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What is most obvious from the general assemblage quantification is that all regions of the skeleton are represented within the cave assemblage, in spite of potential preservation and/or recovery bias.
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This in turn is a consequence of adopting management measures which allow a sustainable catch of the general ray assemblage, which is itself made up of a number of species with dirrerent resiliences to fishing pressure and mortality.
In general, assemblage B has been detected in only a small number of cattle in a few studies worldwide, including in Europe, Italy, Portugal, Uganda, New Zealand, and Canada [ 2, 30].
Post-deforestation, secondary forest assemblages are comprehensively described, both as broad general assemblages and island-specific variations by calculating species importance values from forest inventory data.
The general clay mineral assemblage in the 22/29-2 and 22/29-3 setsle sets consists of authigenic chlorite and authigenic illite.
Despite this gross simplification, some of the macroecological patterns produced by these models (for example, species-abundance distributions) are surprisingly close to those observed in nature [ 11], suggesting that they arise from the general statistics of assemblages rather than being of biological origin.
We have a detailed nqu iry into an assemblage the general contours of which were already known on the one hand, and on the other the remote and speculative possibility of some sort of legislationalbeit legislation in a field where there are serious constitutional limitations.
Paradoxically, the general trends in foraminiferal assemblages with time were consistent with a decreasing impact of pollution and continental influence (e.g., increasing species richness, diversity, density, and decreasing percentages of Ammonia tepida).
The significant relationship with HUM further stresses the general association between polychaete assemblages and environmental conditions at broad spatial scales.
Trends indicate a fall in the general health of the fish assemblage.
This study tested the general proposition that MPAs affected assemblages of algae and invertebrates between 0.0 and 0.5 m above the mean low water level of rocky coasts on two islands in the Tuscan Archipelago (northwest Mediterranean).
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