Changes in cell structure during the formation of root aerenchyma inSAGITTARIA LANCIFOLIA (Alismataceae)

In many wetland species, root aerenchyma is produced by the predictable collapse of root cortex cells, indicating a programmed cell death (PCD). The objective of this study was to characterize the cellular changes that accompany this PCD in the marsh species Sagittaria lancifolia. Structural changes in membranes and organelles were examined during development of root cortex cells to compare with previous examples of PCD. The organization of cortical microtubule (CMT) arrays in root cells from S. lancifolia was also evaluated as a possible predictor of cell lysis. Nuclear fragmentation and condensation were the earliest changes observed in cells undergoing lysis. Breakdown of the tonoplast and other organelles and disruption of the plasma membrane followed. After loss of cytoplasm, cells collapsed to form gas spaces. These results were compared to collapse of root cortical cells of Zea mays and Oryza sativa during aerenchyma development. Changes in the appearance of the cytoplasm of all three species were similar at later stages of aerenchyma development. The relative timing of disintegration of the tonoplast and middle lamella appeared to differ among the three species. Changes in the organization of CMT arrays did not appear to be a predictor of PCD in S. lancifolia. Aerenchyma production in plants involves a type of PCD that is morphologically distinct from PCD described from many animals.     

Rhizome dynamics and resource storage in Phragmites australis

Seasonal changes in rhizome concentrations of total nonstructural carbohydrates (TNC), water soluble carbohydrates (WSC), and mineral nutrients (N, P and K) were monitored in two Phragmites australis stands in southern Sweden. Rhizome biomass, rhizome length per unit ground area, and specific weight (weight/ length ratio) of the rhizomes were monitored in one of the stands.Rhizome biomass decreased during spring, increased during summer and decreased during winter. However, changes in spring and summer were small (< 500 g DW m-2) compared to the mean rhizome biomass (approximately 3000 g DW m^–2). Winter losses were larger, approximately 1000 g DW m-2, and to a substantial extent involved structural biomass, indicating rhizome mortality. Seasonal changes in rhizome length per unit ground area revealed a rhizome mortality of about 30% during the winter period, and also indicated that an intensive period of formation of new rhizomes occurred in June.Rhizome concentrations of TNC and WSC decreased during the spring, when carbohydrates were translocated to support shoot growth. However, rhizome standing stock of TNC remained large (> 1000 g m^–2). Concentrations and standing stocks of mineral nutrients decreased during spring/ early summer and increased during summer/ fall. Only N, however, showed a pattern consistent with a spring depletion caused by translocation to shoots. This pattern indicates sufficient root uptake of P and K to support spring growth, and supports other evidence that N is generally the limiting mineral nutrient for Phragmites.The biomass data, as well as increased rhizome specific weight and TNC concentrations, clearly suggests that reloading of rhizomes with energy reserves starts in June, not towards the end of the growing season as has been suggested previously. This resource allocation strategy of Phragmites has consequences for vegetation management.Our data indicate that carbohydrate reserves are much larger than needed to support spring growth. We propose that large stores are needed to ensure establishment of spring shoots when deep water or stochastic environmental events, such as high rhizome mortality in winter or loss of spring shoots due to late season frost, increase the demand for reserves.     

不同生境条件下滨海芦苇湿地C、N、P化学计量特征

为阐明不同生境对黄河三角洲滨海芦苇湿地土壤和植物碳(C)氮(N)磷(P)含量及生态化学计量特征的影响,选取新生湿地和退耕湿地两种湿地类型为研究对象,对土壤和植物体C、N、P含量及其化学计量特征进行研究。研究表明:1)退耕芦苇湿地土壤TC、TN的含量明显增加,TP的含量变化不大。2)新生湿地和退耕湿地土壤R_(C、N、P)分别为42.6:1.6:1、71.2:2.0:1,R_(NP)低于全球平均水平(13.1)和我国平均水平(5.2),土壤表现为N限制。新生湿地土壤剖面中,R_(CN)和R_(CP)变化剧烈;R_(NP)值随深度的增加而减小;退耕湿地土壤R_(C、N、P)值规律性较好,R_(CN)随深度的增加而变大,R_(CP)和R_(NP)值随深度的增加而减小。3)新生湿地和退耕湿地中芦苇整株R_(CN)、R_(CP)和R_(NP)平均值分别为78.2、1753、22.4;67.0、1539、23.0。开垦活动可以降低芦苇植物体R_(CN)和R_(CP)值,但由于芦苇植物体本身对R_(NP)的约束性较高,对R_(NP)值的影响不大,芦苇植株R_(NP)约为23。以上结论可以为黄河三角洲国家级自然保护区正在进行的湿地保护与恢复工作提供借鉴和参考。     

退耕还湖后湿地土壤对磷的吸附解吸特性

以安徽菜子湖区不同退耕年限(3、5、9和11年)湿地为研究对象,以相邻油菜地和原始湿地为对照(共6个样地),研究退耕还湖后湿地土壤对磷的吸附解吸特性变化.结果表明: 退耕湿地土壤对磷的等温吸附曲线与Langmuir和Freundlich吸附方程拟合程度均达极显著水平(P<0.01);6个样地土壤对磷的最大吸附量(X_m)、吸附常数(K)和最大缓冲容量(MBC)范围分别为478～1074 mg·kg^-1、0.14～0.61和68.6～661.5 mg·kg^-1,且退耕湿地的这些参数均随着退耕年限的延长而升高,但未达到原始湿地水平;6个样地土壤磷的平均解吸率为6.2%～14.6%,且退耕湿地土壤磷解吸率随着退耕年限的延长呈先增高后降低的趋势,但均显著高于原始湿地.表明随着退耕年限的增加,湿地土壤对外源磷的固持能力不断增强,而土壤有机质和粘粒含量是影响湿地土壤对外源磷固持能力的重要因子.     

基于光谱指数的植物叶片叶绿素含量的估算模型

叶绿素是光合作用能力和植被发育阶段的指示器,是监测湿地植被生长健康状况的重要指标之一;高光谱遥感技术可以为植物叶绿素含量的定量化诊断提供简便有效、非破坏性的数据采集和处理方法。为保证被探测叶片面积相同,消除背景反射、叶片表面弯曲造成的光谱波动及叶片内部变异造成的影响,研究采用Field Spec 3光谱仪加载手持叶夹式叶片光谱探测器,测定野鸭湖湿地典型植物的叶片高光谱反射率数据,同时通过分光光度计室内测定相应叶片的叶绿素含量。采用相关性及单变量线性拟合分析技术,建立二者的关系模型,包括叶绿素含量与"三边"参数的相关模型以及比值光谱指数(SR)模型和归一化差值光谱指数(ND)模型,并采用交叉检验中的3K-CV方法对估算模型进行模型精度检验。结果表明:植物叶片叶绿素含量与"三边"参数大多都呈极显著相关,相关系数最大达到0.867;计算光谱反射率组成的比值(SR)和归一化(ND)光谱指数与叶绿素含量的决定系数,总体相关性比较高,较好的波段组合均为550—700nm与700—1400nm以及550—700nm与1600—1900nm,与叶绿素含量相关性最好的指数分别是SR(565nm,740nm)和ND(565nm,735nm)。并通过选取相关性最佳的光谱特征参数,分别基于"三边"参数和ND模型指数构建了植物叶片叶绿素含量的估算模型。其中,基于红边位置(WP_r)光谱特征参数和ND(565nm,735nm)光谱指数建立的叶绿素含量估算模型,取得了较好的测试效果,检验拟合方程的决定系数(R2)都达到0.8以上,估算模型分别为y=0.113x-78.74,y=5.5762x+4.4828。通过3K-CV方法进行测试和检验,植物叶绿素含量估算模型均取得了较为理想的预测精度,预测精度的分别为93.9%及90.7%。高光谱遥感技术对植被进行微弱光谱差异的定量分析,在植被遥感研究与应用中表现出强大优势,为植物叶绿素含量诊断中的实际应用提供了重要的理论依据和技术支持。     

鄱阳湖典型湿地土壤微生物活性对季节性水位变化的响应

为探究湿地土壤微生物对季节性水位变化的响应关系,以鄱阳湖湿地土壤为研究对象,在2014年3、6、10及2015年1月4个季节采集了3个不同高程样带的土壤样品,对土壤微生物基础呼吸、生物量及胞外酶等活性进行了测定。研究结果表明:(1)季节性水位变化不仅显著改变了土壤有机碳、溶解性有机碳、有效磷等含量,也使得微生物量碳和4种水解酶β-葡萄糖苷酶、β-木糖苷酶、N-乙酰氨基葡萄糖苷酶、磷酸酶活性表现出夏冬季较高、秋季最低的动态变化,而2种氧化酶酚氧化酶和过氧化氢酶的表现正好相反。(2)水位高程和地上植被类型同样对土壤微生物产生了显著影响,表现为南荻样带有较高营养元素含量和微生物活性。(3)一些土壤理化指标(含水量、铵态氮、有机碳、有效磷等)与微生物活性(微生物量、基础呼吸、酶活)显著相关;季节水位变化对微生物活性的影响大于高程差异。研究结果表明水位波动对湿地土壤微生物活性产生了重要影响,鄱阳湖水文节律的改变将影响到湿地土壤的正常生态功能。     

崇明东滩鸟类栖息地优化区越冬水鸟的栖息地利用及影响因子

阐明水鸟栖息地利用与环境因子的关系有助于制定针对性的水鸟保护对策。本研究在2012~2013年冬季对崇明东滩鸟类栖息地优化区内越冬水鸟的种类、数量以及6种环境因子(植被面积比例、裸地面积比例、水深、地形变异、栖息地结构多样性和干扰)进行调查,以了解水鸟对人工湿地的栖息地利用及其影响因子。野外调查共记录到水鸟24种9 018只,其中优势种为斑嘴鸭(Anas poecilorhyncha)和绿头鸭(A.platyrhynchos);栖息地优化区内水鸟休息的个体数量占总数量的79.2%,这表明优化区是大多数水鸟的休息地,而小(Tachybaptus ruficollis)、白骨顶(Fulica atra)、黑水鸡(Gallinula chloropus)、白琵鹭(Platalea leucorodia)和黑脸琵鹭(P.minor)的觅食个体数量超过60%,说明优化区也为这些鸟类提供了觅食地。逐步回归分析表明,裸地面积比例是影响越冬水鸟种类分布的最主要因子;尽管游禽在地形变异较大、植被面积比例较低的区域数量较多,但在休息时游禽更偏好于裸地面积比例较高的区域,而涉禽休息时偏好于地形变异较大的区域。为增加栖息地优化区内的水鸟多样性,建议在优化区内种植水鸟可食的沉水植物以增加水鸟的食物资源,同时增加裸地面积比例和地形变异程度,更好地为水鸟提供栖息地。     

Carbon uptake in Eurasian boreal forests dominates the high-latitude net ecosystem carbon budget

Arctic-boreal landscapes are experiencing profound warming, along with changes in ecosystem moisture status and disturbance from fire. This region is of global importance in terms of carbon feedbacks to climate, yet the sign (sink or source) and magnitude of the Arctic-boreal carbon budget within recent years remains highly uncertain. Here, we provide new estimates of recent (2003–2015) vegetation gross primary productivity (GPP), ecosystem respiration (R_eco), net ecosystem CO₂ exchange (NEE; R_eco − GPP), and terrestrial methane (CH₄) emissions for the Arctic-boreal zone using a satellite data-driven process-model for northern ecosystems (TCFM-Arctic), calibrated and evaluated using measurements from >60 tower eddy covariance (EC) sites. We used TCFM-Arctic to obtain daily 1-km² flux estimates and annual carbon budgets for the pan-Arctic-boreal region. Across the domain, the model indicated an overall average NEE sink of −850 Tg CO₂-C year⁻¹. Eurasian boreal zones, especially those in Siberia, contributed to a majority of the net sink. In contrast, the tundra biome was relatively carbon neutral (ranging from small sink to source). Regional CH₄ emissions from tundra and boreal wetlands (not accounting for aquatic CH₄) were estimated at 35 Tg CH₄-C year⁻¹. Accounting for additional emissions from open water aquatic bodies and from fire, using available estimates from the literature, reduced the total regional NEE sink by 21% and shifted many far northern tundra landscapes, and some boreal forests, to a net carbon source. This assessment, based on in situ observations and models, improves our understanding of the high-latitude carbon status and also indicates a continued need for integrated site-to-regional assessments to monitor the vulnerability of these ecosystems to climate change.     

Effects of Cadmium on Chlorophyll Content,Photochemical Efficiency,and Photosynthetic Intensity of Canna indica Linn.

The effects of cadmium (Cd²⁺) on growth status, chlorophyll (Chl) content, photochemical efficiency, and photosynthetic intensity were studied on Canna indica Linn. Plant specimens that were produced from a constructed wetland and precultivated hydroponically in 20 L of 1/10 Hoagland solution under greenhouse conditions for 1 week were exposed to cadmium in concentrations of 0, 0.4, 0.8, 1.6 and 3.2 mg L^―1 Cd²⁺, respectively. The results show that leaves were injured in the Cd²⁺ solution by the third day of exposure and the injury became more serious with an increase in the applied heavy metal. Under 3.2 mg L^―1 Cd²⁺ treatment, growth retardation, the decrease of chlorophyll content from 0.70 to 0.43 mg g^―1 FW, and a decrease in Chl a/b ratio from 2.0 to 1.2 were observed. Chl a was more sensitive than Chl b to Cd²⁺ stress. The decrease was the same with photochemical efficiency. Photosynthetic intensity decreased by 13.3% from 1.5×10⁴ μmol m^―2s^―1 CO₂ in control to 1.3×10⁴ μmol m^―2s^―1 CO₂ in the treatment of 3.2 mg L^―1. Because Canna species are used in heavy metal phytoremediation, these results show that C. indica can tolerate 0.4 to 0.8 mg L^―1 Cd²⁺. Therefore, it is a potential species for phytoremediation of cadmium with some limitations only at higher concentrations.