Aneuploidy and polyploidization in haploid tissue cultures of Larix decidua

Haploid embryogenic lines of Larix decidua which had been maintained on medium free of plant growth regulatiors were screened for chromosomal abnormalities. Chromosome squashes were prepared from fast-growing suspension culture. alternatively, a method using burst protoplasts was devised for improving chromosome spreads. One line showed polyploidization with chromosome mumbers ranging from haploid to tetraploid. This line is presently predominantly diploid. Aneuploidization also occurred. The most effective method for counting chromosomes was from burst protoplasts. It is recommended that long-term cultures of conifer tissues be checked for genetic stability.     

Carbon cycle of larch plantation based on CO2FIX model

Aims
Plantations play important roles in modifying regional carbon budget and maintaining regional carbon balance. In this study, we assessed larch plantation (Larix gmelinii var. principis-rupprechtii) carbon dynamics in Weichang County from a perspective of the forest biomass-soil-wood-products chain. Our objectives were to elucidate the carbon sink capacity of larch plantation and the influences of biomass, soil and wood product pools on carbon balance.
Methods
CO2FIX model was used to evaluate the carbon storage and flow of larch plantation over a time span of 120 years. Input data for model were derived from practical investigations and published papers. We validated the simulated results and found that this model was suitable in the region and the simulated results were reliable.
Important findings
(1) Soil was the largest carbon pool for larch plantation and the wood product pool had the smallest carbon storage. Meanwhile, carbon storage in wood products gradually increased with time. (2) In a rotation of 50 years from secondary poplar-birch forest to larch plantation, 250 t C·hm^-2 was sequestrated by the larch plantation. 70% of the carbon was transferred into soil in the form of litter and logging slash and the other 30% was transferred into wood products. (3) Larch plantation was a carbon sink during most of its growing period and turned to temporary carbon source when it was harvested. Larch plantation could sequestrate about 0.3 t C·hm^-2·a^-1 in the long term. Our results indicated the importance of wood product carbon pool in carbon dynamics of plantation, which facilitated our understanding in the carbon dynamics and capacity of plantation.     

供氮水平对落叶松幼苗光合作用的影响

为探讨落叶松光合作用对外界供氮环境变化的响应规律,采用砂培方法在温室内设置了4种供氮浓度(1、4、8mmol/L和16mmol/L),对生长在不同供氮水平下落叶松(Larixgmelinii)1年生幼苗的气体交换参数、叶绿素荧光参数以及一些生化指标进行了测定。结果显示,随供氮水平的提高,落叶松幼苗针叶氮含量、叶绿素含量、类胡罗卜素含量、可溶性蛋白(TSP)含量和光饱和净光合速率(Pmax)均显著增加,同时伴随着叶磷含量和胞间与外界CO2浓度之比(Ci/Ca)的降低。然而,当供氮水平超过8mmol/L增至16mmol/L时,TSP含量及Pmax不再增加,反而略有下降。供氮不足显著降低了幼苗针叶光系统最大光能转换效率(Fv/Fm)、光系统量子效率(ΦPS)和光化学猝灭系数(qP),却增加了非光化学猝灭系数(NPQ)。而增加供氮可使Fv/Fm和ΦPS回升,同时qP升高,NPQ下降,但当供氮水平超过8mmol/L后,各叶绿素荧光参数变化幅度较小。结果表明,增加供氮可显著提高落叶松幼苗的光合能力,增加光系统天线色素捕获的光能用于光化学电子传递的份额,减缓光抑制。然而,16mmol/L已经超过落叶松幼苗最适的供氮水平,过量供氮引起的负面效应可能主要与过低的叶磷含量导致的营养失衡有关。     

Plant response to climate change along the forest‐tundra ecotone in northeastern Siberia

Russia's boreal (taiga) biome will likely contract sharply and shift northward in response to 21st century climatic change, yet few studies have examined plant response to climatic variability along the northern margin. We quantified climate dynamics, trends in plant growth, and growth–climate relationships across the tundra shrublands and Cajander larch (Larix cajanderi Mayr.) woodlands of the Kolyma river basin (657 000 km²) in northeastern Siberia using satellite‐derived normalized difference vegetation indices (NDVI), tree ring‐width measurements, and climate data. Mean summer temperatures (T_s) increased 1.0 °C from 1938 to 2009, though there was no trend (P > 0.05) in growing year precipitation or climate moisture index (CMI_gy). Mean summer NDVI (NDVI_s) increased significantly from 1982 to 2010 across 20% of the watershed, primarily in cold, shrub‐dominated areas. NDVI_s positively correlated (P < 0.05) with T_s across 56% of the watershed (r = 0.52 ± 0.09, mean ± SD), principally in cold areas, and with CMI_gy across 9% of the watershed (r = 0.45 ± 0.06), largely in warm areas. Larch ring‐width measurements from nine sites revealed that year‐to‐year (i.e., high‐frequency) variation in growth positively correlated (P < 0.05) with June temperature (r = 0.40) and prior summer CMI (r = 0.40) from 1938 to 2007. An unexplained multi‐decadal (i.e., low‐frequency) decline in annual basal area increment (BAI) occurred following the mid‐20th century, but over the NDVI record there was no trend in mean BAI (P > 0.05), which significantly correlated with NDVI_s (r = 0.44, P < 0.05, 1982–2007). Both satellite and tree‐ring analyses indicated that plant growth was constrained by both low temperatures and limited moisture availability and, furthermore, that warming enhanced growth. Impacts of future climatic change on forests near treeline in Arctic Russia will likely be influenced by shifts in both temperature and moisture, which implies that projections of future forest distribution and productivity in this area should take into account the interactions of energy and moisture limitations.     

抚育间伐对长白落叶松人工林土壤碳、氮及其组分的影响

抚育间伐作为重要的森林经营措施之一,能够改变林分结构和稳定性,进而影响森林生态系统的生物地球化学循环.然而,抚育间伐对森林土壤碳、氮循环的影响程度如何尚不明确,尤其缺少长期试验结果报道.本研究以黑龙江省孟家岗林场经过4种不同强度和频度的抚育间伐处理后的60年生长白落叶松人工林为研究对象(4次低强度的间伐,LT4;3次中等强度的间伐,MT3;2次高强度间伐,HT2;不进行间伐的对照,CK),从酸水解法划分土壤碳、氮库(活性碳、氮库Ⅰ,活性碳、氮库Ⅱ和惰性碳、氮库)的角度研究了抚育间伐对长白落叶松人工林土壤总有机碳、全氮的影响机制.结果表明: 抚育间伐显著增加了土壤有机碳和全氮含量,增幅分别高达48.7%～50.3%和28.9%～42.7%.抚育间伐均增加了3种碳、氮组分的含量,而增加的程度因碳、氮组分和抚育间伐措施的不同而异.与活性碳库Ⅰ和活性碳库Ⅱ的增加程度相比,惰性碳库的增加程度最大,LT4、MT3和HT2处理下惰性碳库分别增加71%、69%和75%.此外,抚育间伐也显著增加了惰性碳占土壤总有机碳的比例.LT4显著提高了土壤微生物生物量碳、氮含量和微生物熵,而MT3和HT2对微生物生物量碳、氮和微生物熵却无显著影响.抚育间伐可能通过产生较多的粗木质残体于土体中,增加土壤木栓质和木质素等顽固组分的输入,进而导致土壤惰性碳含量增加,降低有机质的分解,最终导致土壤有机碳增加.     

Soil Carbon Changes Following Afforestation with Olga Bay Larch （Larix olgensis Henry） in Northeastern China

After converting cropland to forest, carbon Is sequestered in the aggradlng blomass of the new forests, but the question remains, to what extent will the former arable soil contribute as a sink for CO2？ Quantifying changes In soil carbon Is an Important consideration In the large-scale conversion of cropland to forest. Extensive field studies were undertaken to Identify a number of suitable sites for comparison of soil properties under pasture and forest. The present paper describes results from a study of the effects of first rotation larch on soil carbon In seven stands In an afforestation chronosequence compared with adjacent Korean pine, pasture, and cropland. An adjacent 250-year-old natural forest was Included to give Information on the possible long-term changes In soil carbon In northeast China In 2004. Soil carbon Initially decreased during the first 12 yr before a gradual recovery and accumulation of soil carbon occurred. The Initial （0-12 yr） decrease In soil carbon was an average 1.2% per year among case studies, whereas the Increase In soil carbon （12-33 yr） was 1.90% per year. Together with the carbon sequestration of forest floors, this led to total soil carbon stores of approximately 101.83 Mg/hm^2 over the 33-year chronosequence. Within the relatively short time span, carbon sequestration occurred mainly In tree blomees, whereas soil carbon stores were clearly higher In the 250-year-old plantation （184 Mg/hm^2）. The ongoing redistribution of mineral soil carbon In the young stands and the higher soil carbon contents In the 250-year-old afforested stand suggest that nutrient-rich afforestation soils may become greater sinks for carbon （C） In the long term.     

火灾恢复年限对大兴安岭森林乔灌草多样性及优势种影响

林火是大兴安岭地区森林生态系统的重要影响因子,研究火灾对植物多样性和优势种多度长期影响,有助于火灾区域森林生态系统重建与管理。本研究以大兴安岭不同火烧年限（1~5、5~10、10~20、20~30、30~40和40~50年）48对配对样地（火烧样地与邻近未火烧对照样地）为研究对象,利用二者差值变化来探讨森林恢复年限对植物多样性指数影响,通过对乔灌草相对多度变化确认火灾恢复对优势种的影响。研究结果表明：（1）火烧与对照间乔木多样性和丰富度差值先降后升趋势,在10年左右最低,而恢复30~40年后与对照样地相当或更高。灌木与乔木变化趋势相似,但是变化趋势多达到统计学显著（P<0.05）,灌木Shannon-wiener多样性指数和丰富度差值随年限增加而线性上升。草本Simpson多样性指数随火烧年限增加而直线下降,但是均匀度与丰富度没有出现线性变化。（2）乔灌草优势种变化趋势为：乔木层白桦（Betula platyphylla）在火烧5~30年占比均超过30%,在30年后占比不超过15%,同时兴安落叶松（Larix gmelinii）在30~40年占比超过50%;灌木层在0~30年均是越桔（Vaccinium vitis-idaea）占比最大,30年之后变为榛子（Corylus heterophylla）,草本层5~30年均是小叶章（Deyeuxia angustifolia）占比最大,30年之后变为其他物种。对照样地乔木层主要是兴安落叶松,占比超过50%,灌木层主要是越桔（Vaccinium vitis-idaea）,草本层主要是小叶章（Deyeuxia angustifolia）。整体来看,乔木火后恢复需要更长的时间,而灌木和草本火后恢复更快。植物多样性及优势种变化是研究其对生态服务功能（如碳汇）影响的基础,我们研究结果为天保工程后续实施及科学管理大兴安岭森林生态系统提供数据支撑。     

Structural and functional organization of a larch phytocenosis in a postfire progressive succession in the north of Central Siberia

The author considers specific features of the postfire formation of a larch (Larix gmelinii) phytocenosis in Central Evenkia, the north of Central Siberia. Morphological parameters of trees, structure, height, growth, and biological productivity of the tree stand, shrub layer, live ground cover, and accumulation of detritus after progressive pyrogene succession are analyzed and discussed.     

Ecophysiological responses of the larch species in northern Japan to environmental changes as a basis for afforestation

For sustainable use and suitable management of larch plantations, we must clarify the ecophysiological responses of larch species to environmental changes. The physical environment has been changing dramatically, e.g., increase in atmospheric CO₂ concentration ([CO₂]), nitrogen (N) deposition, and atmospheric ozone concentration ([O₃]), and these changes may negatively affect growth of larch species. This review summarizes the previous experimental studies on the ecophysiological responses of larch species to elevated [CO₂], soil acidification, elevated [O₃], and N load. Based on the advanced studies, although elevated [CO₂] will stimulate the productivity of larch, increase of [O₃] and severe soil acidification will reduce it. Increase of N deposition, at least, will not negatively affect larch productivity. Finally, we propose the future direction for investigation to understand the mechanism of the responses of larch species and to predict the associated risk.