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Intermediate Disturbances (intermediate + disturbance)
Terms modified by Intermediate Disturbances Selected AbstractsTesting the intermediate disturbance hypothesis: when will there be two peaks of diversity?DIVERSITY AND DISTRIBUTIONS, Issue 1 2005Karin Johst ABSTRACT Succession after disturbances generates a mosaic of patches in different successional stages. The intermediate disturbance hypothesis predicts that intermediate disturbances lead to the highest diversity of these stages on a regional scale resulting in a hump-shaped diversity,disturbance curve. We tested this prediction using field data of forest succession and hypothetical succession scenarios in combination with analytical and simulation models. According to our study the main factors shaping the diversity,disturbance curve and the position of the diversity maximum were the transition times between the successional stages, the transition type, neighbourhood effects and the choice of diversity measure. Although many scenarios confirmed the intermediate disturbance hypothesis we found that deviations in the form of two diversity maximums were possible. Such bimodal diversity,disturbance curves occurred when early and late successional stages were separated by one or more long-lived (compared to the early stages) intermediate successional stages. Although the field data which met these conditions among all those tested were rare (one of six), the consequences of detecting two peaks are fundamental. The impact of disturbances on biodiversity can be complex and deviate from a hump-shaped curve. [source] Maintaining diversity through intermediate disturbances: evidence from rodents colonizing rehabilitating coastal dunesAFRICAN JOURNAL OF ECOLOGY, Issue 4 2000S. M. Ferreira Abstract Rodents inhabit the coastal dune forests of KwaZulu-Natal, South Africa. Here habitat rehabilitation following mining of dunes has resulted in coastal dune forest succession similar to that recorded in nonmined forests. We investigated the colonization of rehabilitating stands and evaluate the role of disturbance in maintaining rodent diversity. A trapping programme was established between July 1993 and February 1995 during which rodent colonization, local extinction and species richness were recorded for rehabilitating stands of different ages. Trends in these variables were closely associated with one of three possible outcomes for a disturbed patch over time, with no intervening disturbances following the initial disturbance. Colonization was initially high which led to an increase in species richness. Extinction was lower than colonization, but became higher when the habitat was 3 years old, which led to a decline in richness. We extrapolate this result assuming negligibly small disturbances after the initiation of rehabilitation and suggest that intermediate levels of disturbance maintain rodent species richness in coastal dune forests. Furthermore, our results illustrated species turnover, a prediction of the recorded outcome, with young stands dominated by Mastomys natalensis and older stands by Saccostomus campestris or Aethomys chrysophilus. Résumé Il y a des rongeurs dans les forêts des dunes côtières du KwaZulu-Natal, en Afrique du Sud. Là, la réhabilitation de l'habitat après l'exploitation minière des dunes a abouti à une succession de forêts côtières des dunes semblable à celle qui est observée dans les forêts non exploitées. Nous avons étudié la colonisation des endroits en voie de réhabilitation et évalué le rôle des perturbations dans le maintien de la diversité des rongeurs. On a mis au point un programme de piégeage entre juillet 1993 et février 1995, pendant lequel on a noté la colonisation par les rongeurs, l'extinction locale et la richesse en espèces pour les endroits à différents stades de réhabilitation. Les tendances pour ces variables étaient étroitement associées à l'un des trois résultats possibles que peut conna,^tre avec le temps un endroit qui a été perturbé, lorsque aucune autre perturbation ne suit la première. La colonisation a d'abord été forte, ce qui a causé un enrichissement des espèces. Les extinctions étaient moins fréquentes que les colonisations, mais elles ont augmenté lorsque le nouvel habitat a atteint l'âge de trois ans, ce qui a entra,^né une perte de richesse en espèces. Nous extrapolons ce résultant en supposant que ce sont de petites perturbations négligeables après le démarrage de la réhabilitation et nous suggérons que des taux moyens de perturbation maintiennent la richesse spécifique des rongeurs dans les forêts des dunes côtières. De plus, nos résultats illustrent une rotation des espèces, une prédiction des résultats rapportés, avec les endroits les plus jeunes dominés par Mastomys natalensis et les plus anciens par Saccostomus campestris et Aethomys chrysophilus. [source] Ice-storm disturbance and long-term forest dynamics in the Adirondack MountainsJOURNAL OF VEGETATION SCIENCE, Issue 2 2004Charles W. Lafon Ice storms cause periodic disturbance to temperate forests of eastern North America. They are the primary agents of disturbance in some eastern forests. In this paper, a forest gap model is employed to explore consequences of ice storms for the long-term dynamics of Tsuga canadensis-northem hardwoods forests. The gap model LINKAGES was modified to simulate periodic ice storm disturbance in the Adirondack Mountains of New York. To adapt the gap model for this purpose, field data on ice storm disturbance are used to develop a polytomous logistic regression model of tree damage. The logistic regression model was then incorporated into the modified forest gap model, LINK ADIR, to determine the type of damage sustained by each simulated tree. The logistic regression model predicts high probabilities of bent boles or severe bole damage (leaning, snapping, or uprooting) in small-diameter trees, and increasing probability of canopy damage as tree size increases. Canopy damage is most likely on gentle slopes; the probability of severe bole damage increases with increasing slope angle. In the LINKADIR simulations, tree damage type determines the probability of mortality; trees with severe bole damage are assigned the highest mortality rate. LINKADIR predicts Tsuga canadensis dominance in mesophytic old-growth forests not disturbed by ice storms. When ice storms are simulated, the model predicts Acer saccharum -dominated forests with higher species richness. These results suggest that ice storms may function as intermediate disturbances that enhance species richness in forested Adirondack landscapes. [source] The radiation of the Cape flora, southern AfricaBIOLOGICAL REVIEWS, Issue 4 2003H. P. LINDER ABSTRACT The flora of the south-western tip of southern Africa, the Cape flora, with some 9000 species in an area of 90 000 km2 is much more speciose than can be expected from its area or latitude, and is comparable to that expected from the most diverse equatorial areas. The endemism of almost 70%, on the other hand, is comparable to that found on islands. This high endemism is accounted for by the ecological and geographical isolation of the Cape Floristic Region, but explanations for the high species richness are not so easily found. The high species richness is accentuated when its taxonomic distribution is investigated: almost half of the total species richness of the area is accounted for by 33,Cape floral clades'. These are clades which may have initially diversified in the region, and of which at least half the species are still found in the Cape Floristic Region. Such a high contribution by a very small number of clades is typical of island floras, not of mainland floras. The start of the radiation of these clades has been dated by molecular clock techniques to between 18 million years ago (Mya)(Pelargonium) and 8 Mya (Phylica), but only six radiations have been dated to date. The fossil evidence for the dating of the radiation is shown to be largely speculative. The Cenozoic environmental history of southern Africa is reviewed in search of possible triggers for the radiations, climatic changes emerge as the most likely candidate. Due to a very poor fossil record, the climatic history has to be inferred from larger scale patterns, these suggest large-scale fluctuations between summer wet (Palaeocene, Early Miocene)and summer dry climates (Oligocene, Middle Miocene to present). The massive speciation in the Cape flora might be accounted for by the diverse limitations to gene flow (dissected landscapes, pollinator specialisation, long flowering times allowing much phenological specialisation), as well as a richly complex environment providing a diversity of selective forces (geographically variable climate, much altitude variation, different soil types, rocky terrain providing many micro-niches, and regular fires providing both intermediate disturbances, as well as different ways of surviving the fires). However, much of this is based on correlation, and there is a great need for (a)experimental testing of the proposed speciation mechanisms, (b)more molecular clock estimates of the age and pattern of the radiations, and (c)more fossil evidence bearing on the past climates. [source] |