Herbivory-induced mortality increases with radial growth in an invasive riparian phreatophyte

Background and Aims

Under equal conditions, plants that allocate a larger proportion of resources to growth must do so at the expense of investing fewer resources to storage. The critical balance between growth and storage leads to the hypothesis that in high-resource environments, plants that express high growth rates are more susceptible to episodic disturbance than plants that express lower growth rates.

Methods

This hypothesis was tested by measuring the radial growth, basal area increment (BAI) and carbon isotope ratios (δ¹³C) in tree-ring α-cellulose of 62 mature tamarisk trees (Tamarix spp.) occurring at three sites in the western USA (n = 31 live and 31 killed trees across all sites, respectively). All of the trees had been subjected to periods of complete foliage loss by episodic herbivory over three or more consecutive growing seasons by the tamarisk leaf beetle (Diorhabda carinulata), resulting in approx. 50 % mortality at each site.

Key Results

Mean annual BAI (measured from annual ring widths) in the 10 years prior to the onset of herbivory was on average 45 % higher in killed trees compared with live trees (P < 0·0001). Killed trees that had higher growth rates also expressed higher (less negative) δ¹³C ratios compared with live trees. In fact, at one site near Moab, UT, the mean annual BAI was 100 % higher in killed trees despite having about a 0·5 ‰ higher δ¹³C relative to live trees (P = 0·0008). Patterns of δ¹³C suggest that the intrinsic water-use efficiency was higher in killed than surviving trees, possibly as a consequence of lower whole-canopy stomatal conductance relative to live trees.

Conclusions

The results show that a likely trade-off occurs between radial growth and survival from foliage herbivory in Tamarix spp. that currently dominates riparian areas throughout the western USA and northern Mexico. Thus, herbivory by D. carinulata may reduce the overall net primary productivity of surviving Tamarix trees and may result in a reduction in genetic variability in this dominant invasive tree species if these allocation patterns are adaptive.     

Factors influencing communities of foliar fungal endophytes in riparian woody plants

Riparian areas within a given arid region frequently contain broadly similar plant communities despite substantive geographic separation. Whether they also harbor similar communities of fungal symbionts, or feature assemblages unique to each riparian zone, is unknown. We examined fungal endophytes in foliage of woody angiosperms in six riparian areas in Arizona. Abundance and diversity differed among host species according to leaf longevity and phytochemistry, and among sites as a function of rainfall. Community composition varied among sites and host species. Comparison with regional data revealed that riparian areas harbor different subsets of the regional mycota rather than a consistent group of riparian taxa. Overall a high species- and phylogenetic richness of endophytes was recovered, especially among Mycosphaerella and affiliated anamorphs. Variation in endophyte communities across sites despite the relative consistency of plant communities underscores the importance of riparian zones both singly and in combination for harboring fungal biodiversity.     

Philip Miller and the plants from the Chelsea Physic Garden presented to the Royal Society of London, 1723–1796

Summary

From 1723 to 1796 the Society of Apothecaries of London presented annually to the Royal Society of London 50 dried specimens of plants grown the previous year in the Chelsea Physic Garden, this being a condition of Sir Hans Sloane's deed of gift of the Garden to the Apothecaries in 1722. These herbarium specimens are now in the Department of Botany, British Museum (Natural History), London. Many represent plants recorded in successive editions of Philip Miller's Gardeners Dictionary and, together with Miller's own specimens also in the British Museum (Natural History) and Ehret's drawings, may serve to typify binomials published in the 8th edition (1768) of his Dictionary. They were listed from 1723 to 1774 in the Philosophical Transactions of the Royal Society; the lists here contain six long-overlooked binomials Galium verrucosum Huds. (syn. G. valantia Weber), Gypsophila pilosa Huds. (syn. G. porrigens (L.) Boiss), Briza pinnata Huds. (= Demazeria sicula (Jacq.) Dumort.) Euphorbia hispanica Huds. (= E. esula var. lanceolata Gren. & Godron), Pteris cheusanica Curtis (= P. ensiformis Burm. f.) and Saxifraga stolonifera Curtis (syn. S. sarmentosa L.). The deed of conveyance is printed as an appendix.     

Biogéographie et spéciation des Odonates de l’île de la Réunion

Du fait de l’histoire géologique des Mascareignes et des trajectoires cycloniques dans le sud-ouest de l’océan Indien, l’affinité de la faune odonatologique de la Réunion est essentiellement mauricienne. L’étude de la distribution des Odonates en fonction des différents écosystèmes aquatiques de l’île montre que: 1. Les espèces indigènes ayant une vaste répartition géographique se rencontrent essentiellement dans les écosystèmes ouverts de basse et moyenne altitude (de 0 à 800 m d’altitude). Ces écosystèmes peuvent héberger jusqu’à 13 espèces et possèdent les plus fortes densités odonatologiques. 2. La faune odonatologique de la Réunion se distingue de celle des autres îles de la sous-région malgache par la présence de deux espèces continentales cantonnées à des altitudes supérieures à 1000 m. 3. Les espèces endémiques fréquentent surtout les écosystèmes forestiers. Ces écosystèmes ne présentent au plus que cinq espèces de la faune odonatologique de l’île. En définitive, il apparaît donc que la spéciation des Odonates à la Réunion ne se fait pas dans les écosystèmes diversifiés comportant des espèces à large répartition géographique, mais dans un ensemble d’écosystèmes marginaux à faible diversité odonatologique.     

Methanogenesis and Methanogen Diversity in Three Peatland Types of the Discontinuous Permafrost Zone,Boreal Western Continental Canada

Because recent patterns of permafrost collapse in boreal peatlands appear to enhance emissions of CH ₄ to the atmosphere, we examined methanogenesis and methanogen diversity in peat soil from peatlands with and without permafrost in two peatland complexes situated in continental western Canada. Peat soil from the active layer of permafrost bogs had very low rates of CH ₄ production (ca. 10 nmol g ^?1 day ^?1 ), and we were unable to PCR-amplify 16s rRNA gene sequences using Archaea-specific primers in four peat samples. Surface peat soil from continental bogs with no permafrost supported moderate rates of CH ₄ production (20–600 nmol g ^?1 day ^?1 ), with maximum rates in soil located close to the mean water table level. Additions of ethanol stimulated CH ₄ production rates, suggesting metabolic substrate limitations. Peat from internal lawns, which have experienced surface permafrost degradation in the past 150 years, had very rapid rates of CH₄ production (up to 800 nmol g ^?1 day ^?1 ) occurring within the soil profile. Concomitant rates of anaerobic CO ₂ production were greater in continental bogs (ca. 6 μmol g ^?1 day ^?1 ) than in internal lawns (ca. 4 μ mol g ^?1 day ^?1 ) or in permafrost bogs (2.8 μ mol g ^?1 day ^?1 ). Analysis of the 16s rRNA gene for Archaea in the continental bog indicated mostly sequences associate with Methanobacteriales and RC-I with a Methanosarcinaceae sequence in the deepest peat soil. In the internal lawn, Methanosarcinaceae were most common in peat soil with a Methanosaetaceae sequence in the deepest peat soil. This study showed that patterns of discontinuous permafrost and ongoing permafrost degradation in boreal regions create patchy soil environments for methanogens and rates of methanogenesis.     

Dynamics of amino acids in the conditioning film developed on glass panels immersed in the surface seawaters of Dona Paula Bay

The conditioning film developed on glass panels immersed in surface seawater over a period of 24?h was analysed for total organic carbon (OC), total organic nitrogen (ON), and total hydrolyzable amino acid (THAA) concentrations and composition. The concentrations of C and N and THAA increased, whereas the C/N ratio decreased over the period of immersion. The amino acid-C and N accounted for 3.7?–?6.7% and 10.3?–?65.3% of OC and ON, respectively. The relative contribution of glycine plus threonine and serine to the total amino acids decreased while that of valine, phenylalanine, isoleucine and leucine increased over the period of immersion. Principal component analysis (PCA) based on mole% amino acid composition showed that the degradation indices (DI) for the conditioning film organic matter increased over the period of immersion. A high C/N ratio, a low %THAA-C, % THAA-N and DI values and the abundance of glycine plus threonine and serine in the conditioning film organic matter during the first few hours following immersion imply that the adsorbed organic matter was mostly derived from degraded organic matter.     

强度干扰后退化森林生态系统中保留木的生态效应研究综述

保留木是指森林生态系统受到强度干扰后所存留的树木,保留木对退化森林生态系统结构与功能的维持和恢复具有多方面的生态效应。在生态系统的尺度上总结了退化森林生态系统中保留木的各种生态效应,主要包括保留木对非生物因子和生物因子(附生生物多样性、动物活动和动物多样性、树木更新、空间结构)的影响。森林生态系统经营中,"绿树保留"的经营方式是基于保留木生态效益的实践应用,它可有效减少采伐对生态系统结构和功能所造成的损失。并将有助于深入理解受到强度干扰后森林生态系统中保留木的多种生态效应,可为退化森林生态系统的恢复与重建提供理论依据。     

近40年青藏高原生态格局演变及其驱动因素

20世纪80年代至今近40年间,青藏高原自然与人工生态系统发生了广泛而深刻的变化,作为我国重要的生态屏障,亟需对其生态系统格局演变过程及其驱动因素进行系统定量的解析。本研究利用1980年至2018年间8期遥感解译土地利用与覆被数据,将青藏高原9类主要生态系统类型,森林、灌丛、草地、农田、城镇、水体与湿地、冰川、裸地、荒漠,依其主要构成组分,划分为以植被为主体的自然生态系统（森林、灌丛、草地）、以无机环境为主体的自然生态系统（水体与湿地、冰川、裸地、荒漠）,以及人工生态系统（农田、城镇）共三大类。统计分析表明1980至2018年的近40年来,青藏高原以植被为主的自然生态系统面积约占61.9%,其中草地生态系统变化率较大,局部年际变化逾30%/10a,草地灌丛面积扩张明显,最高可达约7%/10a。此外,青藏高原喜马拉雅山脉附近的冰川消减较快,下降速率约达25%/10a。青藏高原东缘向西城镇扩张明显,城镇面积占比增加约40%。研究还对气温和降水计算其变化速率,量化驱动生态系统演变的外部气候环境的时空动态特征,结合地理环境变量、人类活动强度、土壤侵蚀度、生物丰度等综合的驱动因素指标,建立多层级结构方程模型。研究发现,以植被为主的自然生态系统变化速率与气温、降水的变化速率呈现显著负相关,以无机环境要素为主的自然生态系统与气候因子的变化速率呈现显著正相关,人工生态系统则与外部环境因素耦合关系不强,结果表明青藏高原森林、灌丛、草地一类自然植被生态系统与环境变化之间呈现负反馈的保守性耦合关系,相比较水体与湿地、冰川、裸地和荒漠生态系统来讲,具有更强的韧性,因此保护区域自然植被将有利于维护青藏高原整体的生态屏障功能。     

草菇不同菌株RT-qPCR参考基因筛选

适合的参考基因是应用实时荧光定量PCR (RT-qPCR)技术进行基因表达分析的前提。本研究以7个食用菌常用参考基因(β-TUB 1、GPD、ACTB、Ras、α-TUB、β-TUB 2和SPRYp)为候选基因,利用RT-qPCR检测其在草菇常用生产菌株(CPS)V844、V5、V971和V844继代退化菌株(SDS) T8、T12、T16、T20中的表达;用Genorm、NormFinder和BestKeeper 3种软件分析候选基因的表达稳定性,并结合几何平均数法筛选出最佳参考基因。结果表明,SPRYp、α-TUB和β-TUB 2基因适用于草菇常用生产菌株检测,SPRYp、GPD和α-TUB基因适用于草菇继代退化检测,SPRYp基因适用于两种条件的检测。两两差异分析表明,草菇常用生产菌株的最佳参考基因组合为SPRYp、α-TUB和β-TUB 2,继代退化菌株的最佳参考基因组合为SPRYp和GPD,两种条件混合菌株的最佳参考基因组合为SPRYp和α-TUB。     

Climate-induced long-term changes in the phenology of Mediterranean fungi

Long-term responses in the phenology of Mediterranean macrofungi to climatic changes are poorly documented. Here, we address this issue by comparing the fruiting patterns of 159 fungal species in Southern France between the first half of the 19th century and the first decade of the 21st century. We used a trait-based approach to assess the influence of phenology and morphology of fungal fruit bodies and their site ecology and biogeography on the response to climate change. We show that early autumnal fruiters, epigeous species and species with affinities for cold climates now start to fruit on average 16.4, 17.3 and 17.3 d later compared to their emergence dates in the 19th century, while late fruiters, hypogeous species and Mediterranean-restricted species did not change their fruiting date. Among ecological guilds, saproxylic species and pine-associated mutualists delayed their autumnal emergence by 32.5 and 19.2 d, likely in response to a delayed rewetting of litter and woody debris after extended summer drought. Our results suggest that long-term climate warming in the Mediterranean was accompanied by contrasting changes in the emergence of fungal fruit bodies according to ecological guilds, sporocarp life-forms and forest types.