedlings from different latitudes, and evaluated the accuracy of the photochemical reflectance index (PRI) and the chlorophyll/carotenoid index (CCI) for tracking the predicted variation in spring and autumn phenology of photosynthesis among provenances. Seedlings from northern, local and southern P. strobus provenances were planted in a temperature‐free‐air‐controlled enhancement (T‐FACE) experiment and exposed to ET (+1.5/3°C; day/night). Over 18 months, we assessed photosynthetic phenology by measuring chlorophyll fluorescence, gas exchange, leaf spectral reflectance and pigment content. During autumn, all seedlings regardless of provenance followed the same sequence of phenological events with the initial downregulation of photosynthesis, followed by the modulation of non‐photochemical quenching and associated adjustments of zeaxanthin pool sizes. However, the timing of autumn downregulation differed between provenances, with delayed onset in the southern provenance (SP) and earlier onset in the northern relative to the local provenance, indicating that photoperiod at the provenance origin is a dominant factor controlling autumn phenology. Experimental warming further delayed the downregulation of photosynthesis during autumn in the SP. A provenance effect during spring was also observed but was generally not significant. The vegetation indices PRI and CCI were both effective at tracking the seasonal variations of energy partitioning in needles and the differences of carotenoid pigments indicative of the stress status of needles. These results demonstrate that PRI and CCI can be useful tools for monitoring conifer phenology and for the remote monitoring of the length of the photosynthetically active season of conifers in a changing climate.     

京津冀地区新型城镇化对土地生态效率影响的实证分析

近年来, 城市化进程的不断推进对城市土地利用及生态环境产生了极大影响。选取城镇化发展最为迅速与典型的京津冀地区作为研究区域, 采用超效率DEA模型及Malmquist效率指数, 从经济学角度分析2006-2015年土地生态效率的时空演变, 随后, 基于人口、富裕和技术(STRIPAT)模型, 构建新型城镇化发展水平的综合指标评价体系, 分析新型城镇化对土地生态效率的影响。研究结果表明: 京津冀地区城镇化发展水平与土地生态效率之间存在显著的正相关关系, 即城镇化水平的不断提升对土地生态效率的提高具有积极作用, 各城市土地生态效率在新型城镇化发展背景下存在明显的空间差异, 此外, 土地利用与管理技术水平的提高、环境政策的改变等均会对土地生态效率的提升产生积极影响。这项研究旨在为提高城市土地管理水平, 推动城市可持续发展提供决策支持。     

大豆滞绿(stay-green)突变体诱变后代表型性状变异分析

本文利用大豆滞绿突变体Z-94320经60Co-γ射线诱变的突变体后代M5、M6代为材料,进行两年的田间性状观察记录统计,用相关性分析、主成分分析、聚类分析对其17个主要表型性状统计分析。结果表明:诱变后代产生了丰富的变异,出现了多种种皮色和子叶色,产生了非滞绿性状,形成了各种生育周期,且分离出晚熟性状。通过相关性分析发现,单株粒重与株重、茎粗、主茎荚数、分枝荚数、一粒荚数、二粒荚数、三粒荚数、瘪粒荚数、虫食数呈极显著正相关,这些性状可以对产量进行预测;主成分分析在M5代提取出“产量因子”、“株型因子”、“粒荚因子”、“茎荚因子”四个主成分,对农艺性状累计贡献率达到70.50%,M6代提取出“产量因子”、“虫害因子”、“株型因子”、“茎杆因子”四个主成分,对农艺性状累计贡献率达到71.54%;聚类分析将M5、M6代材料分别划分为6类,发现同代中各类群农艺性状情况大致相似,但是各农艺性状在两代之间的变化明显,在株重、结荚高度、单株粒重等方面M6代显著高于M5代,并筛选出两株高产品系和一株特色滞绿品系。本研究逐步完善了对滞绿大豆突变体库的构建,为滞绿大豆诱变后代的遗传多样性研究提供了基础的数据分析。     

CaСl2 Salt Signaling in Primary Root Architecture and Lateral Root Emergence in Arabidopsis thaliana

Russian Journal of Plant Physiology - Plant root architecture modulates during developmental stages and adjusts with the environmental condition. The cytosolic calcium which is a ubiquitous...