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The whole assemblage is composed of 48 species of which six are spores.
The fluvio-estuarine facies assemblage is composed of both interfluve and valley-fill deposits, encompassing a variety of depositional environments such as fluvial channel, interfluve paleosol, bay head delta, estuary bay, restricted tidal flat, intertidal channel, and estuary mouth.
In the fine-grained, silty to clayey unit at the base of the profile the benthic foraminiferal assemblage is composed of Ammonia spp., Haynesina germanica, Haynesina depressula, Quinqueloculina spp., Affinetrina planciana and Aubignyna perlucida; few isolated specimens of Peneroplis pertusus were detected.
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Each assemblage was composed of a different set of species and all levels of diversity (combinations of species richness and number of functional groups) were represented by several different assemblages.
The assemblages were composed of ceramics of different production quality (but with a homogenous structure, previously analysed by optical microscopy, which improved the absence of the tempers of considerable grain size and pores whose presences could affect homogenous elemental distribution around the examined surface) and usage (pottery, figurines, and altars).
Each of Gilles Cenazandotti's sculptures and assemblages are composed of polyurethane material culled from the Mediterranean Sea.
The hierarchically integrated system model proposes that cultural assemblages are composed of two types of characters: those belonging to a core tradition that evolves through phylogenesis, and peripheral characters that are commonly exchanged among groups and can be gained or lost with relative ease.
Therefore, we propose that the genome assemblage of AbSV is composed of genes derived from at least four distinct sources: a new family of viruses (or invertebrate viruses), phages, endosymbionts, and bacteria.
The studied area, encompassing the Serra di Pigno and Col de Téghime areas (Cap Corse) is composed of an assemblage of prealpine basement sheets made up of serpentinized mantle rocks, Permian gabbros and gneisses, locally associated with Paleozoic metabasites and micaschists.
The first dyke is a pegmatitic leucogranite in which the assemblage chlorite >> grossular + prehnite locally forms a thick zone of blackwall-type alteration near its contact with serpentinite (Table 1; Gran-1a), whereas the pervasively rodingitized granite is composed of a coarse-grained assemblage of grossular + clinopyroxene (Table 1; Gran-1b) which contains abundant fluid inclusions.
It is a phase-dark body that is composed of an aggregation of membrane-bound vesicles containing cell wall components, serving as a point of assemblage and release of such components intermediate between the Golgi and the cell membrane.
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