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Polarization of competition increases with latitude.

机译:竞争的极化随着纬度的增加而增加。

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摘要

Many organisms overlap in their use of resources in space and time. Where and when resources are restricted, species must compete for them. Living space, often a critical resource controlling food and mate availability, is directly contested by organisms in most habitats. The ensuing animal interactions generally result in a winner gaining space and a loser, which may die. Contact matrices from studies of interference competition in encrusting marine Bryozoa (clonal and colonial animals), spanning at least 60 degrees latitude in both hemispheres, were analysed and subjected to a modern transitivity index. Only data for Bryozoa were used because (i) use of a single taxon with restricted ecology simplifies the scope for types of encounters, (and therefore) interpretation; and (ii) ecological bias is reduced because bryozoans are abundant at all latitudes. The analysis shows that assemblage competition is more hierarchical towards both poles. Thus, poorer competitors fail more frequently in interactions with increasing latitude. The cause of this trend is the simplification of overall outcomes between competitors, such as fewer ties, reversals in outcome or competitive loops (where low-ranking competitors beat those of higher ranking). The implication of such a trend is that the maintenance of biological diversity at high latitudes may principally be by physical rather than biological (competition) processes. Certainly, ocean surface energy increases with latitude through wind and wave action (and ice scour in polar regions).
机译:许多生物在时空上的资源使用重叠。在资源有限的地方和时间,物种必须争夺它们。生活空间通常是控制食物和配偶供应的关键资源,大多数生境中的生物直接争夺它们。随后发生的动物互动通常会导致获胜者获得空间,而失败者则可能死亡。对包埋在两个半球中纬度至少为60度的海洋Bryozoa(克隆和殖民地动物)中的干扰竞争研究的接触矩阵进行了分析,并采用了现代传递指数。仅使用Bryozoa的数据,因为(i)使用受限制的生态的单一分类单元简化了相遇类型的范围(并因此简化了解释); (ii)减少了生态偏见,因为苔藓虫在所有纬度上都很丰富。分析表明,组装竞争在两个方面都更加分等级。因此,较贫穷的竞争者在纬度增加的互动中更容易失败。造成这种趋势的原因是简化了竞争对手之间的总体结果,例如减少了平局,结果反转或竞争循环(排名较低的竞争对手击败了排名较高的竞争对手)。这种趋势的含义是,在高纬度地区维持生物多样性可能主要是通过物理而不是生物(竞争)过程。当然,海洋表面能通过风和波浪作用(和极地冰激凌)随纬度增加。

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