scholarly journals Precipitation Patterns in Cape Verde Islands: Santiago Island Case Study

2014 ◽  
Vol 04 (05) ◽  
pp. 854-865 ◽  
Author(s):  
Gerson Ernesto Varela-Lopes ◽  
Luiz Carlos Baldicero Molion
Antiquity ◽  
2017 ◽  
Vol 91 (358) ◽  
Author(s):  
Christopher Evans ◽  
Marie Louise Stig Sørensen ◽  
Michael J. Allen ◽  
Jo Appleby ◽  
Tania Manuel Casimiro ◽  
...  

After the Portuguese discovered the Cape Verde Islands in AD 1456 they divided its main island, Santiago, into two governing captaincies. The founding settlement in the south-west, Cidade Velha, soon became the Islands’ capital and a thriving trade centre; in contrast, that in the east, Alcatrazes, only lasted as an official seat from 1484–1516 and is held to have ‘failed’ (see Richter 2015).


CATENA ◽  
2014 ◽  
Vol 121 ◽  
pp. 365-374 ◽  
Author(s):  
Juan Francisco Sanchez-Moreno ◽  
Chris M. Mannaerts ◽  
Victor Jetten

2012 ◽  
Vol 150 (1) ◽  
pp. 183-189 ◽  
Author(s):  
B. GUDVEIG BAARLI ◽  
ANA G. SANTOS ◽  
EDUARDO J. MAYORAL ◽  
JORGE LEDESMA-VÁZQUEZ ◽  
MARKES E. JOHNSON ◽  
...  

AbstractTwo distinct Pleistocene assemblages from SE Santiago Island are comparable to modern analogues elsewhere in the Cape Verde Islands. A low-diversity Siderastrea radians assemblage lived atop basalt knobs surrounded by sand on a slope below a cliff. A Millepora alcicornis–Megabalanus azoricus assemblage occupied the cliff. The latter was a typical rocky-shore assemblage from a high-energy setting below the tidal zone. Bioerosion structures in basalt produced by Circolites kotoncensis and Gastrochaenolites isp. also occur there. Despite extensive studies on local limestone deposits in 1832 and 1836, lack of exposure prevented Darwin from seeing these fossils.


2015 ◽  
Vol 1 (9) ◽  
pp. e1500456 ◽  
Author(s):  
Ricardo S. Ramalho ◽  
Gisela Winckler ◽  
José Madeira ◽  
George R. Helffrich ◽  
Ana Hipólito ◽  
...  

Large-scale gravitational flank collapses of steep volcanic islands are hypothetically capable of triggering megatsunamis with highly catastrophic effects. Yet, evidence for the generation and impact of collapse-triggered megatsunamis and their high run-ups remains scarce or is highly controversial. Therefore, doubts remain on whether island flank failures truly generate enough volume flux to trigger giant tsunamis, leading to diverging opinions concerning the real hazard potential of such collapses. We show that one of the most prominent oceanic volcanoes on Earth—Fogo, in the Cape Verde Islands—catastrophically collapsed and triggered a megatsunami with devastating effects ~73,000 years ago. Our deductions are based on the recent discovery and cosmogenic3He dating of tsunamigenic deposits found on nearby Santiago Island, which attest to the impact of this giant tsunami and document wave run-up heights exceeding 270 m. The evidence reported here implies that Fogo’s flank failure involved at least one fast and voluminous event that led to a giant tsunami, in contrast to what has been suggested before. Our observations therefore further demonstrate that flank collapses may indeed catastrophically happen and are capable of triggering tsunamis of enormous height and energy, adding to their hazard potential.


Zootaxa ◽  
2018 ◽  
Vol 4438 (2) ◽  
pp. 381 ◽  
Author(s):  
ULRICH K. SCHLIEWEN ◽  
PETER WIRTZ ◽  
MARCELO KOVAČIĆ

Didogobius janetarum sp. nov. is described from five specimens collected from small caves and rock crevices between 12 and 20 m depth off two locations of Santiago Island, Cape Verde Islands. The species differs from all currently described congeners by the combination of the following characters: (1) 27 vertebrae, (2) second dorsal fin I + 10, (3) posterior quarter of predorsal region in front of first dorsal fin origin scaled, with several rows of cycloid scales, (4) body squamation cycloid anteriorly and ctenoid posteriorly, (5) scales in the lateral series 30–32, (6) anterior oculoscapular canal present, (7) preopercular head canal absent, (8) suborbital row 7 each a single papilla, (9) suborbital rows 2 and 4 close to orbit, and by (10) branchiostegal membranes uniformely black below preopercle, forming a V-shaped mark. Definitions for all used meristic counts are presented to serve as a reference for gobioid meristic studies. The genus is rediagnosed to accommodate recently described Didogobius species. 


Planta Medica ◽  
2009 ◽  
Vol 75 (09) ◽  
Author(s):  
C Grosso ◽  
G Teixeira ◽  
I Gomes ◽  
ES Martins ◽  
JG Barroso ◽  
...  

Oryx ◽  
2011 ◽  
Vol 45 (2) ◽  
pp. 217-224 ◽  
Author(s):  
Sabine M. Hille ◽  
Nigel J. Collar

AbstractScavenging raptors have been postulated to be declining at a rate far higher than predatory raptors. To test this hypothesis we reviewed the historical and present status of the seven raptor species—three scavengers (two kites and a vulture), one partial scavenger (a buzzard) and three species (osprey and two falcons) that take live prey—that breed on the Cape Verde islands. Scavenging raptors have experienced steeper declines and more local extinctions than non-scavengers in Cape Verde, with the partial scavenger midway between the two groups. Causes of scavenger decline include incidental poisoning, direct persecution and declines in the availability of carcasses and other detritus. These findings, which highlight the conservation importance of the island of Santo Antão, indicate the priority that needs to be accorded to scavengers, particularly in Europe where many insular populations are reaching unsustainable levels.


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