POST-FIRE VEGETATION, SOIL, AND STREAM PROCESSES IN URBAN MEDITERRANEAN SYSTEMS

2019 ◽  
Author(s):  
Alicia M. Kinoshita ◽  
2017 ◽  
Vol 65 (1) ◽  
pp. 60 ◽  
Author(s):  
Mandy Lock ◽  
Barbara A. Wilson

In Mediterranean systems, such as south-east Australia, predictions of climate change including lower rainfall and extended drought, threaten vulnerable mammal species. We investigated the relationship between rainfall and population dynamics for a native rodent at risk of extinction, the New Holland mouse (Pseudomys novaehollandiae). In the eastern Otways, the species was significantly influenced by rainfall, exhibiting a population irruption (15–20 individuals ha–1) following six years of above-average rainfall and a precipitous decline to site extinction during subsequent drought. The decline was predominantly related to loss of adults before and during breeding seasons, together with an apparent decrease in juvenile survival. Population abundance was positively correlated with a rainfall lag of 0–9 months. We propose that the response of this omnivore to high rainfall was mediated through increased productivity and that rainfall decline resulted in resource depletion and population decline. Under a drying climate the direct impacts of rainfall decline will continue. However management of other threats may increase the species’ resilience. Burning to provide optimal successional vegetation, protection of refugia, and predator control are priorities. However, burning should be avoided during drought, as the likelihood of local extinctions is substantial.


2000 ◽  
Vol 15 (2) ◽  
pp. 137-150 ◽  
Author(s):  
CRISTINA GORRAIZ ◽  
Ma JOSE BERIAIN ◽  
JULIA CHASCO ◽  
MAITE IRAIZOZ

2008 ◽  
Vol 72 (10) ◽  
pp. 1803-1810 ◽  
Author(s):  
M. Teresa Pardo ◽  
M.A. Esteve ◽  
A. Giménez ◽  
J. Martínez-Fernández ◽  
M.F. Carreño ◽  
...  

2017 ◽  
Vol 23 (6) ◽  
pp. 2473-2481 ◽  
Author(s):  
Camilla Wellstein ◽  
Peter Poschlod ◽  
Andreas Gohlke ◽  
Stefano Chelli ◽  
Giandiego Campetella ◽  
...  

2002 ◽  
Vol 73 (2-3) ◽  
pp. 275-283 ◽  
Author(s):  
M Avondo ◽  
S Bordonaro ◽  
D Marletta ◽  
A.M Guastella ◽  
G D’Urso

2008 ◽  
Vol 70 (3) ◽  
pp. 358-367 ◽  
Author(s):  
Amos Frumkin ◽  
Miryam Bar-Matthews ◽  
Anton Vaks

AbstractThis paper explores the environmental conditions that faced the people of ancient Jawa during the Holocene, as well as previous prehistoric periods of the mid-late Pleistocene. Calcite speleothems in a lava tube are dated using the U-Th method, to marine oxygen isotope stage 7 from ∼ 250 to 240 ka and from ∼ 230 to ∼ 220 ka; and the stage 5/4 transition between ∼ 80 and 70 ka. The available evidence indicates general aridity of the Black Desert during most of the mid-late Quaternary, punctuated by short wetter periods, when the Mediterranean cyclonic systems intensified and penetrated the north Arabian Desert. These Mediterranean systems had a longer and more intense effect on the desert fringe closer to the Mediterranean and only rarely penetrated the Black Desert of Jawa. The results do not exclude some increase of rainfall which did not change water availability dramatically during the warm Holocene. The ancient Jawa city appears to have depended on technological ability to build elaborate runoff-collection systems, which became the prime condition for success.


Author(s):  
Sarah Davis-Secord

This conclusion summarizes the book's findings about Sicily's conceptual place in the Mediterranean world—a position that had been crafted by the Norman rulers. Later medieval maps, together with the Hereford Mappa Mundi, show that Sicily was closely integrated into larger currents in the political and religious world of Latin Christendom. The island's political and diplomatic role in the dār al-Islām was fundamentally different to what it had been under the Byzantine empire. Sicily's place within larger Mediterranean systems was determined not by its geographical location but by larger forces of political change, shifts in the balance of power, and economic need as well as the actions of regular people—merchants, pilgrims, envoys, and others—who traveled to and from Sicily and thus involved the island in patterns of communication, contact, conflict, and exchange.


2021 ◽  
Author(s):  
István Bozsó ◽  
Ylona van Dinther ◽  
Liviu Matenco ◽  
Attila Balázs ◽  
István Kovács

<p>The Carpathians subduction system evolved similarly to many Mediterranean systems where extensional back-arc basins and separate large sag basins develop in the overriding plate. The evolution of such basins can be explained in the context of roll-back of narrow oceanic slabs. Their evolution is linked to extensional and sag back-arc basins, retreating orogenic systems and slab detachment. A recent example of slab detachment can be studied by the Vrancea slab beneath the SE Carpathians.<br>Significant effort has been dedicated to modelling such Mediterranean-style subduction systems, and in most cases the model was set up with a narrow oceanic domain, which has an increased difficulty to create rollback due to reduced buoyancy of the slab.<br>Our approach is to use a two-dimensional thermo-mechanical numerical model that introduces an inherited oceanic domain, which adds to the younger, narrow ocean developed in the later stages.<br>Our model can produce sustained subduction of the oceanic slab associated with roll-back and slab detachment. In most of our models a retro-arc sag basin develops, which can be interpreted as the Transylvanian Basin. This sag basin is one of the most consistent features of our model. At larger distances from the subduction zone, the extensional back-arc of the Pannonian basin can be modelled by introducing an lithospheric weakness zone, which represents a suture zone inherited from a previous orogenic evolution. Such a suture zone is compatible with the overall orogenic evolution of the Alps-Carpathians-Dinarides system. We furthermore discuss the limitations of our 2D modeling in the overall 3D settings of the Carpathians system and possibilities of future integration.</p>


2019 ◽  
Vol 224 ◽  
pp. 40-49 ◽  
Author(s):  
Véronique Alary ◽  
Charles-Henri Moulin ◽  
Jacques Lasseur ◽  
Adel Aboul-Naga ◽  
Mohamed Taher Sraïri

Sign in / Sign up

Export Citation Format

Share Document