首页> 外文期刊>Palaeogeography, Palaeoclimatology, Palaeoecology: An International Journal for the Geo-Sciences >The species richness of Miocene browsers, and implications for habitat type and primary productivity in the North American grassland biome
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The species richness of Miocene browsers, and implications for habitat type and primary productivity in the North American grassland biome

机译:中新世浏览器的物种丰富度及其对北美草原生物群落中生境类型和初级生产力的影响

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摘要

We have documented elsewhere, and briefly reviewed here, the anomalously high species richness of browsing ungulates (hoofed mammals) in the mid Miocene (~18–12 Ma) woodland savanna habitats of North America. In the mid Miocene these habitats supported substantially more brachydont (browsing) species than do any present-day savanna habitats. We present some preliminary data to show that such species-rich browser communities are not observed after the mid Miocene. The data also suggest that these mid Miocene browser communities and their subsequent disappearance may have been a global phenomenon. We then focus on possible explanations for these observations. We discuss the possibility that the high species numbers are a preservational artifact, and conclude that taphonomic factors are unlikely to be responsible for the level of species richness observed. We then consider various possible explanations for high species richness, including the unique aspects of climatic change (cooling, drying, increased seasonality), unique biotic interactions (the effects of competition, keystone herbivores, changes in predator pressure), and consider that none of these are fully consistent with the available data. The most likely explanation for the observed species-rich browser palaeocommunities is an elevated level of primary productivity, relative to the present day, within (at least some) mid Miocene grassland habitats. Such an increase in productivity could possibly have been the result of higher-than-present levels of atmospheric carbon dioxide in the mid Miocene, but this conflicts with current interpretations of geochemical evidence, and a satisfactory mechanism for the inferred increased primary productivity is an unresolved issue.
机译:我们已经在其他地方进行了文献记录,并在这里进行了简要回顾,它是北美中新世中期(〜18-12 Ma)林地热带稀树草原栖息地中有蹄类动物(蹄类哺乳动物)的异常高物种丰富度。在中新世中期,这些栖息地支持的brachydont(浏览)物种比当今任何热带稀树草原栖息地都要多。我们提供了一些初步数据,以表明在中新世中期以后没有观察到这种物种丰富的浏览器社区。数据还表明,这些中新世中期的浏览器社区及其随后的消失可能是全球现象。然后,我们将重点放在这些观察的可能解释上。我们讨论了高物种数量是一种保存人工产物的可能性,并得出结论,言语学因素不太可能与观察到的物种丰富度有关。然后,我们考虑各种有关物种丰富度的可能解释,包括气候变化的独特方面(冷却,干燥,季节性增加),独特的生物相互作用(竞争的影响,梯形草食动物,捕食者压力的变化),并认为没有这些与可用数据完全一致。相对于当今,在(至少某些)中新世中部草地栖息地内,观察到的物种丰富的浏览器古群落的最可能解释是初级生产力水平的提高。生产率的这种提高可能是中新世中期大气二氧化碳含量高于当前水平的结果,但这与当前对地球化学证据的解释相矛盾,并且无法确定令人满意的机制来推断初级生产率的提高问题。

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