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Evenness and diversity in U pper C ambrian – L ower O rdovician trilobite communities from the C entral A ndean B asin ( C ordillera O riental, A rgentina)
Author(s) -
Balseiro Diego,
Waisfeld Beatriz G.
Publication year - 2014
Publication title -
palaeontology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.69
H-Index - 63
eISSN - 1475-4983
pISSN - 0031-0239
DOI - 10.1111/pala.12075
Subject(s) - species evenness , species richness , ecology , biology
Community evenness has recently received much attention, either because it is related to ecosystem functioning or because it may affect estimation of diversity. Temporal and environmental trends in diversity and evenness of trilobite communities during the L ate C ambrian – E arly O rdovician of the C ordillera O riental (north‐western A rgentina) are here analysed. Richness and evenness increase through time in both deep subtidal (between fair‐weather and storm wave base) and offshore (below storm wave base) communities. Two significant patterns are superimposed on this general trend: (1) the magnitude of the increase in evenness is much more pronounced in deep than in shallower settings, and (2) richness and evenness trajectories are decoupled (while a significant rise in evenness is recorded in the middle T remadocian ( T r2), an increase in richness is delayed until the late T remadocian ( T r3)). In contrast to expectations, a single family ( O lenidae) is dominant in samples associated with this earlier rise in evenness relative to richness. Hence, this trend is explained neither by the number of families present in the communities nor by the familial identity of the most abundant taxon. Large‐scale comparisons of the timing and geographical components of these trends are restricted to the patterns recognized in L aurentian N orth A merican studies. Results from the C ordillera O riental mirror those of L aurentia regarding the rise in both metrics in deep marine settings. Nevertheless, the timing of this increase in richness and evenness is delayed in the C ordillera O riental, supporting the idea that palaeogeographical regions differed in the nature and timing of ecological changes. Finally, the rise in trilobite alpha‐diversity through the L ate C ambrian – E arly O rdovician of the C ordillera O riental supports the idea that trilobite alpha‐diversity did not decline worldwide, suggesting that the relative decline in trilobite alpha‐diversity is most probably caused by the dilution effect.