Evaluierung und Optimierung biologischer Verfahren zur Regulierung des Pflaumenwicklers (Cydia funebrana) und der Monilia-Krankheit im ökologischen Steinobstanbau

Im Verbundforschungsprojekt FKZ 06OE198, FKZ 06OE057 und FKZ 06OE348 wurden Möglichkeiten der Regulierung des Pflaumenwicklers (Cydia funebrana) an Zwetschgen in Labor-, Halbfreiland und Freilandversuchen in Geisenheim, Darmstadt, Klein-Altendorf und Weinsberg untersucht. Labor- und Freilandversuche zur Regulierung der Monilia-Krankheit wurden in Geisenheim, Weinsberg und Dresden durchgeführt. Sauerkirschsorten-Versuche sind in Weinsberg und Dresden aufgepflanzt. Umfangreiche Freilandversuche zur Verwirrung des Pflaumenwicklers mit „Isomate OFM Rosso“ in Baden-Württemberg und Rheinland-Pfalz bestätigten mit Wirkungsgraden von bis zu 70 % die Wirksamkeit dieser Methode bei ausreichend großen Flächen und niedrigem Befallsniveau. Für den kleinparzellierten Anbau und bei höherem Befallsdruck wurden entomopathogene Nematoden im Freiland gegen überwinternde Larven mit heterogenen Wirkungsgraden erprobt. Es gelang nicht Pflaumenwickler ganzjährig unter Laborbedingen zu züchten, jedoch wurden mit Tieren aus Freilandsammlungen bzw. deren Eiern nach der Überwinterung Versuche zur Infektion der neonaten Larven mit dem Apfelwicklergranulosevirus, Eiparasitierungsversuche mit Trichogramma cacoeciae, zu Applikationen mit NeemAzal-T/S und zum Einsatz von insektenpathogen Pilzen gegen überwinternde Larven durchgeführt. Bei weiterführenden Versuchen im Freiland wurden mit dem Apfelwicklergranulosevirus V15 sehr heterogene Ergebnisse erzielt. Der Einsatz von Trichogramma in Form von Trichokarten ergab Wirkungsgrade von bis zu 47 %. Eine bessere Verteilung der Trichogramma in der Anlage sollte mit einer spritzfähigen Formulierung erreicht werden, dafür liegen jedoch erst einjährige Ergebnisse vor. Für die Bekämpfung der überwinternden Pflaumenwickler mit insektenpathogenen Pilzen stellte sich Isaria fumosorosea, als am geeignetsten heraus. Jedoch gestaltete sich bisher ein Nachweis der Wirksamkeit des mit dem Pilz infizierten Mulches im Freiland sehr schwierig. Die Pflaumenwicklerlarve sucht sich zur Überwinterung kleinste Ritzen am Stamm aus. Mit Wellpappe, die um den Stamm gewickelt wurde, konnte den Larven ein attraktives Überwinterungsquartier angeboten werden. Durch Entfernen und Verbrennen der Pappringe im Winter kann der Befallsdruck im Folgejahr minimiert werden. Für die Monilia-Regulierung an Zwetschgen konnte im Labor unter einer Vielzahl an getesteten Präparaten lediglich Serenade mit einer antagonistischen Wirkung überzeugen. Es hat jedoch keine Zulassung als Pflanzenschutzmittel im Steinobst. Versuche im Freiland ergaben außerdem, dass das konsequente Eliminieren von möglichen Infektionsquellen durch das Entfernen von Monilia-Nestern vor der Ernte und von Fruchtmumien nach der Ernte letztlich bessere Effekte erzielte, als Behandlungen mit mittelgut wirksamen Pflanzenstärkungsmitteln. Für die Behandlung der Monilia-Spitzendürre an Sauerkirschen wurden verschiedene Präparate im Freiland überprüft. Die Handelsprodukte BoniProtect® forte und BoniProtect® reduzierten tendenziell die Blüteninfektionen. Da für SPU 2720 und Cuprozin bisher nur aus einem Jahr Versuchsergebnisse vorliegen, ist keine abschließende Beurteilung möglich. Jedoch lässt sich bereits durch den konsequenten Rückschnitt befallener Triebe der Befallsdruck erheblich reduzieren. An beiden Standorten erscheinen die Sauerkirschsorten ‘Morina‘, ‘Jade‘, ‘Coralin‘ und ‘Safir‘ als geeignet für den ökologischen Anbau, in Weinsberg zusätzlich ‘Topas‘ und ‘Ungarische Traubige‘. Allerdings war der Monilia-Druck nur in wenigen Jahren hoch. Bis jetzt wurden keine Infektionen mit Gloeosporium sp., einer weiteren bedrohlichen Krankheit im ökologischen Sauerkirschanbau, beobachtet

Holocene wildfire regimes in forested peatlands in western Siberia: interaction between peatland moisture conditions and the composition of plant functional types

Wildfire is the most common disturbance type inboreal forests and can trigger significant changes in forestcomposition. Waterlogging in peatlands determines the degree of tree cover and the depth of the burnt horizon associated with wildfires. However, interactions between peatland moisture, vegetation composition and flammability, andfire regime in forest and forested peatland in Eurasia remain largely unexplored, despite their huge extent in borealregions. To address this knowledge gap, we reconstructedthe Holocene fire regime, vegetation composition, and peatland hydrology at two sites located in predominantly lighttaiga (Pinus sylvestris Betula) with interspersed dark taigacommunities (Pinus sibirica, Picea obovata, Abies sibirica)in western Siberia in the Tomsk Oblast, Russia. We foundmarked shifts in past water levels over the Holocene. Theprobability of fire occurrence and the intensification of firefrequency and severity increased at times of low water table(drier conditions), enhanced fuel dryness, and an intermediate dark-to-light taiga ratio. High water level, and thus wetpeat surface conditions, prevented fires from spreading onpeatland and surrounding forests. Deciduous trees (i.e. Betula) and Sphagnum were more abundant under wetter peatland conditions, and conifers and denser forests were moreprevalent under drier peatland conditions. On a Holocenescale, severe fires were recorded between 7.5 and 4.5 ka withan increased proportion of dark taiga and fire avoiders (Pinussibirica at Rybnaya and Abies sibirica at Ulukh–Chayakh)in a predominantly light taiga and fire-resister communitycharacterised by Pinus sylvestris and lower local water level.Severe fires also occurred over the last 1.5 kyr and were associated with a declining abundance of dark taiga and fireavoiders, an expansion of fire invaders (Betula), and fluctuating water tables. These findings suggest that frequent,high-severity fires can lead to compositional and structuralchanges in forests when trees fail to reach reproductive maturity between fire events or where extensive forest gaps limitseed dispersal. This study also shows prolonged periods ofsynchronous fire activity across the sites, particularly duringthe early to mid-Holocene, suggesting a regional imprint ofcentennial- to millennial-scale Holocene climate variabilityon wildfire activity. Humans may have affected vegetationand fire from the Neolithic; however, increasing human presence in the region, particularly at the Ulukh–Chayakh Mireover the last 4 centuries, drastically enhanced ignitions compared to natural background levels. Frequent warm and dryspells predicted by climate change scenarios for Siberia inthe future will enhance peatland drying and may convey acompetitive advantage to conifer taxa. However, dry conditions will probably exacerbate the frequency and severityof wildfire, disrupt conifers’ successional pathway, and accelerate shifts towards deciduous broadleaf tree cover. Furthermore, climate–disturbance–fire feedbacks will acceleratechanges in the carbon balance of boreal peatlands and affecttheir overall future resilience to climate chang

Herd-level animal management factors associated with the occurrence of bovine neonatal pancytopenia in calves in a multicountry study

Since 2007, mortality associated with a previously unreported haemorrhagic disease has been observed in young calves in several European countries. The syndrome, which has been named ‘bovine neonatal pancytopenia’ (BNP), is characterised by thrombocytopenia, leukocytopenia and a panmyelophthisis. A herd-level case-control study was conducted in four BNP affected countries (Belgium, France, Germany and the Netherlands) to identify herd management risk factors for BNP occurrence. Data were collected using structured face-to-face and telephone interviews of farm managers and their local veterinarians. In total, 363 case farms and 887 control farms were included in a matched multivariable conditional logistic regression analysis. Case-control status was strongly associated with the odds of herd level use of the vaccine PregSure® BVD (PregSure, Pfizer Animal Health) (matched adjusted odds ratio (OR) 107.2; 95% CI: 41.0–280.1). This was also the case for the practices of feeding calves colostrum from the calf’s own dam (OR 2.0; 95% CI: 1.1–3.4) or feeding pooled colostrum (OR 4.1; 95% CI: 1.9–8.8). Given that the study had relatively high statistical power and represented a variety of cattle production and husbandry systems, it can be concluded with some confidence that no other herd level management factors are competent causes for a sufficient cause of BNP occurrence on herd level. It is suggested that genetic characteristics of the dams and BNP calves should be the focus of further investigations aimed at identifying the currently missing component causes that together with PregSure vaccination and colostrum feeding represent a sufficient cause for occurrence of BNP in calves

On the Interplay of Telomeres, Nevi and the Risk of Melanoma

The relationship between telomeres, nevi and melanoma is complex. Shorter telomeres have been found to be associated with many cancers and with number of nevi, a known risk factor for melanoma. However, shorter telomeres have also been found to decrease melanoma risk. We performed a systematic analysis of telomere-related genes and tagSNPs within these genes, in relation to the risk of melanoma, dysplastic nevi, and nevus count combining data from four studies conducted in Italy. In addition, we examined whether telomere length measured in peripheral blood leukocytes is related to the risk of melanoma, dysplastic nevi, number of nevi, or telomere-related SNPs. A total of 796 cases and 770 controls were genotyped for 517 SNPs in 39 telomere-related genes genotyped with a custom-made array. Replication of the top SNPs was conducted in two American populations consisting of 488 subjects from 53 melanoma-prone families and 1,086 cases and 1,024 controls from a case-control study. We estimated odds ratios for associations with SNPs and combined SNP P-values to compute gene region-specific, functional group-specific, and overall P-value using an adaptive rank-truncated product algorithm. In the Mediterranean population, we found suggestive evidence that RECQL4, a gene involved in genome stability, RTEL1, a gene regulating telomere elongation, and TERF2, a gene implicated in the protection of telomeres, were associated with melanoma, the presence of dysplastic nevi and number of nevi, respectively. However, these associations were not found in the American samples, suggesting variable melanoma susceptibility for these genes across populations or chance findings in our discovery sample. Larger studies across different populations are necessary to clarify these associations

Fire hazard modulation by long-term dynamics in land cover and dominant forest type in eastern and central Europe

Wildfire occurrence is influenced by climate, vegetation and human activities. A key challenge for understanding the risk of fires is quantifying the mediating effect of vegetation on fire regimes. Here, we explore the relative importance of Holocene land cover, land use, dominant functional forest type, and climate dynamics on biomass burning in temperate and boreo-nemoral regions of central and eastern Europe over the past 12 kyr. We used an extensive data set of Holocene pollen and sedimentary charcoal records, in combination with climate simulations and statistical modelling. Biomass burning was highest during the early Holocene and lowest during the mid-Holocene in all three ecoregions (Atlantic, continental and boreo-nemoral) but was more spatially variable over the past 3–4 kyr. Although climate explained a significant variance in biomass burning during the early Holocene, tree cover was consistently the highest predictor of past biomass burning over the past 8 kyr. In temperate forests, biomass burning was high at ~ 45% tree cover and decreased to a minimum at between 60% and 70% tree cover. In needleleaf-dominated forests, biomass burning was highest at ~60 %–65%tree cover and steeply declined at > 65% tree cover. Biomass burning also increased when arable lands and grasslands reached ~15 %–20 %, although this relationship was variable depending on land use practice via ignition sources, fuel type and quantities. Higher tree cover reduced the amount of solar radiation reaching the forest floor and could provide moister, more wind-protected microclimates underneath canopies, thereby decreasing fuel flammability. Tree cover at which biomass burning increased appears to be driven by warmer and drier summer conditions during the early Holocene and by increasing human influence on land cover during the late Holocene. We suggest that longterm fire hazard may be effectively reduced through land cover management, given that land cover has controlled fire regimes under the dynamic climates of the Holocene

Modeling the multi-functionality of African savanna landscapes under global change

Various recent publications have indicated that accelerated global change and its negative impacts on terrestrial ecosystems in Southern Africa urgently demand quantitative assessment and modelling of a range of ecosystem services on which rural communities depend. Information is needed on how these Ecosystem Services (ES) can be enhanced through sustainable land management interventions and enabling policies. Yet, it has also been claimed that, to date, the required system analyses, data and tools to quantify important interactions between biophysical and socio-economic components, their resilience and ability to contribute to livelihood needs do not exist. We disagree, but acknowledge that building an appropriate integrative modelling framework for assessing the multi-functionality of savanna landscapes is challenging. Yet, in this Letter-to-the-Editor, we show that a number of suitable modelling components and required data already exist and can be mobilized and integrated with emerging data and tools to provide answers to problem-driven questions posed by stakeholders on land management and policy issues.German Federal Ministry of Education and Researchhttps://onlinelibrary.wiley.com/journal/1099145xhj2022Zoology and Entomolog

Rolle der Savannen der Erde und ihre Gefährdung

Tropische Savannen bedecken ca 20% der Landoberfläche und sind durch die Koexistenz von Gräsern und holziger Vegetation definiert. Savannen stellen viele Ökosystemleistungen wie Nahrungsmittel oder Baumaterial bereit, die als Lebensgrundlage für Menschen von Bedeutung sind. Darüber hinaus speichern Savannen einen erheblichen Anteil an Kohlenstoff und beherbergen eine hohe Biodiversität. Klimawandel, Intensivierung der Landnutzung durch Bevölkerungswachstum und das Verdrängen von Savannen durch landwirtschaftliche Flächen und Plantagen bedrohen die Verbreitung und Biodiversität von Savannen. Aufgrund der weiten Verbreitung von Savannen und ihrer vielfältigen Nutzung stellt der Erhalt von Savannen in Zukunft eine große Herausforderung dar, da vielfältige Interessen berücksichtigt werden müssen. The role of the earth‘s savannahs and their endangerment: Tropical savannas cover about 20% of the land surface and are defined by the coexistence of grasses and woody vegetation. Savannas provide many ecosystem services such as food or building materials, which are important for the livelihood of humans. In addition, savannas store a significant amount of carbon and harbor high biodiversity. Climate change, intensifica- tion of land use due to an increase in the human population, and the replacement of savannas by agricultural land and plantations threaten the distribution and biodiversity of savannas. Due to the widespread distribution of savannas and their diverse use, the conservation of savannas in the future is a major challenge, as multiple interests need to be reconciled. El papel de las sabanas terrestres y su peligro: Las sabanas tropicales cubren alrededor del 20% de la superficie terrestre y se definen por la coexistencia de pastos y vegetación leñosa. Las sabanas proporcionan muchos servicios ecosistémicos, como alimentos o materiales de construcción, que son importantes como base de la vida de los seres humanos. Además, las sabanas almacenan una cantidad significativa de carbono y albergan un alto nivel de biodiversidad. El cambio climático, la intensificación del uso de la tierra debido al crecimiento de la población y la sustitución de las sabanas por tierras agrícolas y plantaciones amenazan la expansión y la biodiversidad de las sabanas. Debido al uso generalizado de las sabanas y sus diversos usos, la preservación de éstas es un gran desafío para el futuro, ya que se deben tener en cuenta los diversos intereses

SPITFIRE-2 : an improved fire module for dynamic global vegetation models

Fire is the primary disturbance factor in many terrestrial ecosystems. Wildfire alters vegetation structure and composition, affects carbon storage and biogeochemical cycling, and results in the release of climatically relevant trace gases, including CO2, CO, CH4, NO and aerosols. Assessing the impacts of global wildfire on centennial to multimillennial timescales requires the linkage of process-based fire modeling with vegetation modeling using Dynamic Global Vegetation Models (DGVMs). Here we present a new fire module, SPITFIRE-2, and an update to the LPJ-DGVM that includes major improvements to the way in which fire occurrence, behavior, and the effect of fire on vegetation is simulated. The new fire module includes explicit calculation of natural ignitions, the representation of multi-day burning and coalescence of fires and the calculation of rates of spread in different vegetation types, as well as a simple scheme to model crown fires. We describe a new representation of anthropogenic biomass burning under preindustrial conditions that distinguishes the way in which the relationship between humans and fire are different between hunter-gatherers, obligate pastoralists, and farmers. Where and when available, we evaluate our model simulations against remote-sensing based estimates of burned area. While wildfire in much of the modern world is largely influenced by anthropogenic suppression and ignitions, in those parts of the world where natural fire is still the dominant process, e.g. in remote areas of the boreal forest, our results demonstrate a significant improvement in simulated burned area over previous models. With its unique properties of being able to simulate preindustrialfire, the new module we present here is particularly well suited for the investigation of climate-human-fire relationships on multi-millennial timescales