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Additional empirical evidence on the intrinsic trend to stationarity in the long run and the nested relationship between abiotic, biotic and anthropogenic factors starting from the organic biophysics of ecosystems (OBEC)

机译:额外的经验证据在长期持续时间内具有固有趋势的额外趋势和从生态系统的有机生物物理学开始的非生物,生物和人为因子之间的嵌套关系(OBEC)

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摘要

Conventional ecology lacks a non-contingent theory on the relationship between abiotic, biotic and anthropogenic factors under natural or quasi-natural conditions. As a result, since ecology is the science that studies the interaction between ecological factors in nested complex systems, we should recognize that ecology needs significant enhancements to understand the functioning of ecosystems. This article combines the ecological state equation (ESE, one of the earliest models derived from the Organic Biophysics of Ecosystem -OBEC), with abundant field data of abiotic factors, biotic factors and human factors from inland water rotifers and crustaceans (1022 samples taken over 21 years), litter invertebrates in laurel forest and pine forest (308 samples), and marine interstitial meiofauna of sandy beaches (90 samples). This has been done in order to obtain additional empirical evidence on the intrinsic trend to stationarity in the long run, even in perturbed ecosystems (manmade eutrophic water reservoirs, forest vegetation affected by traffic, and coastal ecosystems close to disposal points of sewage that are fully or partially treated, respectively to the above-mentioned taxocenes), and the relationship between the above-mentioned ecological factors. Our results indicate that there is a complex natural arrangement that intertwines the trend to stationarity and the resilience capability of ecosystems with a clear pattern of hierarchical setup between ecological factors. This is reflected by the role of ESE as a trophodynamic interface in hierarchical statistical models (cluster analysis) because they involve, in the following order of increasing rank: lower level abiotic factors (a.f.), biotic factors (b.f.), the holistic combination of state variables included in the ESE and, finally, higher level human factors (h.f.). In such a way, there is a clear trend to a hierarchical assemblage in agreement with the evolutionary origin of ecological factors in the deep time,
机译:传统生态学缺乏非缺失的非目的地,自然或准自然条件下的非生物,生物和人为因子之间的关系。因此,由于生态学是研究嵌套复杂系统中生态因素之间相互作用的科学,我们应该认识到生态需要显着的增强,以了解生态系统的运作。本文结合了生态状态方程(ESE,来自生态系统--Obec的有机生物物理学的最早模型之一),内陆水转子和甲壳类动物的非生物因子,生物因子和人类因素的丰富现场数据(1022个样品21年),垃圾在月桂林和松林(308个样品)中的垃圾无脊椎动物(308个样品),以及沙滩的海运间质梅诺纳(90个样品)。这已经完成,以便在长期运行中获得有关固有趋势的额外经验证据,即使在扰动的生态系统中(Manade Euterophic水库,受交通影响的森林植被以及靠近完全的污水点的沿海生态系统)。或部分治疗,分别于上述撒母蛋白),以及上述生态因素之间的关系。我们的结果表明,具有复杂的自然安排,使趋势与生态系统之间的趋势和生态系统的抵御能力相互依赖于生态因子之间的分层设置。这反映了ESE作为分层统计模型(聚类分析)中的滋养动力学界面的作用,因为它们涉及等级的顺序:较低水平的非生物因子(AF),生物因子(BF),整体组合状态变量包括在ESE中,最后,较高的人类因素(HF)。以这样的方式,与深度时期生态因子的进化起源一致的分层组合有明显的趋势,

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