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- 'bottom–up' and 'top–down' processes (1)
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- (Euliina) (1)
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- 1977 (wing lustre, new combination) (1)
- 1992. Heliogomphus sp (1)
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- 2006 (1)
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- 28S phylogeny (1)
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- crapemyrtle scale (1)
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Von 1994 bis 2003 erfassten wir in einem Braunschweiger Untersuchungsgebiet die Brutbesiedlung von Nistkastenrondellen (jeweils 8 Höhlen rings um einen Eichenstamm). Wenn ein Rondell im selben Jahr von 2 Brutpaaren genutzt wurde, ging in die Auswertung nur die Wahl des Erstbesiedlers ein. Erstbesiedler waren 74 x Kohlmeisen Parus major, 7 x Blaumeisen Parus caerulus, 28 x Kleiber Sitta europaea, 34 x Trauerschnäpper Fidecula hypoleuca und 4 x Stare Sturnus vulgaris. Die meisten dieser Paare wählten Nisthöhlen, deren Eingang nach Osten (NE, E, SE) zeigte. Die stärkste Bevorzugung für den wetterabgewandten Ostsektor ließ sich bei Fidecula hypoleuca feststellen. Bei Nistkästen mit nach Osten weisendem Einflugloch dürfte das Risiko für Brutverluste durch Feuchtigkeit und/oder Überhitzung minimiert werden. Allerdings kann das Ergebnis der experimentellen Studie nicht auf die Situation von Naturhöhlen übertragen werden. Denn in benachbarten Waldparzellen waren die vom Star zur Brut genutzten Naturhöhlen (n = 72) bevorzugt in westliche Richtungen orientiert. Sekundäre Höhlenbrüter können ihre Präferenz hinsichtlich der Ausrichtung des Höhleneingangs unter natürlichen Verhältnissen offenbar nur eingeschränkt oder gar nicht realisieren, weil sich das Naturhöhlenangebot witterungsbedingt vor allem im S/SW-Sektor befindet.
Die bedeutendste Entdeckung der letzten 30 Jahre in Bezug auf das Fortpflanzungsverhalten von Vögeln war die Erkenntnis, dass es bei mehr als 80% aller sozial monogamen Singvogelarten regelmäßig zu Kopulationen außerhalb des Paarbundes kommt („extra-pair copulations“; EPCs). In der Folge setzte sich eine beeindruckende Zahl von Untersuchungen mit verschiedenen Aspekten dieses Verhaltens auseinander. Neben Studien, die sich mit Unterschieden in der Häufigkeit des Auftretens von „Fremdvaterschaften” bei verschiedenen Vogelarten beschäftigten, wurden vor allem Untersuchungen zum Kosten und Nutzen von EPCs für Männchen und Weibchen durchgeführt. Auf der Basis eigener Untersuchungen, die dazu dienten, das genetische Paarungssystem von sozial monogamen Kohl- und Tannenmeisen (Parus major and P. ater) zu ergründen, werden hier einige Resultate dieser Bemühungen und auch die ihnen zugrundeliegenden Überlegungen dargestellt. Kosten von EPCs beinhalten für Weibchen möglicherweise eine Reduktion in der Brutfürsorge durch die Männchen, weil die Anzahl eigener Nachkommen und damit der Fortpflanzungswert einer Brut für „betrogene“ Männchen abnimmt. In Übereinstimmung mit dieser Hypothese fanden wir, dass sich die Brutverteidigung männlicher Kohlmeisen nach der Anzahl eigener Nachkommen und nicht nach der Brutgröße richtet. Außerdem fütterten „betrogene“ Männchen ihre Bruten weniger als nicht „betrogene“ Männchen. Wenn EPCs den Weibchen Kosten verursachen, so muss auf der anderen Seite ein entsprechender Nutzen vorhanden sein, da Selektion sonst zum Verschwinden dieses Verhaltens führen sollte. Während männliche Kohl- und Tannenmeisen ihren Fortpflanzungserfolg durch EPCs direkt erhöhen können, ist ein Nutzen für die Weibchen nicht derart offensichtlich. Bei der Analyse einer großen Zahl von Tannenmeisenbruten konnten wir keinerlei Hinweis dafür finden, dass die vieldiskutierten „Gute Gene”-Modelle den Nutzen von EPCs für Weibchen erklären. Würden Weibchen durch EPCs „bessere“ oder „kompatiblere“ väterliche Gene für die betreffenden Nachkommen erhalten, wäre zu erwarten, dass EPY ihren Halbgeschwistern in irgendeiner Form überlegen sind. Zwischen den beiden Halbgeschwistergruppen fand sich jedoch weder in Bezug auf die Überlebenswahrscheinlichkeit noch in Bezug auf den Fortpflanzungserfolg im ersten Brutjahr ein Unterschied. Aus diesen und anderen Befunden wird geschlossen, dass „Gute Gene”-Modelle das weit verbreitete Auftreten von EPCs bei Vögeln alleine kaum erklären können und dass wahrscheinlich mehr als ein einzelner Selektionsfaktor die Evolution dieses Verhaltens bei Vögeln beeinflusst hat.
The German Working Group on Vegetation Databanks has held annual meetings since 2002 with financial support by the German Federal Agency for Nature Conservation. Ca. 215 members are regularly informed through a mailing-list. The 2008 meeting was hosted by University of Oldenburg’s Landscape Ecology Group and was attended by 72 participants from 15 countries. Software demonstrations of vegetation databanks Turboveg and VegetWeb as well as plant trait databanks LEDA and BiolFlor opened the workshop. There were lecture sessions on trait databanks, recalibration of ecological indicator values and new developments in the field of vegetation databanks. Working groups were devoted to an initiative to build a meta-databank of existing vegetation databanks in Germany and to mathematical modelling of species habitats. In 2009 the 8th workshop will be held on "Vegetation Databanks and Biodindication" at the University of Greifswald.
Naturalness is one of the most important criteria in nature conservation. This paper examines the fundamental concepts underlying the definition and assessment of naturalness. Its role in nature conservation and forest management under conditions of global change is also discussed. The degree of naturalness may be defined in ordinal classes. The “static” concept of the potential natural vegetation (pnV), developed in the 1950ies, is mostly used as the reference state. In other cases, its reversed concept, the hemeroby (degree of articifiality) is assessed, based on the intensity and frequency of human impacts. Since the 1970ies, more attention has been given to natural dynamics than in earlier approaches, e.g. in forest succession models. At the end of the 1980ies, the previous importance was increasingly stressed of natural browsing by large herbivores and the role of predators. These large herbivors are extinct today in most cultural European landscapes. It is assumed, that they open up the canopy, and create park-like forest structures which contain a diversity of habitats for other types of organism (birds, insects). Changed and permanently changing environments and altering patterns of competition between species continue to modify natural processes today. Some of the more conspicuous effects are the extinction of native species and immigration of species to new regions. Long-lived ecosystems like forests are however not able to adapt quickly to such changes and may be unable to find a new balance with the environment. Today, such changes occur very rapidly, and are reducing the original naturalness of ecosystems. Because of this, the criterion “naturalness” must be downweighted. Conversely, more importance should be attached to other criteria: particularly originality (= original naturalness) and restorability. Forestry is contributing to this accelerated change of biocoenoses by increasing disturbances and introducing exotic tree species. Naturalisation of some exotic tree species modifies the natural processes and creates a “new allochthonous naturalness”. Because of this, forest planning should try to preserve or restore stands with attributes of the “original forest”. Exotic species should not be planted, or only in a very restricted way.
Anhand der Daten von 33 Standorten des Bayerischen Waldboden Dauerbeobachtungsprogramms (Bodendauerbeobachtungsflächen, BDF) wurden die durch kleinräumige Variabilität verursachten Unsicherheiten bei der Charakterisierung von Böden geschätzt. Diese Datenbasis erlaubte es zudem zu untersuchen, inwieweit geostatistische Eigenschaften in Zusammenhang mit den Standortsbedingungen stehen. Für diesen Zweck entwickelten wir einen einfachen Ansatz zur Typisierung von Böden nach ihren räumlichen Eigenschaften. Beim BDF-Programm wurden auf jedem Standort 18 Proben in einem Kreuz-Transekt 18 x 18 m entnommen bei einem Mindestabstand von 3 m. Der Datenbestand umfasst die Parameter Corg und Ntot-Konzentrationen sowie -Vorräte und C / N - Verhältnis, effektive Kationen-Austausch-Kapazität (Ake), Basensättigung (BS), pH-Wert des Bodens und Grobbodenfraktion (> 2 mm). In die Metaanalyse wurden pro Bodenparameter 3780 Datensätze zur Erzeugung aggregierter Kennwerte einbezogen wie Schiefe, Variationskoeffizient (VK), Moran‘s I und den Anteil der räumlich strukturierten Varianz (SV) der Daten. Die beobachtete räumliche Struktur von Bodenparametern konnte zwar nicht eindeutig in Zusammenhang mit den Standortbedingungen gebracht werden. Es zeigt sich aber, dass die Gesamtvarianz einiger Parameter mit steigendem Tongehalt tendenziell zurück geht und dass das Niveau der Streuung (VK) der untersuchten Boden-Parameter sich erheblich unterscheidet. Die Rangfolge der Parameter hinsichtlich der Streuung ist pH-Wert (1), C/N - Verhältnis (2), C und N-Konzentration (3a), BS und Ake (3b), C- und N- Vorräte (4). Die Unsicherheitsabschätzung anhand der BDF Daten findet Eingang in das Fehlerbudget der zweiten bundesweiten Bodenzustandserhebung im Wald (BZE II) und dient dazu die Chancen zu bestimmen mit denen etwaige Bodenveränderungen nachgewiesen werden können.
Zur Kennzeichnung und Gliederung von periglaziär bedingten Differenzierungen in der Pedosphäre
(2008)
Im periglaziären Milieu der letzten Kaltzeit wurde der oberflächennahe Tiefenbereich in Mitteleuropa entscheidend geprägt, was durch lithogene und pedogene Differenzierungen bis etwa 1...2 m unter Gelände zum Ausdruck kommt. Die Prozesse Kryoklastik und Kryotranslokation, Kryoperstruktion sowie Kryopedogenese – jeweils mit mehreren Teilprozessen – prägten die Profilgliederung und Substratausbildung in der Auftauzone des Dauerfrostbodens. In den Untersuchungen und Diskussionen der letzten Jahrzehnte zur Genese der Phänomene im Bereich der Pedosphäre erfuhren die beteiligten Prozesse bei den Autoren unterschiedliche Aufmerksamkeit und Sichtung. Die verschiedenen Konzepte zur Kennzeichnung und Gliederung der Profildifferenzierungen lassen sich letztlich dem Deckenkonzept, im Wesentlichen fußend – jedoch unter Beteiligung weiterer Prozesse – auf Kryotranslokation sowie dem Konzept der Perstruktions- bzw. Umlagerungszonen, vorrangig basierend auf den Prozessen Kryoperstruktion und Kryopedogenese, zuordnen. Der entscheidende Unterschied zwischen der Ansprache der periglaziär bestimmten Differenzierungen innerhalb der Pedosphäre mit Hilfe der Abfolge verschiedener Zonen einerseits und der Abfolge verschiedener Decken – wie auch Lagen – andererseits besteht darin, dass bei der Kennzeichnung und Gliederung des Zonenprofils sedimentär bedingte Substratunterschiede nicht vorrangig und nur als Hilfskriterien herangezogen und somit gleiche Zonen auch in lithostratigraphisch unterschiedlichem Material oder auch umgekehrt in gleichem Material verschiedene Zonen ausgewiesen werden. Nach dem Decken-/Lagenkonzept werden dagegen die sedimentären Prozesse als dominante Ursachen der heute vorliegenden vertikalen Substratdifferenzierung angesehen, wobei auch den syn- und postsedimentären periglaziären Umbildungen durch Teilprozesse der Kryoperstruktion immerhin entscheidender Anteil am Deckenbildungsprozess beigemessen wird, die zur zusätzlichen Vertikaldifferenzierung innerhalb der jeweiligen Decke führen können. Zur Definition der Lagen (nach der Kartieranleitung der Staatlichen geologischen Dienste und der Bundesanstalt für Geowissenschaften und Rohstoffe) wurden die Prozesse der Kryotranslokation sowie Teilprozesse der Kryoperstruktion herangezogen, jedoch sind bisher die Kryohomogenisierung (Entschichtung, Vermischung) und (Skelett-)Umsortierung (Kryolithotropie) sowie außerdem die mit der Kryoperstruktion häufig verknüpften Prozesse der Kryopedogenese in die Definition nicht eingegangen. In vielen Fällen ist eine Zuweisung der Profile zu einem bestimmten Gliederungsprinzip bzw. Genesetyp nicht möglich. So ist es nicht haltbar, von regional abgegrenzten Gebieten sowie räumlichen Insellagen der Entstehung von periglaziären Decken einerseits und von Bereichen mit Ausbildung von Kryoperstruktionszonen andererseits zu sprechen. Im periglaziären Milieu wirkten die o. g. jeweils unterschiedlich dominanten Vorgänge im Komplex, und die Abkopplung von Teilprozessen der periglaziären Umbildung der Oberfläche ist nicht sinnvoll. Das für die Böden ausgewiesene Substratprofil baut sich aus erheblich variierenden Anteilen des durch Kryotranslokation akkumulierten Fremdmaterials sowie des ortsbürtigen Materials auf. Die jeweiligen Komponenten wurden im Wesentlichen durch das örtlich anstehende Gestein und Relief, die Exposition und Höhenlage sowie die Lage zum Eisrand und zu den äolischen Akkumulationsräumen gesteuert. Im Zuge einer Analyse der oberflächennahen Profildifferenzierungen ist durchaus die detaillierte Kennzeichnung des Substratprofils nach fremden und ortsbürtigen Komponenten einerseits sowie nach Merkmalen der Kryoperstruktion andererseits möglich. Darüber hinaus ist aber eine integrierende und aggregierende sowie landschaftsübergreifende Gliederung und Kennzeichnung der periglaziär bedingten Profildifferenzierungen notwendig. Dafür ist der Begriff „Lage“ nach bisheriger Definition nur bedingt geeignet, da dieser nicht die Beteiligung des gesamten Prozesskomplexes ausdrückt. Deshalb wird zur Unterscheidung vorerst der Neubegriff „Segment“ (bzw. periglaziäres Segment) vorgeschlagen, der hinsichtlich Kryoperstruktions-, Kryotranslokations- und Kryohorizontprofil neutral ist und somit keinen Anlass für nomenklatorische Missverständnisse bietet. Bei der Weiterverwendung der Bezeichnung „Lagen“ im Sinne einer hier vorgeschlagenen ergänzenden Definition ist also nicht nur dessen neue Begriffsbestimmung erforderlich, sondern darüber hinaus auch eine Klarstellung, dass die so ergänzt definierten Lagen nach allen genannten Prozesssystemen – also erweitert gegenüber der bisherigen Lagendefinition – gekennzeichnet sind. Sofern dies mit allen Konsequenzen allgemein verbindlich würde, könnte allerdings der Lagenbegriff mit dem Zusatz „Lage – ergänzt definiert“ auch weiterhin angewandt werden. Die periglaziären Segmente bzw. die Lagen – ergänzt definiert – lassen sich folgendermaßen kennzeichnen: Periglaziäre Segmente (kurz: Segmente) oder Lagen – ergänzt definiert – sind im periglaziären Milieu im Bereich der Pedosphäre durch • Substratbereitstellung infolge Frostverwitterung (Kryoklastik) und Kryotranslokation [äolische Akkumulation und/oder (Geli-)Solifluktion bzw. Anspülung] aus den jeweils anstehenden Gesteinen sowie aus unterschiedlichen Anteilen allochthonen Materials und • durch Kryoperstruktion (Entschichtung und Homogenisierung sowie Vermischung, Umsortierung des Skelettanteils und Kryoturbation) sowie • kryopedologische Prozesse (periglaziäre Vorprägung oder sogar Prägung der pedogenen Horizontabfolge) entstanden. Die genannten Teilprozesse können mit unterschiedlichem Anteil und zu verschiedenen Zeiten an der Bildung und Differenzierung der Bodendecke beteiligt sein. In Abhängigkeit vom Paläorelief (Hangneigung, Hangform, Hangexposition) und vom Verbreitungsmuster der anstehenden Gesteine sowie vom Anteil allochthonen Materials und von den lokalklimatischen Bedingungen ist die stoffliche Zusammensetzung, Lagerungsart und Struktur sowie die Ausprägung der Bodenhorizonte in der Vertikalabfolge der einzelnen Segmente bzw. Lagen – ergänzt definiert – und in der horizontalen Ausprägung differenziert. Die Vertikalabfolge der periglaziär bedingten Differenzierung der Bodendecke wird gegliedert in das bisher nur lokal im Bergland sicher nachgewiesene Obersegment bzw. in die Oberlage – ergänzt definiert, außerdem in das fast flächendeckend an der Oberfläche verbreitete Hauptsegment, bzw. Hauptlage – ergänzt definiert, das von einem häufig unterteilten Mittelsegment (oberer Teil und unterer Teil) bzw. Mittellage – ergänzt definiert – unterlagert sein kann. Über dem periglaziär kaum oder nicht beeinflussten Untergrund lagert fast überall das Basissegment bzw. die Basislage – ergänzt definiert, das u. a. nach Zusammensetzung, Strukturmerkmalen sowie ggf. nach der Altersstellung differenziert werden kann. Durch die konsequente Verknüpfung aller im periglaziären Milieu wirksamen Prozesssysteme mit Hilfe der Ausweisung periglaziärer Segmente bzw. der Lagen – ergänzt definiert – ist eine detaillierte sowie integrierende und landschaftsübergreifende Kennzeichnung der Substratdifferenzierung der Böden möglich.
The moderate halophile Halobacillus halophilus is the paradigm for chloride dependent growth in prokaryotes. Recent experiments shed light on the molecular basis of the chloride dependence that is reviewed here. In the presence of moderate salinities Halobacillus halophilus mainly accumulates glutamine and glutamate to adjust turgor. The transcription of glnA2 (encoding a glutamine synthetase) as well as the glutamine synthetase activity were identified as chloride dependent steps. Halobacillus halophilus switches its osmolyte strategy and produces proline as the main compatible solute at high salinities. Furthermore, Halobacillus halophilus also shifts its osmolyte strategy at the transition from the exponential to the stationary phase where proline is exchanged by ectoine. Glutamate was found as a second messenger" essential for proline production. This observation leads to a new model of sensing salinity by sensing the physico-chemical properties of different anions.
In einem ausgedehnten Laubwaldgebiet im Hochspessart (Nordwestbayern, Bezirk Unterfranken) wurde 2006 untersucht, ob sich alte Rot-Buchenbestände, die seit mehr als 15 Jahren nach dem „Rothenbucher Totholz- und Biotopbaumkonzept“ bewirtschaftet werden, hinsichtlich Struktur-, und Artenvielfalt, von vergleichbaren Beständen ohne ein derartiges Konzpt unterscheiden. Qualitätsziele des Konzeptes sind: Schutz von Horstbäumen, Belassen von 10 ökologisch besonders wertvollen Bäumen pro Hektar, Erhalt und Akkumulation von durchschnittlich 10 m3 Totholz (ohne Stockholz und Kronentotholz) ab 20 Zentimeter pro Hektar auf der gesamten Fläche. Die Umsetzung erfolgt nach dem Grundsatz, dass bei der Auswahl jedes zu entnehmenden Altbaums stets zwischen dem zu erwartenden Holzertrag, der waldbaulichen Notwendigkeit und dem ökologischen Wert abzuwägen ist. Der Vergleich erfolgte in Rothenbuch, und in einem unmittelbar angrenzenden Gebiet ohne entsprechendes Konzept bei Altenbuch, in jeweils 30 ein Hektar großen Gitterfeldern sowie in je 25 Probekreisen (0,1 Hektar). Vögel wurden zur Brutzeit im Rahmen einer quantitativen Gitterfeldkartierung erhoben. Xylobionte Käfer wurden mit Hilfe von Kreuzfensterfallen und zeitstandardisierten Handfängen auf je 25 Probekreisen gefangen. Die Mollusken und Holz bewohnenden Pilze wurden auf je 15 Probekreisen durch standardisierte Aufsammlungen erfasst. In Wirtschaftswäldern seltene Strukturen, die zudem meist geklumpt auftreten (stehendes Totholz, Mulmhöhlen- und sonstige Biotopbäume), wurden auf den 60 Hektarrastern, häufigere und regelmäßiger verteilte Strukturen wie Stockholz oder liegendes Totholz wurden in den Probekreisen aufgenommen. Folgende Hypothesen wurden getestet: 1. Das Rothenbucher Totholz- und Biotopbaumkonzept hat bisher keine Auswirkungen auf Quantität und Qualität von liegendem und stehendem Totholz und Biotopbäumen. 2. Das Rothenbucher Totholz- und Biotopbaumkonzept hat bisher keine Auswirkungen auf Abundanzen und Artenreichtum von Indikatorgruppen. 3. Das Rothenbucher Totholz- und Biotopbaumkonzept hat bisher keine Auswirkungen auf Abundanzen und Artenreichtum an Habitat- und Strukturtradition gebundener und gefährdeter Arten. Es konnte kein Unterschied bei der Anzahl von Biotopbäumen in beiden Gebieten festgestellt werden. Signifikante Unterschiede zugunsten von Rothenbuch ergaben sich bei den Mengen an liegendem und stehendem Totholz und dem Angebot an Totholz stärkerer Dimensionen. Es wurden in Rothenbuch signifikant mehr Vogelarten und Individuen als in Altenbuch registriert. Besonders deutlich im Vergleich der Avizönosen war der Unterschied bei Höhlenbrütern, während die Werte für Vogelarten mit Bindung an Holzstrukturen nur einen Trend ergaben. Die Artenindikatoranalyse ergab folgende Arten als signifikant häufiger und stetiger im totholzreicheren Rothenbuch: Mittelspecht, Kohlmeise, Rotkehlchen, Grauspecht, Halsband- und Trauerschnäpper, Sumpfmeise und Mönchsgrasmücke. Nur der Buchfink (der im bayerischen Wirtschaftwald häufigste Vogel) erwies sich als Charakterart für Altenbuch. Die Artenzahl und Abundanzen der Mollusken lag in Rothenbuch signifikant über den Werten von Altenbuch. Auch die Anzahl gefährdeter Weichtierarten und die entsprechenden Individuenzahlen waren in Rothenbuch höher. Bei xylobionten Käferarten wurden in Rothenbuch signifikant höhere Artenzahlen aller Arten und der gefährdeten Arten festgestellt. Auch die Registrierungen und Artenzahlen von Holz bewohnenden Pilzen pro Probekreis lagen in Rothenbuch signifikant höher. Damit konnte gezeigt werden, dass bezüglich der Totholzmengen bereits nach etwa 15 Jahren deutliche Erfolge erzielt werden können. Das Fehlen von Unterschieden bei Biotopbäumen und wichtiger Indikatorarten der übergeordneten Großlandschaft Spessart in den untersuchten Beständen zeigt aber auch, dass ein Zeitraum von 15 Jahren für die Entstehung hochwertiger Biotopbäume nicht ausreicht. Die Dichte der Totholzstrukturen ist noch unzureichend, um den im Spessart reliktär vorhandenen, an Urwaldstrukturen gebundenen xylobionten Arten eine Wiederbesiedlung auf größerer Fläche zu ermöglichen. Inzwischen geht das Schutzkonzept der Bayrischen Staatsforsten (NEFT 2006) konsequent einen Schritt weiter, nämlich das Erreichen einer Gesamttotholzmenge von mindestens 40 m³ Totholz pro Hektar für über 140jährige Buchenbestände und Bestände älter als 180 gänzlich aus der Nutzung zu nehmen.
The habitat requirements of most Aradidae and the decisive factors that influence their occurrence are still poorly understood. To reduce this lack of knowledge a standardised survey of Aradidae in two large beech forest areas of Bavaria (northern Steigerwald and High Spessart) was conducted. The following hypotheses were tested: 1) With increasing habitat tradition (temporal continuity), population densities of Aradidae increase, 2) Increasing dead wood supply supports higher abundance of Aradidae, 3) There are key structures for particular species with respect to type of dead wood, diameter and exposure to sunlight, and 4) The occurrence of particular fungi species determines the occurrence of Aradidae. In our study, Aradidae were sampled in point sample plots by flight-interception traps and time-standardised hand collection. To analyse specific habitat requirements additional sampling was performed to increase the sample size. Four species of Aradidae were observed in the two forest areas: Aneurus avenius, Aradus betulae, A. conspicuus and A. depressus. The results demonstrate that all species have different and specific habitat requirements. Especially for A. betulae habitat tradition of standing dead wood of large dimensions infested by Fomes fomentarius seems to be crucial. Hence, A. betulae was only observed in the Spessart and only at the sites with habitat tradition.