Petrography and sedimentology of aeolian sands: a tool for diagnose the sedimentary deficit in La Graciosa island (Natural Park of Archipielago Chinijo, Canary Islands, Spain).

[EN] Petrography and sedimentology of aeolian sands: a tool for diagnose the sedimentary deficit in La Graciosa island (Natural Park of Archipielago Chinijo, Canary Islands, Spain).

Characterization of sands in the beach-dune systems of the Eastern Canary Islands.

Characterization of sands in the beach-dune systems of the Eastern Canary Islands.

Selección de sustrato de la Holothuria tubulosa en función del tamaño de las partículas

Holothuria tubulosa, cuando la concentración de materia orgánica es constante en el sedimento, muestra una clara preferencia por ambientes con arenas conformadas mayoritariamente por partículas gruesas. Esta tendencia a permanecer más tiempo en estos ambientes se corresponde igualmente con la composición granulométrica de sus excrementos, principalmente conformados por partículas propias de arenas gruesas o medias. Este patrón de selección positiva hacia un determinado grosor de sedimentos contrasta con la composición de las excreciones cuando estos animales se han alimentado en su medio natural. ABSTRACT: Holothuria tubulosa, when the rate of organic matter in the sediments is a constant, shows a clear preference to stay in sandy environments conformed by thick particles. This tendency to pass more time in these environments is also corresponded with the granulometric composition of its excrements, mainly constituted by particles of thick or medium sized sands. This positive selection pattern toward a specific size of the sediment grains contrast with the size composition of the excretions when this animals feed at their natural habitat.

Differences in diversity, structure, and variability between intertidal and subtidal meiofaunal assemblages

[EN] Meiofaunal assemblages from intertidal and shallow subtidal seabeds were studied at two sites (one dominated by volcanic sands and the other by organogenic sands) at Tenerife (Canary Islands, NE Atlantic Ocean) throughout an entire year (May 2000?April 2001). Specifically, we aimed (i) to test for differences in diversity, structure, and stability between intertidal and subtidal meiofaunal assemblages, and (ii) to determine if differences in the meiofaunal assemblage structure may be explained by environmental factors (granulometric composition, availability of organic matter, and carbonate content in sediments). A total of 103,763 meiofaunal individuals were collected, including 203 species from 19 taxonomic groups (Acari, Amphipoda, Cnidaria, Copepoda, Echinodermata, Gastrotricha, Isopoda, Insecta, Kinorrhyncha, Misidacea, Nematoda, Nemertini, Oligochaeta, Ostracoda, Polychaeta, Priapulida, Sipuncula, Tanaidacea, and Turbellaria). Nematodes were the most abundant taxonomic group. Species diversity was higher in the subtidal than in the intertidal zone at both sites, as a result of the larger dominance of a few species in the intertidal zone. The meiofaunal assemblage structure was different between tidal levels at both sites, the intertidal presenting greater temporal variability (multivariate dispersion) in the meiofaunal assemblage structure than the subtidal. Sediment grain size, here quantified by the different granulometric fractions, explained the variability in meiofaunal assemblage structure to a greater extent than the percentage of carbonates, a variable linked to sediment origin. This study revealed differences in diversity, assemblage structure, and variability between intertidal and subtidal meiofauna.

Late Pliocene and Quaternary Eurasian locust infestations in the Canary Archipelago

[EN] The Canary Archipelago has long been a sensitive location to record climate changes of the past. Interbedded with its basalt lavas are marine deposits from the principal Pleistocene interglacials, as well as aeolian sands with intercalated palaeosols. The palaeosols contain African dust and innumerable relict egg pods of a temperate-region locust (cf. Dociostaurus maroccanus Thunberg 1815). New ecological and stratigraphical information reveals the geological history of locust plagues (or infestations) and their palaeoclimatic significance.