闽江河口春季互花米草入侵过程对短叶茳芏沼泽土壤碳氮分布特征的影响

2014年4月,选择闽江口鳝鱼滩湿地中未被入侵的短叶茳芏群落(A)、互花米草入侵斑块边缘(B)以及互花米草入侵斑块中央(C)为研究对象,基于时空互代研究方法,探讨了互花米草入侵序列下湿地土壤碳氮空间分布特征的差异。结果表明,互花米草入侵显著降低了土壤的NO_3~--N含量(P0.05),但整体增加了NH_4~+-N含量,这与其入侵后导致湿地土壤颗粒组成发生显著变化(砂砾含量增加33.81%),进而促进了土壤的矿化作用和硝化作用,并有助于硝态氮的垂直淋失有关。互花米草入侵整体增加了土壤的碳氮含量和C/N比,与入侵进程和入侵前相比,互花米草入侵后湿地土壤的碳储量分别增加了8.73%和24.37%,氮储量则分别增加了10.22%和17.87%,这主要与其对闽江口湿地植物群落格局、养分生物循环以及强促淤作用引起的土壤颗粒组成等显著改变有关。研究发现,闽江口互花米草入侵对短叶茳芏湿地土壤碳氮含量的影响相对于江苏盐城、长江口以及杭州湾湿地的影响可能更为显著,其互花米草入侵较大改变了土壤中陆源和海源有机质的来源比例,使得入侵后湿地土壤养分的自源性增强。     

不同生境盐地碱蓬对氮饥饿的响应

为了探讨不同生境盐地碱蓬对低氮生境的适应机制,测定了盐渍环境下(200 mmol/L Na Cl)不同浓度硝态氮(0.3、5 mmol/L NO~-_3-N)预处理两种生境盐地碱蓬经氮饥饿后的NO~-_3含量、硝酸还原酶(NR)活性、光合特性及生长状况。结果表明,0.3和5 mmol/L NO~-_3-N处理以及进行氮饥饿时,潮间带生境盐地碱蓬叶片NO~-_3含量均高于内陆生境盐地碱蓬。与内陆生境盐地碱蓬相比,氮饥饿后,潮间带生境盐地碱蓬叶绿素含量、NR活性和光合放氧速率下降幅度均小于内陆生境盐地碱蓬,在0.3mmol/L NO~-_3-N预处理进行氮饥饿时趋势更加明显。0.3 mmol/L NO~-_3-N预处理后氮饥饿对潮间带生境盐地碱蓬根冠比没有影响,却降低内陆生境盐地碱蓬根冠比。上述结果表明,低氮条件下潮间带生境盐地碱蓬具有较高的NO~-_3储存能力,在环境持续氮素缺乏时具有较高的NO~-_3-N再利用能力,能更好地维持氮代谢以及光合性能。说明潮间带生境盐地碱蓬能更好地适应低氮生境。     

Exotic Spartina alterniflora invasion alters ecosystem–atmosphere exchange of CH4 and N2O and carbon sequestration in a coastal salt marsh in China

Coastal salt marshes are sensitive to global climate change and may play an important role in mitigating global warming. To evaluate the impacts of Spartina alterniflora invasion on global warming potential (GWP) in Chinese coastal areas, we measured CH₄ and N₂O fluxes and soil organic carbon sequestration rates along a transect of coastal wetlands in Jiangsu province, China, including open water; bare tidal flat; and invasive S. alterniflora, native Suaeda salsa, and Phragmites australis marshes. Annual CH₄ emissions were estimated as 2.81, 4.16, 4.88, 10.79, and 16.98 kg CH₄ ha^?1 for open water, bare tidal flat, and P. australis, S. salsa, and S. alterniflora marshes, respectively, indicating that S. alterniflora invasion increased CH₄ emissions by 57–505%. In contrast, negative N₂O fluxes were found to be significantly and negatively correlated (P < 0.001) with net ecosystem CO₂ exchange during the growing season in S. alterniflora and P. australis marshes. Annual N₂O emissions were 0.24, 0.38, and 0.56 kg N₂O ha^?1 in open water, bare tidal flat and S. salsa marsh, respectively, compared with ‐0.51 kg N₂O ha^?1 for S. alterniflora marsh and ?0.25 kg N₂O ha^?1 for P. australis marsh. The carbon sequestration rate of S. alterniflora marsh amounted to 3.16 Mg C ha^?1 yr^?1 in the top 100 cm soil profile, a value that was 2.63‐ to 8.78‐fold higher than in native plant marshes. The estimated GWP was 1.78, ?0.60, ?4.09, and ?1.14 Mg CO₂eq ha^?1 yr^?1 in open water, bare tidal flat, P. australis marsh and S. salsa marsh, respectively, but dropped to ?11.30 Mg CO₂eq ha^?1 yr^?1 in S. alterniflora marsh. Our results indicate that although S. alterniflora invasion stimulates CH₄ emissions, it can efficiently mitigate increases in atmospheric CO₂ and N₂O along the coast of China.     

滩地人工林幼林不同时间尺度CH4通量变化特征——基于涡度相关闭路系统的研究

长江滩地是甲烷(CH_4)排放的潜在热点区域,然而目前其CH_4通量的变化特征及控制因子尚未被揭晓。基于涡度相关闭路系统进行为期2年多的连续观测,旨在揭示长江滩地杨树(Populus deltoides)人工林幼林CH_4通量在不同时间尺度上的变化特征及其调控机理。结果显示,全年和部分未淹水月份表现出白天排放强而夜间排放弱的平均日变化特征,且淹水前、淹水期间和退水后分别表现出日间双峰型(7:00和10:00)、日间与夜间各一峰的双峰型(10:00和23:00),以及典型的日间单峰型(10:00)。淹水年份(2012年)在夏季(6—8月)排放最强,在春末(5月)和秋末冬初(11—12月)排放最弱,而未淹水年份(2013年)在初夏(6月)排放最强,在盛夏(7月)和秋末(11月)转变为较弱的吸收。淹水年份的年排放量((128.0±42.4)mmol/m~2)是未淹水年份((51.5±29.1)mmol/m~2)的2.5倍。滩地人工林幼林CH_4通量的日变化和季节变化最可能受到摩擦风速、水位和土壤温度的调节,而年际间的巨大差异主要由淹水状况决定。     

Habitat modification inhibits conspecific seedling recruitment in populations of an invasive ecosystem engineer

Invasive species that strongly modify their physical habitat are a particular management concern. Theoretical models predict that habitat modification could speed spread rates or allow invasion of sites that would otherwise resist invasion. There are few empirical tests of this hypothesis, however. We tested whether habitat modification by invading Spartina alterniflora populations facilitates conspecific seedling recruitment and spatial spread in Willapa Bay, WA, USA. Established S. alterniflora individuals strongly modified their local physical environment. Hydrologic flow, porewater salinity, and light availability were decreased while sediment NH₄ ⁺ increased with increasing S. alterniflora stem density. The S. alterniflora seed bank was greater and spring seedlings were denser within meadows of S. alterniflora than on unvegetated tideflats. However, almost all seedling recruitment after 1 year occurred on tideflats or on meadow edge plots where the above ground S. alterniflora biomass had been removed. Instead of facilitating invasive spread, ecosystem engineering in this system appears to create conditions that inhibit local seedling recruitment. These results suggest that the influence of ecosystem engineering on invasive spread is highly contingent on the relative spatial scales of habitat modification, environmental heterogeneity, and propagule availability. Control activities could change these spatial relationships, however, inadvertently promoting invasive recruitment.     

江苏滨海湿地芦苇和互花米草光合特性对模拟增温的响应

滨海湿地生态系统具有较高的初级生产力,是地球生态系统主要的碳库之一。然而,气候变暖和外来物种入侵通过改变植物光合特征性能使这一碳库的稳定性存在诸多的不确定性。利用在江苏盐城芦苇湿地和互花米草湿地建设的两个增温观测站,采用便携式光合荧光测量系统研究了本土植物芦苇（Phragmites australis）和入侵物种互花米草（Spartina alterniflora）光合特性对模拟增温的响应特征和机制。光合作用日调查变化曲线显示,增温使芦苇的净光合速率（P_n）、气孔导度（G_s）、蒸腾速率（T_r）和水分利用效率（WUE）都发生了显著的下降,但互花米草的各同名参数却表现出相反的变化特征,表明增温使互花米草的生理机能增强,促进了光合作用;根据P_n和胞间CO₂浓度（C_i）的变化趋势推断互花米草和芦苇光合速率变化均为非气孔限制因素驱动。利用直角双曲线修正模型拟合的光响应曲线结果显示,芦苇增温组的光响应曲线位于对照组下方,互花米草增温组的光响应曲线位于对照组上方;增温降低了所研究植物的光补偿点（LCP）,表明增温可提高两种植物利用弱光的能力;增温增加了互花米草光补偿点（LCP）和光饱和点（LSP）间值域范围,从而揭示了增温可有效提高互花米草利用光合有效辐射的能力;增温降低了芦苇的暗呼吸速率（R_d）,芦苇受到增温的胁迫,在减缓新陈代谢的同时也减弱了光合作用,而互花米草表现出相反特征。由此推测增温条件下入侵植物互花米草同化大气CO₂的能力（即碳汇能力）优于本土植物芦苇,这也是互花米草成为入侵物种的主要原因之一。     

北部湾大风江口互花米草湿地有机碳储量的分布特征

互花米草被引入我国滨海地区后,经过多年的生长与演替,改变了潮间带原有生态系统的碳储量,而影响机制仍有待深入研究.为进一步探讨互花米草入侵后潮滩有机碳储量演变特征,该文以广西北部湾大风江口入侵约6 a的互花米草湿地为研究对象,分析了2018年8月、11月及2019年1月、3月采集的样品中有机碳及相关理化指标.结果表示:(...     

张掖湿地甲烷通量动态特征及其影响因子

于2012年7月—2014年6月对地处干旱区的张掖湿地甲烷(CH_4)通量进行观测,分析其CH_4通量的变化特征及其影响因子。结果表明:CH_4通量的日变化趋势总体表现为白天大于夜间;不同季节CH_4通量排放特征差异明显,夏季最大,春秋次之,冬季最小;CH_4通量日总量与空气温度、土壤温度之间指数相关关系显著,其中4 cm处土壤温度与之相关性最强;1—6月摩擦风速(U*)与CH_4通量显著正相关;结合CO_2通量观测数据,研究时段张掖湿地净碳吸收量为495.92 g C m~(-2)a~(-1),为明显碳汇。     

水沙条件及氮输入对黄河口滨岸潮滩湿地碱蓬和土壤15N吸收特征的影响

受自然及人为活动的影响,黄河三角洲水沙条件存在较大变化,由此带来的外源营养物质增加对潮滩湿地植被生长及元素吸收利用具有重要的影响。为此采用3因素4水平的正交试验,以黄河口滨岸潮滩湿地先锋物种碱蓬（Suaeda salsa）为研究对象,利用¹⁵N示踪技术,研究了水沙条件及氮输入对碱蓬和土壤¹⁵N吸收特征的影响。结果表明：淹水深度、泥沙沉积及氮输入对土壤全氮含量的影响不显著,但外源氮输入对土壤¹⁵N固持量（N_dff）和比例（N_dff%）的影响达到显著水平,且最大值（10.44 mg/kg和3.83%）均出现在W₄S₂N₃（30 cm淹水+3 cm泥沙沉积+6 g/m²氮输入）处理;碱蓬叶和茎中全氮含量、¹⁵N吸收量（N_dff）及比例（N_dff%）在深淹水和泥沙沉积处理时较大,而根中全氮含量、N_dff及N_dff%在高氮输入较大。且根N_dff和N_dff%最大值（1.10 mg/kg和18.21%）在W₁S₄N₄（2 cm淹水+12 cm泥沙沉积+9 g/m²氮输入）处理时取得,此时碱蓬的生长情况最好,表明适当的淹水和泥沙埋深以及高氮输入（9 g/m²）有利于根系对外源氮的吸收,从而促进植株的生长。由此可见,在黄河三角洲水沙变化大的背景下,淹水、泥沙沉积和外源氮输入的适当把控,可促进碱蓬对外源氮的吸收利用而有助于其生长,从而对维护黄河三角洲潮滩湿地的健康具有重要作用。     

Diel vertical migration thresholds of Karenia brevis (Dinophyceae)

Light and nutrient availability change throughout dinoflagellate diel vertical migration (DVM) and/or with sub-population location in the water column along the west Florida shelf. Typically, the vertical depth of the shelf is greater than the distance a sub-population can vertically migrate during a diel cycle, limiting the ability of a sub-population to photosynthetically fix carbon toward the surface and access nutrients sub-surface. This project investigated changes of Karenia brevis (C.C. Davis) G. Hansen et Moestrup intracellular carbon, nitrogen, internal nitrate (iNO₃), free amino acid (FAA), and total lipid concentrations in high-light, nitrate-replete (960 μmol quanta m⁻² s⁻¹, 80 μM NO₃), and high-light, nitrate-reduced (960 μmol quanta m⁻² s⁻¹, <5 μM NO₃) mesocosms. The nitrate-reduced mesocosm had a slowed cell division rate when compared to the nitrate-replete mesocosm. Minimum intracellular carbon, nitrogen, iNO₃, FAA, and total lipid concentrations during the largest surface sub-population aggregations led to the conclusion that daughter cells resulting from cell division received unequal shares of the parental resources and that this inequality influenced migration behavior. Nutrient reduced daughter cells were more strongly influenced by light and phototaxis for carbon production than their replete same cell division sister cells during vertical migration thus rapidly increasing the fulfillment of constituents through photosynthesis. Vertical migration was consistent with an optimization scheme based on threshold limits through utilization or formation of photosynthate. We propose a simplified conceptual model describing how K. brevis is transported along the benthos of the west Florida shelf from off-shore to on-shore. Dynamic carbon thresholds are also suggested for future DVM modeling efforts on K. brevis populations transported between nitrogen replete and nitrogen reduced environmental conditions.     

Seasonal variation in CH4 emission and its 13C-isotopic signature from Spartina alterniflora and Scirpus mariqueter soils in an estuarine wetland

Although invasions by non-native species represent a major threat to biodiversity and ecosystem functioning, little attention has been paid to the potential impacts of these invasions on methane (CH₄) emission and its ¹³C-CH₄-isotope signature in salt marshes. An invasive perennial C₄ grass Spartina alterniflora has spread rapidly along the east coast of China since its introduction from North America in 1979. Since its intentional introduction to the Jiuduansha Island in the Yangtze River estuary in 1997, S. alterniflora monocultures have become the dominant component of the Jiuduansha’s vegetation, where monocultures of the native plant Scirpus mariqueter (a C₃ grass) used to dominate the vegetation for more than 30 years. We investigated seasonal variation in soil CH₄ emission and its ¹³C-CH₄-isotope signature from S. alterniflora and S. mariqueter marshes. The results obtained here show that S. alterniflora invasion increased soil CH₄ emissions compared to native S. mariqueter, possibly resulting from great belowground biomass of S. alterniflora, which might have affected soil microenvironments and /or CH₄ production pathways. CH₄ emissions from soils in both marshes followed similar seasonal patterns in CH₄ emissions that increased significantly from April to August and then decreased from August to October. CH₄ emissions were positively correlated with soil temperature, but negatively correlated with soil moisture for both S. alterniflora and S. mariqueter soils (p?<?0.05). The δ¹³C values of CH₄ from S. alterniflora, and S. mariqueter soils ranged from -39.0‰ to -45.0‰, and -37.3‰ to -45.7‰, respectively, with the lowest δ¹³C values occurring in August in both marshes. Although the leaves, roots and soil organic matter of S. alterniflora had significantly higher δ¹³C values than those of S. mariqueter, S. alterniflora invasion did not significantly change the ¹³C- isotopic signature of soil emitted CH₄ (p?>?0.05). Generally, the CH₄ emissions from both invasive S. alterniflora and native S. mariqueter soils in the salt marshes of Jiuduansha Island were very low (0.01–0.26 mg m^-2 h^-1), suggesting that S. alterniflora invasion along the east coast of China may not be a significant potential source of atmospheric CH₄.     

入侵种互花米草空间扩张模式识别与景观变化模拟

在3S技术支撑下,通过景观格局指数、质心变化等方法,分析2006—2015年研究区内互花米草群落的景观空间分布特征,并利用2015年高分二号影像识别出扩张模式及预测扩张趋势。结果表明:(1)近年来,互花米草沼泽向陆扩张速度大于向海扩张速度,其质心不断向陆方向移动。(2)2006—2015年,互花米草斑块密度变大,面积加权平均形状指数也相应增大为8.63,景观形状越来越复杂。(3)利用LEI和PFD识别出互花米草的3种扩张模式,边缘扩张面积远大于外部隔离扩张面积,外部隔离扩张斑块数量远多于边缘扩张和潮沟引领式扩张斑块数之和,潮沟对互花米草的向陆扩张起到引领作用。(4)利用缓冲区分析模拟互花米草向陆扩张的趋势,未来5年碱蓬沼泽的面积将减少11.45%。研究可为进一步认识互花米草入侵碱蓬沼泽机制提供科学参考。     

互花米草入侵影响下闽江河口湿地土壤有效硅的时空变化特征

2016年1—12月,选择闽江河口鳝鱼滩的短叶茳芏湿地、互花米草湿地以及二者的交错带湿地为研究对象,采用定位研究方法探讨了互花米草入侵影响下湿地土壤有效硅含量的时空变化特征。结果表明:互花米草入侵影响下3块湿地土壤有效硅含量随时间推移整体呈波动上升趋势;互花米草入侵显著提高了鳝鱼滩湿地30—60 cm土层土壤有效硅含量(P0.01),与短叶茳芏湿地相比,交错带湿地和互花米草湿地30—60 cm土层土壤有效硅含量分别增加了8.56%和19.97%,逐步线性回归分析表明土温和电导是影响其变化的重要因素(P0.01)。研究互花米草入侵影响下湿地土壤有效硅含量的变化特征,对于揭示湿地生态系统生源要素硅生物地球化学循环过程以及互花米草入侵及其扩张机制具有重要意义。     

安吉毛竹林水汽通量变化特征及其与环境因子的关系

以浙江省安吉县毛竹(Phyllostachys edulis)林生态系统为研究对象,利用涡度相关技术进行观测,获取2011年毛竹林的水汽通量数据,同时结合常规气象观测数据,分析了水汽通量全年变化。结果表明:毛竹林全年水汽通量基本为正值,月尺度上,水汽通量呈单峰型变化趋势,且各月的最大值均在12:00—14:00出现,呈现一定规律性,7月(0.1116 g m-2s-1)最高,12月(0.0209 g m-2s-1)最低;季节尺度上,夏季最高(0.0873 g m-2s-1),呈现典型单峰型变化趋势,春秋季(均为0.0541 g m-2s-1)次之,变化特征与夏季相似,冬季最低(0.0221 g m-2s-1),曲线变化复杂,波动较大。毛竹林全年蒸散量占全年降水量48.26%。2、4、5、11、12月蒸散量略大于降水量,其余月份蒸散量均小于降水量,6月份降水量与蒸散量差别最大。季节尺度上,对毛竹林水汽通量与净辐射进行回归关系分析,夏季最大,R2为0.6111,秋季为0.5295,春季为0.2605,冬季最小0.0455。通过F检验,水汽通量与净辐射有极显著线性关系。在植物生长期,毛竹林水汽通量随饱和水汽压差的增大而增大,植物发育成熟后,当饱和水汽压差增大到一定程度时,其增大反而抑制了水分的蒸散。     

互花米草NHX2基因的克隆与功能鉴定

NHX2属于CPA1基因家族,编码Na~+/H~+逆向转运蛋白,控制液泡膜中活性K~+的摄取,同时调节气孔的关闭。该研究以耐盐植物互花米草为材料,采用PCR技术克隆NHX2基因,并将其转入拟南芥进行相关功能鉴定。结果显示:(1)成功克隆获得互花米草NHX2基因CDS序列(1 602 bp),命名为SaNHX2,该基因编码533个氨基酸,SaNHX2蛋白的分子量约为58.65 kD,定位于细胞核和细胞膜,表明SaNHX2基因可能发挥转录调控的功能。(2) qRT-PCR结果显示,在ABA、NaCl和干旱胁迫处理下,互花米草叶和根中SaNHX2基因的表达量均上调。(3)为进一步鉴定其功能,成功构建植物表达载体,将SaNHX2基因转入拟南芥;经RT-PCR检测结果显示,SaNHX2基因在转基因植株中过表达;高盐胁迫处理后,转SaNHX2基因拟南芥的主根长度、叶绿素总量和相关胁迫应答基因表达量均高于转空载拟南芥,表明转SaNHX2基因拟南芥的耐盐能力显著增强。研究表明,SaNHX2基因可能在盐胁迫调节机制中发挥调控作用,可作为改良农作物耐盐的重要候选基因。     

Contents of volume 137 1991

The halophyte, Suaeda salsa, was grown in saline soil in pots and watered with a NaCl solution containing 0.2 g L^-1 Na-ions. S. salsa accumulated Na during a 120-day growing period and caused a net reduction in the Na content of the soil. S. salsa also decreased the Na content of saline soil in a field experiment. The Na content of the soil at depth 20–30 cm was reduced by 4.5% with S. salsa at a density of 15 plants m^-2 and by 6.7% with a density of 30 plants m^-2. In contrast, the Na content was decreased by only 1% with Medicago sativa at 15 plant m^-2 and increased by 3.8% with bare soil. The results confirm that S. salsa is an effective salt absorber in saline soils.     

Highly efficient Agrobacterium-based transformation system for callus cells of the C3 halophyte Suaeda salsa

Genetic manipulation technologies have been limited in the halophyte Suaeda salsa L. due to the lack of an efficient transformation system. Here, we examined factors affecting transformation and developed an efficient transformation system at the cell level using S. salsa hypocotyl as starting material. S. salsa hypocotyl explants from 10-day-old seedlings were precultured for 2 days on a hygromycin (hyg)-free callus induction medium (CIM) and then inoculated with Agrobacterium tumefaciens suspension at a concentration of 0.5 at OD₆₀₀ for 5–10 min. After cocultivation with A. tumefaciens for 4 days in the dark, followed by selection on carbenicillin (carb) for 3 days, explants were placed on CIM containing 10 mg l⁻¹ hyg and 500 mg l⁻¹ carb with three to four consecutive subcultures for up to 45 days. β-Glucuronidase assays showed an average transformation frequency of 62.89%. Gene integration was confirmed by polymerase chain reaction analysis and Northern blot analysis. To our knowledge, this is the first study to show Agrobacterium-mediated transformation in the C₃ halophyte S. salsa.     

Enhanced Tonoplast H+-ATPase Activity and Superoxide Dismutase Activity in the Halophyte Suaeda salsa Containing High Level of Betacyanin

In this study, high-betacyanin Suaeda salsa seedlings were developed and used to explore whether the betacyanin accumulation is related to salinity tolerance in S. salsa. After 8 days of culture, betacyanin content decreased markedly in both high-betacyanin S. salsa seedlings and the control under nonsalt stress, but the decreases were suppressed by NaCl treatments. Betacyanin content in high-betacyanin seedlings was much higher than that in the control throughout the salt treatments. Growth of S. salsa plants was significantly promoted by NaCl treatments, and the fresh weight of high-betacyanin seedlings was much higher than that of the control when grown in 400 mmol L⁻¹ NaCl. Similar cell sap osmolarity and K⁺/Na⁺ ratios were observed in high-betacyanin seedlings and the control. No obvious differences in V-ATPase (tonoplast H⁺-ATPase) activity, leaf SOD (superoxide dismutase) activity, and total chloroplast SOD (including thylakoid-bound SOD and stroma SOD) activity were detected between high-betacyanin seedlings and the control under nonsalt stress conditions. However, V-ATPase hydrolytic activity increased dramatically in S. salsa seedlings when subjected to different levels of NaCl, and the increases in V-ATPase activity in high-betacyanin seedlings were much higher than that in the control. No clear pattern was observed for NaCl-dependent activity changes of P-ATPase (plasma membrane H⁺-ATPase) and V-PPase (tonoplast H⁺-pyrophosphatase). Similar changes were demonstrated in leaf SOD activity and chloroplast SOD activity under salt stress. Both leaf SOD activity and chloroplast SOD activity were markedly enhanced with the increase of NaCl or with time, especially thylakoid-bound SOD activity. Furthermore, the increases in chloroplast SOD activity and thylakoid-bound SOD activity were much higher in high-betacyanin seedlings than that in the control at different levels of NaCl treatment. The higher V-ATPase activity, chloroplastic SOD activity, and thylakoid-bound SOD activity demonstrated in high-betacyanin seedlings, but lower in the control, suggest that high-betacyanin S. salsa seedlings may have higher potential to be energized by the electrochemical gradient for ion uptake into the vacuole and to scavenge O₂^−• in situ produced in the chloroplasts, which may lead to higher salt tolerance than the control under salt stress. Thus, betacyanin may be involved in salt tolerance of S. salsa.     

滩涂湿地入侵种互花米草植被覆盖度的高空间分辨率遥感估算

互花米草是沿海滩涂生态系统的重要入侵物种,其分布状况和覆盖度是湿地生态研究的重要参数和基础。以宁德三沙湾(三都澳)滩涂湿地为研究区,以SPOT6 6 m空间分辨率卫星影像为数据源,对互花米草分布和植被覆盖度进行研究,并与同期10 cm空间分辨率无人机影像进行比较验证。结果表明,影像覆盖区域内互花米草总面积为20.19 km~2,其中蕉城区互花米草分布较广,面积为9.63 km~2,占研究区互花米草总面积的47.70%。互花米草植被覆盖度整体上以40%-60%和60%-80%的中、高覆盖度分布为主,其分布面积分别为5.44 km~2和4.95 km~2,占互花米草总分布面积的26.92%和24.52%,而40%以下的低覆盖度和80%以上较高覆盖度分布相对较少。SPOT6遥感影像估算得到的互花米草植被覆盖度具有较好的精度,与无人机影像值之间的均方根误差RMSE为0.117,线性回归决定系数R~2为0.918,可用于滩涂湿地植被覆盖度分析。     

广西山口红树林保护区互花米草扩散动态及其驱动力

互花米草在红树林湿地中扩散对生境与生态系统造成严重影响,已成为生物入侵问题研究的焦点之一。然而目前关于互花米草扩散动态及其驱动力的研究成果仍为鲜见。论文以广西山口红树林保护区为研究对象,以2009、2013、2019年遥感影像为数据源,采用人机互译、野外勘查结合的方法识别互花米草布局,利用土地类型转移矩阵、质心的变化、景观指数以及灰色关联度等方法分析互花米草扩散特征及其驱动力。结果表明：（1）2009-2019年间,互花米草面积、斑块数量呈现增长趋势,但面积增幅下降,2009-2013年间年均增长率为7.60%,2013-2019年间年均增长率则为1.99%;互花米草面积年均增长率大于红树林,光滩转化为互花米草的面积是其转化为红树林面积的1.507倍;互花米草、红树林均有破碎化趋势;（2）2009-2019年间,互花米草的质心坐标都位于丹兜海潮滩,2009-2013年互花米草斑块质心向西北方向偏移,2013-2019年向东南方向偏移;（3）2009-2019年间,互花米草动态变化受到人为因素与自然因素共同影响。其中,赶海人口比例与最大斑块指数、斑块密度、斑块数相关性最大;年均最高温与互花米草分维数、破碎化指数、面积相关性最大。（4）影响互花米草面积变化的因素依次为：年均最高温、年均最低温、赶海人口比例、地区生产总值;互花米草面积与年均最高、年均低温均呈正相关,与赶海人口比例呈负相关。研究结果将为互花米草监控提供科学借鉴,为红树林保护提供理论依据。