大丽轮枝菌微菌核的萌发条件及致死温度

微菌核是大丽轮枝菌在土壤中的主要存活结构和初侵染源,在土壤中可存活14年之久,其数量及存活状况直接影响着大丽轮枝菌型黄萎病的发生为害程度。以棉花黄萎病菌Verticillium dahliae XJ2008菌株为试材,研究了微菌核萌发的最佳条件、致死温度及土壤温度对微菌核存活的影响。结果表明,20℃、pH8.0是微菌核萌发的最佳条件。大丽轮枝菌微菌核具有很强的耐高温特性,随着处理时间的延长,微菌核的萌发率呈下降趋势,在55℃及以上处理时其萌发率下降迅速,而在50℃及以下处理时其萌发率下降相对较慢,在55℃处理360min可使微菌核完全致死,而在40℃、45℃和50℃处理1,440min,仍然有少量的微菌核存活,但其萌发率随着时间的推移呈下降趋势。土壤微菌核模拟试验结果表明,土壤温度对微菌核有很强的致死作用,40℃条件下处理4d后土壤中的微菌核已全部死亡。该研究结果为通过覆膜增温防治作物黄萎病提供了理论依据。     

菌核寄生菌Talaromyces flavus的生物学特性及寄生菌核规律初探

本文对核盘菌菌核寄生菌Ｔａｌａｒｏｍｙｃｅｓｆｌａｖｕｓ的基本生物学特性及影响其寄生菌核的生态因子进行了初步研究。结果表明：Ｔ。ｆｌａｖｕｓ在我国南北方菌核病发生区土壤中普遍存在。其菌丝在３－３５℃及ｐＨ值２－１０范围内均能生长及产孢,最适生Ｋ温度为３０℃,最适生长ｐＨ值为４。对峙培养结果表明Ｔ,Ｆｌａｖｕｓ对核盘菌的抗生作用微弱,对菌丝和菌核均有很强的寄生致腐作用。除核盘菌外它还能寄生三叶草核盘菌、小核盘菌及离菌上的一种待鉴定的产菌核真菌。Ｔ,ｆｌａｖｕｓ寄生菌核的最适温度为２５－３０℃,土壤类型也影响到其寄生致腐菌核的效果。     

菌核寄生菌Talaromyces flavus的生物学特性及寄生菌核规律初探

本文对核盘菌菌核寄生菌Ｔａｌａｒｏｍｙｃｅｓｆｌａｖｕｓ的基本生物学特性及影响其寄生菌核的生态因子进行了初步研究。结果表明：Ｔ.Ｆｌａｖｕｓ在我国南北方菌核病发生区土壤中普遍存在。其菌丝在３－３５℃及ｐＨ值２－１０范围内均能生长及产孢,最适生Ｋ温度为３０℃,最适生长ｐＨ值为４。对峙培养结果表明Ｔ,fｌａｖｕｓ对核盘菌的抗生作用微弱,对菌丝和菌核均有很强的寄生致腐作用。除核盘菌外它还能寄生三叶草核盘菌、小核盘菌及离菌上的一种待鉴定的产菌核真菌。Ｔ,ｆｌａｖｕｓ     

链孢粘帚霉几丁质酶的诱导及其抗真菌活性研究

链孢粘帚霉HL-1-1菌株在不同培养条件下产几丁质酶活性不同,核盘菌菌核对其几丁质酶的诱导作用高于几丁质;首次用菌核配制培养基成功诱导了几丁质酶的产生,其产酶的最适初始pH值为4.5,最适培养时间为6d。几丁质酶对10种病原菌都有不同的抑制作用,对小麦雪腐病、葡萄白腐病、玉米黄斑病及斑点落叶病等病原菌的孢子萌发具有明显的抑制作用;该几丁质酶还能明显抑制核盘菌和立枯丝核菌的菌核萌发。     

核盘菌可溶性蛋白质及同工酶电泳研究*

为了研究核盘菌的分类和生理分化问题,对供试的28个核盘菌株进行了可溶性蛋白质,芳香基酯酶和酸性磷酸酯酶同工酶电泳谱带以及紫外光吸收峰图形的试验研究,其结果,可分为五种类型。其中属于核盘菌属有四个种,即核盘菌Sclerotinia sclerotiorum(Lib.)de Bary(=Whetzelinia sclerotiorum(Lib.)Korf & Dumont),三叶草核盘菌S.trifoliorum Erikss.,细辛核盘菌(S.asari Wu et C.R.Wang和人参菌核病菌Sclerotinia sp。人参菌核病的另一分离菌和油菜菌核病的一个分离菌其谱带与灰葡萄孢(Botrytis cinerea)谱带相似,应归属于与葡萄孢属(Botrytis)相应的核盘菌。在核盘菌S.sclerotiorum种群中,南方菌系与北方菌系的可溶性蛋白质稍有差异,芳香基酯酶和酸性磷酸酯酶活性强度也稍有不同,可能存在生理分化现象。     

核盘菌可溶性蛋白质及同工酶电泳研究

为了研究核盘菌的分类和生理分化问题,对供试的28个核盘菌株进行了可溶性蛋白质,芳香基酯酶和酸性磷酸酯酶同工酶电泳谱带以及紫外光吸收峰图形的试验研究,其结果,可分为五种类型。其中属于核盘菌属有四个种,即核盘菌Sclerotinia sclerotiorum(Lib.)de Bary(=Whetzelinia sclerotiorum(Lib.)Korf & Dumont),三叶草核盘菌S.trifoliorum Erikss.,细辛核盘菌(S.asari Wu et C.R.Wang和人参菌核病菌Sclerotinia sp。人参菌核病的另一分离菌和油菜菌核病的一个分离菌其谱带与灰葡萄孢(Botrytis cinerea)谱带相似,应归属于与葡萄孢属(Botrytis)相应的核盘菌。在核盘菌S.sclerotiorum种群中,南方菌系与北方菌系的可溶性蛋白质稍有差异,芳香基酯酶和酸性磷酸酯酶活性强度也稍有不同,可能存在生理分化现象。     

黄绿木霉菌代谢产物对大豆菌核病核盘菌的抑菌能力研究

利用室内实验的方法,研究了黄绿木霉对大豆菌核病菌的抑菌能力。黄绿木霉在与核盘菌（Sclerotinia sderotiorum）对峙培养过程中,5-7d即可将菌核病菌完全覆盖,在形成的菌核上会有黄绿木霉孢子出现,扫描电镜中观察到核盘菌的菌丝体发生变形;其代谢产物在经121℃处理25min后,抑菌作用仍可高达100％;在对黄绿木霉发酵过程中,利用PD培养基即可达到有效的控制大豆菌核病菌菌丝生长的目的,而且利用PD培养基发酵3-4d的黄绿木霉代谢产物抑菌效果最好,抑菌中浓度最低,发酵时间过长与过短,均不利于对病原菌的抑制。经黄绿木霉代谢产物处理的菌核菌电导率与呼吸强度均发生变化,在光学显微镜下观察到菌核菌菌体发生变化,且处理后的菌核菌致病力明显降低。     

植病生防菌盾壳霉的研究进展

盾壳霉是世界性病原真菌核盘菌的主要拮抗真菌之一。许多研究表明盾壳霉具有控制温室和田间多种作物菌核病的潜力。目前欧洲一些国家已有盾壳霉商品制剂销售。为了加速盾壳霉产业化进程和更好地发挥其控制菌核病的作用 ,以及为了使人们对盾壳霉的研究不断深入 ,综述了盾壳霉生态学特性、遗传改良、对核盘菌的生防机制、在菌核病防治上的应用及基因工程研究等方面的研究进展。     

滇南红厚壳种子的脱水敏感性及其影响萌发的因子

滇南红厚壳(Colophyllum polyanthum Wall.ex Choisy)种子的千粒重约为4700g,脱落时种子的含水量为45％(鲜重),其存活率对脱水高度敏感;当种子含水量降至30％以下时,存活率迅速下降;种子存活率的半致死含水量约为23％;可以认为它是一种典型的顽拗性种子。含水量为45％的种子,在20--30℃的范围内,随着温度的升高种子萌发50％所需要的时间缩短;高于和低于这个温度范围(如15℃,30℃),种子的萌发率均下降;变温处理有利于提高种子的萌发率和萌发速率。除去种皮和切除部分子叶能提高种子的萌发率、萌发速率,以及种子萌发后的早期幼苗生长量。光照明显地促进整粒种子的萌发,但对除去种皮的种子、具有1／2子叶的种子、以及胚轴的萌发没有影响。     

Endomelanconiopsis microspora发酵产物乙酸乙酯提取物对人参核盘菌的抑制机理

【背景】人参菌核病是人参的主要病害之一,严重影响人参的产量。【目的】探索白花蒲公英内生菌(Endomelanconiopsis microspora)发酵产物乙酸乙酯提取物对人参核盘菌的抑制机理。【方法】采用人参核盘菌菌丝生长和孢子萌发试验测定抑制效果;采用显微镜观察菌丝形态变化,通过电导率和核酸含量的变化测定细胞膜通透性,通过丙二醛(malondialdehyde,MDA)含量和超氧化物歧化酶(superoxide dismutase,SOD)、过氧化物酶(peroxidase,POD)和过氧化氢酶(catalase,CAT)活力的变化测定膜脂过氧化程度。【结果】内生菌E. microspora发酵产物乙酸乙酯提取物能显著抑制人参核盘菌菌丝生长,最小抑菌浓度为3.75 mg/mL,培养6 d后抑制率为76.22%。该提取物能显著抑制人参核盘菌孢子萌发,15.00 mg/mL时抑制效果最好,抑制率达90.69%。提取物影响菌丝形态,增加人参核盘菌细胞膜通透性,造成菌丝内含物外渗,7.50 mg/mL处理10 h后电导率和核酸含量分别比对照组增加30.11%和62.85%。同时提取物显著增加人参核盘菌MDA含量和SOD、POD、CAT活力,7.50 mg/mL处理组呈现先上升后下降的变化趋势,并在12 h时达到最高值。【结论】内生菌E. microspora发酵产物乙酸乙酯提取物通过改变人参核盘菌细胞膜通透性,加剧膜脂过氧化,破坏细胞膜完整性,导致细胞内含物流失,显著抑制孢子萌发和菌丝生长。     

不同幅度的实验增温对藏北高寒草甸净生态系统碳交换的影响

全球气候变暖将对陆地生态系统(尤其是高寒草甸生态系统)碳循环产生深远影响。该研究依托中国科学院地理科学与资源研究所藏北高原草地生态系统研究站(那曲站), 设置不同增温幅度实验, 模拟未来2 ℃增温和4 ℃增温的情景, 探究不同增温幅度对青藏高原高寒草甸净生态系统碳交换(NEE)的影响。研究结果显示: 1)在2015年生长季(6-9月), 不增温和2 ℃增温处理下NEE小于0, 总体表现为碳汇, 而4 ℃增温处理下NEE大于0, 总体表现为碳源; 2)在生长季的6月、8月及整个生长季, 与不增温相比, 4 ℃增温处理显著提高了NEE, 而2 ℃增温处理没有显著改变NEE; 7月, 2 ℃和4 ℃增温处理均显著提高了NEE; 3)在半干旱的高寒草甸生态系统, 土壤水分是决定NEE的关键因素, 增温通过降低土壤水分而导致高寒草甸生态系统碳汇能力下降。该研究可为青藏高原高寒草甸生态系统应对未来气候变化提供基础数据和理论依据。     

Effects of experimental warming on net ecosystem CO2 exchange in Northern Xizang alpine meadow

AimsGlobal warming could have profound effects on ecosystem carbon (C) fluxes in alpine ecosystems. The aim of our study is to examine the effects of gradient warming on net ecosystem carbon exchange (NEE).MethodsIn the Northern Tibetan Grassland Ecosystem Research Station (Nagqu station), Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, we conducted various levels of temperature increasing experiments (i.e., 2 °C and 4 °C increments). The warming was achieved using open-top chambers (OTCs). In total, there were three levels of temperature treatments (control, 2 °C and 4 °C increment), and four replicates for each treatment. The ecosystem NEE was monitored every five days during the growing season in 2015.Important findings Our findings highlight the importance of soil moisture in mediating the responses of NEE to climatic warming in alpine meadow ecosystem. The 4 °C warming significantly stimulated NEE,except for July measurements. The 2 °C warming had no effects on NEE during the growing season. Compared to the 2 °C warming, the 4 °C warming significantly stimulated NEE. The results showed that our targeted ecosystem acts as a carbon sink under 2 °C warming, whereas will act as a net carbon source under 4 °C warming in the future. This study provides basic data and theoretical basis for evaluating the alpine ecosystem’s responses to climate change.     

天山雪莲SiSAD基因与拟南芥AtFAB2基因转化 烟草的抗寒性分析

通过转基因烟草(Nicotiana tabacum)验证天山雪莲(Saussurea involucrata) Δ9硬脂酰-ACP脱饱和酶基因SiSAD与拟南芥(Arabidopsis thaliana)中同源基因AtFAB2的抗寒性功能。利用农杆菌介导法将植物表达载体P_SiSAD:AtFAB2和P_SiSAD:SiSAD导入烟草, 然后将2种转基因和野生型烟草分别置于20°C、10°C、5°C、0°C及-2°C下处理2小时, 检测其相对电导率、丙二醛(MDA)含量、叶绿素荧光参数(F_v/F_m)及脂肪酸含量。将-2°C处理2小时后的植株置于25°C培养1周进行生长恢复实验。结果表明, 生长恢复实验中转SiSAD基因烟草的恢复效果显著优于转AtFAB2基因和野生型烟草。在0°C和-2°C处理2小时后, 转SiSAD、AtFAB2基因型和野生型烟草的相对电导率和丙二醛含量呈现显著递增趋势; 转SiSAD、AtFAB2基因型烟草的F_v/F_m显著高于野生型烟草, 其中, 转SiSAD基因烟草的F_v/F_m显著高于转AtFAB2基因烟草。转AtFAB2基因型和野生型烟草的油酸(C18:1)含量随着温度的降低逐渐升高后降低并在0°C时达到最高值; 而转SiSAD基因型烟草C18:1含量持续升高, 并在-2°C时达到最高值, 其含量分别是转AtFAB2基因型和野生型烟草的1.58倍和1.7倍。以上结果表明, 天山雪莲Δ9硬脂酰-ACP脱饱和酶基因SiSAD与拟南芥中同源基因AtFAB2均可以显著增强非低温驯化烟草的抗寒性, 但是SiSAD基因效果显著优于AtFAB2。     

海三棱藨草的组织培养与快繁体系

以海三棱藨草(Scirpus × mariqueter)成熟种子为外植体, 通过无菌萌发、丛生芽诱导、增殖、壮苗、生根和移栽等过程, 建立了海三棱藨草的无菌快繁体系。结果表明: 丛生芽诱导和增殖的最适培养基为MS+2.0 mg·L^-1 6-BA+0.002 mg·L^-1 TDZ+0.2 mg·L^-1 IBA; 壮苗最适培养基为1/2MS+0.05 mg·L^-1 6-BA+0.01 mg·L^-1 IBA; 生根最适培养基为1/2 MS+0.2 mg·L^-1 IBA; 最适培养温度为30°C; 再生苗移入珍珠岩:草炭:蛭石=1:1:1 (体积比)的混合基质中, 移栽成活率可达85%以上。生根培养阶段选用容积较大的塑料容器育苗, 可以降低生产成本和提高生产效率。     

培养基及培养条件对冬虫夏草菌固体发酵产分生孢子的影响

为获得冬虫夏草菌固体发酵产分生孢子的最优工艺,以野生分离的冬虫夏草菌为材料,对其固体发酵产分生孢子的培养基及培养条件进行了研究。试验结果表明：泥炭土为最佳基础培养基,该培养基中冬虫夏草菌气生菌丝生长一般,但产分生孢子最多,可达4.2×10³个/g;泥炭土培养基中添加0.1‰ IAA（吲哚乙酸）、0.1‰ IBA（吲哚丁酸）和0.1‰ NAA（萘乙酸）能促进冬虫夏草菌气生菌丝的生长和分生孢子的产生,其分生孢子达8.1×10³个/g;该基础培养基中,冬虫夏草菌于18℃培养30d后,在10℃、相对湿度45%、蓝光照射进行诱导,分生孢子可达1.0×10⁴个/g。本研究建立了一种大量获取冬虫夏草菌分生孢子的方法,为冬虫夏草繁育奠定了基础。     

北亚热带地带性森林土壤温室气体通量对土地利用方式改变和降水减少的响应

弄清土地利用和降水变化对林地土壤主要温室气体(CO₂、CH₄和N₂O)排放通量变化的影响, 是准确评估森林土壤温室气体排放能力的重要基础。该研究以常绿落叶阔叶混交林原始林、桦木(Betula luminifera)次生林和马尾松(Pinus massoniana)人工林为对象, 采用静态箱-气相色谱法研究了3种土地利用方式(常绿落叶阔叶混交林原始林、桦木次生林和马尾松人工林)和降水减少处理状况下森林土壤CO₂、CH₄和N₂O通量排放特征, 并探讨了其环境驱动机制。研究结果表明: 原始林土壤CH₄吸收通量显著高于次生林和人工林, 次生林CH₄吸收通量显著高于人工林土壤。人工林土壤CO₂排放通量显著高于原始林和次生林土壤。次生林土壤N₂O排放通量高于原始林和人工林, 但三者间差异不显著。降水减半显著抑制了3种不同土地利用方式下林地土壤CH₄吸收通量; 降水减半处理对原始林和次生林土壤CO₂排放通量均具有显著的促进作用, 而对人工林土壤CO₂排放通量具有显著的抑制作用; 降水减半处理促进了原始林和人工林林地土壤N₂O排放而抑制了次生林林地土壤N₂O排放。原始林和次生林林地土壤CH₄吸收通量随土壤温度升高显著增加, CH₄吸收通量与土壤温度均呈显著相关关系; 原始林、次生林和人工林土壤CO₂和N₂O排放通量与土壤温度均呈显著正相关关系; 土壤湿度抑制了次生林和人工林土壤CH₄吸收通量, 其CH₄吸收通量随土壤湿度增加显著减少; 原始林土壤CO₂排放通量与土壤湿度呈显著正相关关系。自然状态下, 原始林土壤N₂O排放通量与土壤湿度呈显著正相关关系, 原始林和次生林土壤N₂O排放通量与硝态氮含量呈显著相关关系。研究结果表明全球气候变化(如降水变化)和土地利用方式的转变将对北亚热带森林林地土壤温室气体排放通量产生显著的影响。     

Greenhouse gas fluxes of typical northern subtropical forest soils: Impacts of land use change and reduced precipitation

Aims It is important to study the effects of land use change and reduced precipitation on greenhouse gas fluxes (CO₂, CH₄ and N₂O) of forest soils. Methods The fluxes of CO₂, CH₄ and N₂O and their responses to environmental factors of primary forest soil, secondary forest soil and artificial forest soil under a reduced precipitation regime were explored using the static chamber and gas chromatography methods during the period from January to December in 2014. Important findings Results indicate that CH₄ uptake of primary forest soil ((-44.43 ± 8.73) μg C·m^-2·h^-1) was significantly higher than that of the secondary forest soil ((-21.64 ± 4.86) μg C·m^-2·h^-1) and the artificial forest soil ((-10.52 ± 2.11) μg C·m^-2·h^-1). CH₄ uptake of the secondary forest soil ((-21.64 ± 4.86) μg C·m^-2·h^-1) was significantly higher than that of the artificial forest ((-10.52 ± 2.11) μg C·m^-2·h^-1). CO₂ emissions of the artificial forest soil ((106.53 ± 19.33) μg C·m^-2·h^-1) were significantly higher than that of the primary forest soil ((49.50 ± 8.16) μg C·m^-2·h^-1) and the secondary forest soil ((63.50 ± 5.35) μg C·m^-2·h^-1) (p < 0.01). N₂O emissions of the secondary forest soil ((1.91 ± 1.22) μg N·m^-2·h^-1) were higher than that of the primary forest soil ((1.40 ± 0.28) μg N·m^-2·h^-1) and the artificial forest soil ((1.01 ± 0.86) μg N·m^-2·h^-1). Reduced precipitation (-50%) had a significant inhibitory effect on CH₄ uptake of the artificial forest soil, while it enhanced CO₂ emissions of the primary forest soil and the secondary forest soil. Reduced precipitation had a significant inhibitory effect on CO₂ emissions of the artificial forest soil and N₂O emissions of the secondary forest (p < 0.01). Reduced precipitation promotes N₂O emissions of the primary forest soil and the artificial forest soil. CH₄ uptake of the primary forest and the secondary forest soil increased significantly with the increase of soil temperature under natural and reduced precipitation. CO₂ and N₂O emission fluxes of the primary forest soil, secondary forest soil and artificial forest soil were positively correlated with soil temperature (p < 0.05). Soil moisture inhibited CH₄ uptake of the secondary forest soil and the artificial forest soil (p < 0.05). CO₂ emissions of the primary forest soil were significantly positively correlated with soil moisture (p < 0.05). N₂O emissions of primary forest soil and secondary forest soil were significantly correlated with the nitrate nitrogen content (p < 0.05). It was implied that reduced precipitation and land use change would have significant effects on greenhouse gas emissions of subtropical forest soils.     

Differential effects of diurnal asymmetric and symmetric warming on yield and water utilization of soybean

Aims Global warming does not mean similar warmer temperatures between daytime and nighttime. Soybean (Glycine max) is a widely planted legume crop around the world and an important food crop in China. The aim of this study was to understand the responses of soybean growth and water utilization to future asymmetric warming, which would provide scientific reference for evaluating the adaptation of soybean to the future climate scenarios.Methods This experiment was carried out in artificial climate chambers, using the method of potted plants, under three temperature conditions; contrast (CON, 26 °C during the day and 16 °C during night), symmetric warming (ETs, elevated temperature of 3 °C both during the day and night), asymmetric warming (ETa, elevated temperature of 2 °C during the day and elevated temperature of 4 °C during night). We investigated the differential effects of diurnal asymmetric and symmetric warming on the yield and water consumption of soybean. Important findings The results revealed that, under the background of 26 °C during the day and 16 °C during night: 1) the effect of ETs on soybean yields showed no significant function that mainly benefit from the increase in the amount of biomass to ease negative influence of decrease in the harvest index. ETa reduced yields of soybean by 38.9% (p < 0.05) due to both significant decrease in harvest index and yield components (pod number per plant, grain number per pod and 100-grain weight). 2) ETs showed no obvious effect on the whole growing stage evapotranspiration (ET) of soybean, while ETa reduced the whole growing stage ET by 14.8% (p < 0.05). 3) The effect of the two warming pattern on water consumption of soybean were not significant. The difference in water consumption was mainly derived from the difference in transpiration (T). ETs and ETa reduced total transpiration by 10.7% (p < 0.05) and 26.1% (p < 0.05), respectively. In conclusion, our results suggest that ETs will underestimate the detrimental effects of real climate warming (ETa) on the growth and yield of soybean, and overestimate the effects on water consumption of soybean.     

昼夜不对称性与对称性升温对大豆产量和水分利用的影响

全球气候变暖并不是白天和夜间的平均变暖, 而是呈现一定的不对称性。大豆(Glycine max)是世界范围内种植较广泛的豆科作物, 也是中国重要的粮食作物。研究大豆的生长与水分利用对不对称性气候变暖的响应, 可为预测未来气候变暖情景下大豆的适应提供科学的参考依据。该实验在人工气候箱中采用盆栽方式进行, 设立对照(CON, 昼26 ℃夜16 ℃)、对称性升温(ETs, 昼夜均升高3 ℃)和不对称性升温(ETa, 昼升高2 ℃, 夜升高4 ℃)三个温度情景, 研究了大豆产量和水分利用对昼夜不对称性与对称性升温的差异性响应。结果表明: 在昼/夜26 ℃/16 ℃的背景下, 1) ETs对大豆产量影响不显著, 主要是因为生物量的增加缓解了收获指数下降对大豆的不利影响; ETa使大豆产量减少38.9%, 是由于大豆的收获指数和产量构成要素(荚数、粒数、百粒重)均显著降低。2) ETs对大豆全生育期蒸散量(ET)的影响不显著, ETa使大豆整个生育期ET减少14.8%。3)两种升温模式对大豆耗水量中蒸发量的影响都不显著, 耗水量的差异主要来自蒸腾量的差异, 其中ETs和ETa分别使大豆全生育期蒸腾量降低10.7%和26.1%。综上所述, 只针对ETs进行研究, 而没有对ETa进行研究的实验会低估真正的气候变暖情景(ETa)对大豆生长和产量的不利影响, 高估其对大豆耗水量的影响。     

Exposure Time to Lethal Temperatures for Meloidogyne incognita Suppression and Its Implication for Soil Solarization

Meloidogyne incognita eggs or J2 were incubated in test tubes containing sand:peat mix and immersed in a water bath heated to 38, 39, 40, 41, 42, 43, 44 and 45°C for a series of time intervals. Controls were maintained at 22°C. Nematodes surviving or hatching were collected from Baermann trays after three weeks of incubation. Regression analyses between percent survival or egg hatch and hours of heat treatment were performed for each temperature. Complete suppression of egg hatch required 389.8, 164.5, 32.9, 19.7 and 13.1 hours at 38, 39, 40, 41 and 42°C, respectively. Complete killing of J2 required 47.9, 46.2, 17.5 and 13.8 hours at 39, 40, 41 and 42°C, respectively. J2 were not completely killed at 38°C within 40 hours of treatment, but were killed within one hour at 44 and 45°C. Effect of temperature on nematode killing is not determined by heat units. Oscillating temperature between cool and warm did not interfere with the nematode suppressive effect by the heat treatment. Six-week solarization in the field during the summers of 2003 and 2004 in Florida accumulated heat exposure times in the top 15 cm of soil that surpassed levels required to kill M. incognita as determined in the water bath experiments. Although near zero M. incognita were detected right after solarization, the nematode population densities increased after a cycle of a susceptible pepper crop. Therefore, future research should address failure of solarization to kill nematodes in the deeper soil layers.