秦岭南坡松栎林群落演替过程中种间联结性和相关性研究

为了揭示秦岭南坡松栎林群落动态变化过程中物种间关系与群落演替的相互作用,基于2×2列联表,采用方差比率法、χ2检验、Jaccard指数和Spearman秩相关性系数探讨了油松林→松栎混交林→锐齿栎林演替序列过程中3个演替阶段群落优势种群的种间联结性和相关性。结果表明:(1)油松林、松栎混交林和锐齿栎林群落总体联结性均为显著正联结,各自具有相对的稳定性。(2)油松和松栎混交林群落正负联结性和相关性比例较小,群落稳定性均低于锐齿栎林群落。(3)先锋种间及其与前期过渡种间、顶级种间及其与后期过渡种间竞争较为激烈,过渡种间(包括前期过渡种间、前期过渡种与后期过渡种间、后期过渡种间)正联结占优势,较为稳定。(4)不同演替阶段群落可分别划分为4个、5个、4个生态种组。研究认为,秦岭南坡松栎混交林演替过程中种间关系逐渐趋于稳定共存,实践中及时调整种间关系可促使秦岭南坡松栎林群落趋于健康稳定,有效缩短演替的进程。     

公路碾压干扰下群落植物多样性——以藏北矮嵩草草甸为例

运用时空替换法,以空间变换替代时间变换,对公路碾压干扰下藏北矮嵩草草甸恢复演替中不同阶段群落植物多样性进行研究.结果表明：各草地群落样方中共出现高等植物33种,其中菊、豆、禾本科和蔷薇科合计16种,占48.48﹪,在其自然恢复演替所起的作用最大;莎草科植物作为顶级群落的建群种具有重要作用.物种构成具有明显的阶段性特征：演替前期以1年生和2年生植物为主;中期多年生草本植物逐渐占据优势;后期矮嵩草成为单优势种;菊叶萎陵菜和二裂萎陵菜几乎贯穿始终.物种积聚主要是在演替前期和中期完成,其积聚过程符合二次曲线.演替后期群落植物多样性程度最高,多样性随演替进程表现为逻辑斯谛增长规律：前期群落物种丰富度较低,均匀度较高,生态优势度？也比较高,但综合多样性较低;中期群落的均匀度下降,生态优势度也同时下降,综合多样性高;后期矮嵩草成为群落的单优势种,群落的均匀度和生态优势度均下降,综合多样性仍然增加.     

山西文峪河上游河岸林的土壤种子库与树种更新特征

以山西文峪河上游13种典型的河岸林为研究对象,通过土壤种子库和树种更新研究,分析群落种子库与林下更新随演替进展的变化趋势,以及该区河岸树种的繁殖对策。结果表明：13种群落的土壤种子库密度间于1290±103～3950±154粒/m2,63.5%的种子留存于0～5 cm的层次;种子库包含49种植物,以多年生草本为主,存在耐干扰种和湿地植物的种子;处于相同或相邻演替阶段的群落,种子库相似性较高;随演替进展,种子库密度、丰度、Shannon-Wiener指数及种子库与地上植被的相似性均呈降低趋势;处于演替后期的青杄Picea wilsonii林存在丰富的＂青杄幼苗库＂;先锋种白桦Betula platyphylla的种子存在于演替各阶段的群落中,储量丰富,其更新主要依赖于风媒种子,并存在少量萌蘖;青杄、白杄P.meyeri、华北落叶松Larix principis-rupprechtii、油松Pi-nus tabulaeformis和辽东栎Quercus liaotongensis的种子库损耗严重,没有或仅存少量种子,其中云杉和油松的更新幼苗幼树多,属持久幼苗库更新;华北落叶松幼苗幼树少,且仅出现于林缘或林窗等开阔地,属植被空隙中季节性更新;辽东栎主要依赖丰富的幼苗库进行更新,同时存在一定的萌蘖;青杨Populus cathayana以大量风媒种子更新结合营养扩展。     

海南岛吊罗山热带山地雨林两个演替阶段的种间联结性

种间联结一直是群落演替理论研究的焦点之一, 关于物种间相互作用与群落演替之间的动态关系仍然存在争议。本文中, 作者通过出现-不出现数据的方差比例、基于2×2列联表的种间联结分析和 ²检验, 对海南岛吊罗山热带山地雨林演替前期和演替后期群落的种间联结性进行了研究, 以揭示种间联结与群落演替的相互作用。结果表明: (1)在演替前期, 群落内所有树种间总体呈正联结, 但不显著; 发展至演替后期达到显著正联结。群落内所有物种间正、负联结种对数占总种对数的比例随演替进程呈现下降趋势, 而无联结种对数的比例则大幅上升; 优势种和伴生种间呈现相同的趋势。这表明群落演替正朝着有利于物种稳定共存的方向发展。(2)演替前期建群种和后期侵入种间正联结与无联结种对数的比例(分别为37.8%与41.5%)远大于负联结的比例(20.7%), 但正联结均不显著; 前期定居树种和后期侵入种通过分割资源而共存, 而且也趋于独立存在。(3)后期侵入种间不存在负联结, 所有正联结(占总对数的33.3%)均达显著水平, 显示它们对生境有相似的适应和相互重叠的生态位。     

中亚热带常绿阔叶林不同演替阶段土壤活性有机碳含量及季节动态

为探明不同演替阶段土壤碳吸存潜力,选取演替时间为15a(演替初期)、47a(演替中期)、110a(演替后期)3个中亚热带常绿阔叶林,分析了各演替阶段的土壤有机碳(SOC)含量以及土壤微生物量碳(MBC)、可溶性碳(DOC)和微生物熵(SMQ)的季节变化。结果表明:演替中、后期不同土层的土壤SOC、MBC、DOC含量和SMQ均显著高于演替初期(P<0.05);与演替中期相比,演替后期土壤MBC、DOC含量有所降低,SOC含量和SMQ无显著差异。土壤SOC、MBC和DOC含量随土层加深而显著性降低(演替初、中期DOC除外),并随演替进行逐渐向腐殖质层富集。不同演替阶段MBC、DOC和SMQ均有显著季节变化,最低值出现在秋季,最高值随演替进程由冬季逐步转向夏季。相关分析表明,不同演替阶段土壤活性有机碳含量与土壤有机碳含量极显著相关(P<0.01),且土壤活性有机碳(MBC、DOC)和SMQ对土壤碳库变化更为敏感。     

千岛湖次生林优势种植物光合特性对不同光环境的响应

在林窗、林缘、林下3种自然光环境下,对千岛湖次生林优势种马尾松、苦槠、石栎和青冈栎在不同季节的光合作用日变化、光响应、CO2响应和叶绿素荧光参数进行比较,探讨优势种对光环境的适应及响应的差异,以期了解群落演替的内在机制.结果表明:在3种光环境下,马尾松、苦槠的日均净光合速率(Pn)为夏季最高,石栎、青冈栎为秋季最高.在林窗、林缘中,年均最大净光合速率(Amax)、光饱和点(LSP)、光补偿点(LCP)、暗呼吸速率(Rd)均为马尾松最高,苦槠次之,青冈栎和石栎最低;林下生境中,青冈栎的年均Amax、表观量子效率(AQY)最高,其次是石栎和苦槠,马尾松最低.3种生境中,马尾松的年均最大羧化速率(Vc max)、最大电子传递速率(Jmax)和磷酸丙糖利用率(TPU)均显著高于其他3种优势种.马尾松、苦槠4个季节的PSII最大光化学效率(Fv/Fm)均为林窗最高,石栎、青冈栎为林下最高;马尾松、苦槠的Fv/Fm最大值出现在夏季,石栎、青冈栎出现在秋季.马尾松、苦槠更适合生长于林窗等高光强生境中,而石栎、青冈栎在林下等低光强生境中生长较好.随着演替的进程,群落郁闭度增大,石栎和青冈栎将取代马尾松和苦槠成为群落演替顶极阶段的优势种.     

草原群落退化演替过程中微斑块土壤碳氮的空间异质动态

微斑块变化是草原退化过程中的活跃成分。分析了呼伦贝尔克氏针茅草原逆行演替过程中微斑块土壤全碳、全氮和碱解氮含量的空间异质性,提出了"养分聚集效应"的概念。研究结果表明:随着群落退化演替的加剧,土壤全碳、全氮和碱解氮的含量均表现为演替前期演替后期演替中期(P0.05)。从土壤全碳、全氮和碱解氮的变异系数和变异函数综合分析来看,10 cm×10 cm微尺度上,草原退化演替过程中土壤全碳、全氮和碱解氮的空间异质性具有明显的不一致性;全碳的空间异质性表现为演替中期演替前期演替后期,全氮表现为演替后期演替前期演替中期,碱解氮表现为演替中期演替后期演替前期。草原退化过程中土壤养分在微斑块上的富积和迁移表现出尺度依赖性和变异性。     

秦岭山地油松群落更新特征及影响因子

采用样方法,对秦岭山地油松次生林群落更新特性和相关环境因子进行了研究.结果表明:油松次生林更新层乔木树种共36种,占总种数的51.4%;优势种有短柄枹栎、锐齿栎和榛子等;幼苗库丰富,高度级及龄级较小;更新方式以实生为主,该森林群落处于演替中期、林分密度对林下乔木幼苗、幼树数量影响极显著(P<0.01),当林分密度从580株.hm-2增加到1500株.hm-2时,林下更新的幼苗、幼树密度呈增加趋势,随着林分密度的继续增加,其密度逐渐减少;坡向对幼苗、幼树密度的影响显著(P<0.05),当坡向由南偏西10°到南偏西40°,林下幼树密度逐渐减少,至阴坡(北偏东10°)幼树数量又逐渐增加.不同坡位林分更新特征各异,平坡林分中幼苗、幼树密度均较大;从坡下向上,幼苗密度逐渐减少,而幼树密度逐渐增大;海拔从1159 m增至1449 m,幼树密度逐渐增加,至1658 m时,幼树密度逐渐减小,而幼苗密度则一直呈现增加趋势.处于阴坡的中密度林分更新效果最佳.合理调整林分密度是加快林分更新的有效途径之一.     

中亚热带森林群落不同演替阶段优势种凋落物分解试验

选择我国亚热带森林群落3个主要演替阶段的7个优势种（其中马尾松代表演替初期优势种,木荷和香樟代表演替中期优势种,甜槠、小叶青冈栎、青冈和乐昌含笑代表演替后期优势种）的凋落物,采用网袋法进行分解试验. 结果表明:马尾松凋落物分解得最慢,年分解速率为0.51;木荷和香樟居中,分别为0.55和0.61;小叶青冈栎和乐昌含笑分解得最快,分别为0.89和1.12.沿着植被顺向演替的梯度,凋落物分解速度呈现加快的趋势. 分解速率同凋落物的初始P、N和木质素含量及木质素/N比值呈极显著相关(P<0.01),同C/N比值有显著相关关系(P<0.05).凋落物的P、N和木质素含量及木质素/N比值是预测凋落物分解快慢的良好指标.     

长白山森林不同演替阶段比叶面积及其影响因子

比叶面积(SLA)是植物功能性状的重要指标,反映了植物生长过程中资源收获策略。以长白山森林演替过程中4个阶段的典型群落为研究对象,分析了不同演替阶段比叶面积的差异及影响因素。结果表明:比叶面积随演替的发生进行呈现明显增加趋势,且差异显著(P0.05)。相关分析结果表明,比叶面积与海拔、坡位和土壤氮含量均呈显著正相关关系,与其他影响因子无显著相关关系。进一步的通径分析结果表明,演替前期坡位是主要的影响因素,演替中期模型解释度不高,各通径系数较小,演替后期土壤氮含量对比叶面积的作用凸显。     

长期施肥下红壤性水稻土有机碳储量变化特

研究了1982—2012年长期不同施肥下红壤性水稻土土壤有机碳含量变化、固碳趋势及外源碳输入对土壤固碳的贡献.结果表明： 施肥能提高土壤有机碳含量,连续30年不同施肥后,各施肥处理土壤有机碳含量趋于稳定,有机无机配施的土壤有机碳含量为21.02～21.24 g·kg^-1,增加速率为0.41～0.59 g·kg^-1·a^-1,单施化肥的土壤有机碳含量为15.48 g·kg^-1.各有机无机肥配施处理土壤的平均有机碳储量为43.61～48.43 t C·hm^-2,历年平均土壤有机碳储量显著大于单施化肥处理.土壤固碳速率与年均投入碳量呈显著指数正相关.本试验条件下,每年需要增加外源有机碳为0.12 t C·hm^-2才能维持土壤有机碳的平衡.     

Dynamics of soil organic carbon storage following restoration of grassland on Yunwu Mountain

Grassland recovery and reconstruction are critical to ecological restoration in the Chinese Loess Plateau (CLP). Investigating changes in soil organic carbon density (SOCD), soil organic carbon (SOC) storage, and the rate of SOC sequestration is very important to assess the effect of ecological recovery and estimate the capacity of soil carbon sequestration. Here, we present the data of SOCD, SOC storage, and SOC sequestration rate from grasslands conversion from farmlands in the CLP. Our results indicate that: (1) The average SOCD (0–100 cm) in sites continued cultivation (CC), cultivation abandonment at 1999 (AC-99) and cultivation abandonment at 1989 (AC-89) is 6.00, 21.64 and 22.23 kg m^?2, respectively. SOCD in sites AC-99 and AC-89 is significantly higher than that in site CC and the average SOCD of China (10.53 kg m^?2), which indicates that vegetation restoration is benefit to increase soil carbon storage as well as preserve soil and water in this area. (2) The SOC storage (0–100 cm) in sites CC, AC-99 and AC-89 is 60.02, 216.35 and 222.32 kg m^?2, respectively. Results of ANOVA indicate that SOC storage of AC-99 is significantly higher than that of CC, while SOC storage of AC-89 is significantly higher than that of AC-99 at the depth of 0–50 cm (P < 0.001). It suggests that the capability of soil carbon sequestration increases after vegetation restoration, which is mainly due to the increase of plant roots. (3) The rate of SOC sequestration varies at different depths, which is high at the depth of 0–50 cm while low at the depth of 50–100 cm. This is probably due to the accumulation of plant root in the surface layer, which is the main controlling factor of SOC in this area. Our results indicate that the SOCD and SOC storage increase with vegetation restoration in our study site significantly.     

Dynamics of soil organic carbon storage following restoration of grassland on Yunwu Mountain

Grassland recovery and reconstruction are critical to ecological restoration in the Chinese Loess Plateau (CLP). Investigating changes in soil organic carbon density (SOCD), soil organic carbon (SOC) storage, and the rate of SOC sequestration is very important to assess the effect of ecological recovery and estimate the capacity of soil carbon sequestration. Here, we present the data of SOCD, SOC storage, and SOC sequestration rate from grasslands conversion from farmlands in the CLP. Our results indicate that: (1) The average SOCD (0–100 cm) in sites continued cultivation (CC), cultivation abandonment at 1999 (AC-99) and cultivation abandonment at 1989 (AC-89) is 6.00, 21.64 and 22.23 kg m^?2, respectively. SOCD in sites AC-99 and AC-89 is significantly higher than that in site CC and the average SOCD of China (10.53 kg m^?2), which indicates that vegetation restoration is benefit to increase soil carbon storage as well as preserve soil and water in this area. (2) The SOC storage (0–100 cm) in sites CC, AC-99 and AC-89 is 60.02, 216.35 and 222.32 kg m^?2, respectively. Results of ANOVA indicate that SOC storage of AC-99 is significantly higher than that of CC, while SOC storage of AC-89 is significantly higher than that of AC-99 at the depth of 0–50 cm (P < 0.001). It suggests that the capability of soil carbon sequestration increases after vegetation restoration, which is mainly due to the increase of plant roots. (3) The rate of SOC sequestration varies at different depths, which is high at the depth of 0–50 cm while low at the depth of 50–100 cm. This is probably due to the accumulation of plant root in the surface layer, which is the main controlling factor of SOC in this area. Our results indicate that the SOCD and SOC storage increase with vegetation restoration in our study site significantly.     

Variable temperature sensitivity of soil organic carbon in North American forests

We investigated mean residence time (MRT) for soil organic carbon (SOC) sampled from paired hardwood and pine forests located along a 22 °C mean annual temperature (MAT) gradient in North America. We used acid hydrolysis fractionation, radiocarbon analyses, long-term laboratory incubations (525-d), and a three-pool model to describe the size and kinetics of the acid insoluble C (AIC), active and slow SOC fractions in soil. We found that active SOC was 2 ± 0.2% (mean ± SE) of total SOC, with an MRT of 33 ± 6 days that decreased strongly with increasing MAT. In contrast, MRT for slow SOC and AIC (70 ± 6% and 27 ± 6% of total SOC, respectively) ranged from decades to thousands of years, and neither was significantly related to MAT. The accumulation of AIC (as a percent of total SOC) was greater in hardwood than pine stands (36% and 21%, respectively) although the MRT for AIC was longer in pine stands. Based on these results, we suggest that the responsiveness of most SOC decomposition in upland forests to global warming will be less than currently modeled, but any shifts in vegetation from hardwood to pine may alter the size and MRT of SOC fractions.     

Modeling the impact of store-operated Ca2+ entry on intracellular Ca2+ oscillations

Calcium (Ca2+) oscillations play fundamental roles in various cell signaling processes and have been the subject of numerous modeling studies. Here we have implemented a general mathematical model to simulate the impact of store-operated Ca2+ entry on intracellular Ca2+ oscillations. In addition, we have compared two different models of the inositol 1,4,5-trisphosphate (IP3) receptor (IP3R) and their influences on intracellular Ca2+ oscillations. Store-operated Ca2+ entry following Ca2+ depletion of endoplasmic reticulum (ER) is an important component of Ca2+ signaling. We have developed a phenomenological model of store-operated Ca2+ entry via store-operated Ca2+ (SOC) channels, which are activated upon ER Ca2+ depletion. The depletion evokes a bi-phasic Ca2+ signal, which is also produced in our mathematical model. The IP3R is an important regulator of intracellular Ca2+ signals. This IP3 sensitive Ca2+ channel is also regulated by Ca2+. We apply two IP3R models, the Mak-McBride-Foskett model and the De Young and Keizer model, with significantly different channel characteristics. Our results show that the two separate IP3R models evoke intracellular Ca2+ oscillations with different frequencies and amplitudes. Store-operated Ca2+ entry affects the oscillatory behavior of these intracellular Ca2+ oscillations. The IP3 threshold is altered when store-operated Ca2+ entry is excluded from the model. Frequencies and amplitudes of intracellular Ca2+ oscillations are also altered without store-operated Ca2+ entry. Under certain conditions, when intracellular Ca2+ oscillations are absent, excluding store-operated Ca2+ entry induces an oscillatory response. These findings increase knowledge concerning store-operated Ca2+ entry and its impact on intracellular Ca2+ oscillations.     

Soil carbon stocks in stable tropical landforms are dominated by geochemical controls and not by land use

Soil organic carbon (SOC) dynamics depend on soil properties derived from the geoclimatic conditions under which soils develop and are in many cases modified by land conversion. However, SOC stabilization and the responses of SOC to land use change are not well constrained in deeply weathered tropical soils, which are dominated by less reactive minerals than those in temperate regions. Along a gradient of geochemically distinct soil parent materials, we investigated differences in SOC stocks and SOC (Δ¹⁴C) turnover time across soil profile depth between montane tropical forest and cropland situated on flat, non-erosive plateau landforms. We show that SOC stocks and soil Δ¹⁴C patterns do not differ significantly with land use, but that differences in SOC can be explained by the physicochemical properties of soils. More specifically, labile organo-mineral associations in combination with exchangeable base cations were identified as the dominating controls over soil C stocks and turnover. We argue that due to their long weathering history, the investigated tropical soils do not provide enough reactive minerals for the stabilization of C input in either high input (tropical forest) or low-input (cropland) systems. Since these soils exceeded their maximum potential for the mineral related stabilization of SOC, potential positive effects of reforestation on tropical SOC storage are most likely limited to minor differences in topsoil without major impacts on subsoil C stocks. Hence, in deeply weathered soils, increasing C inputs may lead to the accumulation of a larger readily available SOC pool, but does not contribute to long-term SOC stabilization.     

土壤有机碳形成机制的探索历程

土壤有机碳(SOC)是生态系统的重要资产,在全球碳平衡中发挥着关键的作用。2015年巴黎气候会议以来,促进SOC在陆地生态系统中的积累受到特别重视,被认为是有效减缓大气CO2浓度上升的最重要地表措施。从服务于这个目标出发,对过去几十年全球在探索SOC形成机制上的历程进行了回顾和总结,从弄清SOC全球分布规律,阐明样地以下尺度的SOC循环过程及其相应的物理、化学与生物机理,到样地及以上尺度的土壤固碳机制,最后给出了成熟森林SOC积累机制的实例。SOC形成机制的探索历程就是寻求为促进土壤固碳提供理论指导的过程。     

鼎湖山3种演替阶段森林土壤C、N、P现状及动态

为探讨森林演替过程中土壤C、N、P的变化,通过测定鼎湖山3种演替阶段的森林土壤有机碳(SOC)、总氮(TN)、总磷(TP)含量,对他们的化学计量进行分析。结果表明,鼎湖山3种森林土壤SOC和TN随演替阶段而增加,演替中后期表层土壤(0~20 cm)与演替初期的差异达到显著水平(P0.05),在土壤剖面上的分布都呈现显著的表层富集现象,且表层土壤与其他土层均有显著差异(P0.05)。土壤TP含量随演替阶段没有呈现出有规律的变化,不同演替阶段间也没有显著差异,但不同演替阶段土壤TP在土壤剖面上的分布表现不同,演替前期土壤TP含量随着土层深度增加而增加,演替后期土壤TP随土层深度的增加而降低,而演替中期土壤TP含量在各土层间没有显著差异。土壤C∶N不受土层深度和演替进程的影响,而土壤C∶P和N∶P均表现为随演替阶段而增加,随土层加深而降低。这些揭示了森林土壤SOC、TN和TP含量随演替进展及其在土壤剖面上的分布取决于土壤C、N、P的来源方式。