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首页> 外文期刊>Journal of foraminiferal research >THE ECOLOGICAL BALANCE OF NATURE AND THE EVOLUTION OF BAFFIN BAY, TEXAS
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THE ECOLOGICAL BALANCE OF NATURE AND THE EVOLUTION OF BAFFIN BAY, TEXAS

机译:德克萨斯州葡萄干湾的自然生态平衡与百杉湾演变

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The mixed siliciclastic/carbonate sediments of Baffin Bay, Texas, provide a record of the evolution of the Bay for the last 10 ka. Flooding surfaces at 8 ka and 5.5. ka provided an a priori separation of sediments in a core into three groups. Discriminant analysis and interpretation of species composition of the foraminifera from these groups indicated a progression from deltaic to open-bay to hypersaline environments. This traditional paleoecological analysis, however, does not utilize the information available in the relative abundance distribution (RAD) within each community. An approach capable of assessing within community change is provided by S (species richness), H (Shannon information function) and E (evenness) analysis. Using this approach not only can communities be designated without a priori assumptions and environments identified easily, but also the RAD within each community can be evaluated, providing a record of community growth, decline or stasis with time. Stasis, or the ecological balance of nature, is mathematically defined as an equilibrium between S and E such that diversity (H) remains constant with time. This stasis requires that, as the number of individuals (N) gets larger with time, the value of H remains constant. Thus, at stasis a regression between H versus hiN will have a 0 value for the regression coefficient ((beta(1H)), here termed the Relative Abundance Distribution Index, RADI. A positive value of RADI indicates community growth, a negative value indicates community decline. In the Baffin Bay core 6, communities were identified from 46 samples using SHE analysis. At similar to 9 ka the RADI was positive, indicating the growth of a normal marine community with a high S. A second community, still largely normal marine but with a slightly negative RADI, formed at similar to 8 ka. Beginning at similar to 6.4 ka, the 3rd and 4th marginal marine communities with highly negative RADIs formed, indicating a sharp decline for similar to 1
机译:德克萨斯州葡萄干湾的混合硅酸盐/碳酸盐沉积物,为最后10 kA提供了湾的演变的记录。溢出表面为8 KA和5.5。 KA提供了核心沉积物的优先分离成三组。从这些组中判别分析和解释Foraminifera的组成表明了德国对开放式海湾的普通环境的进展。然而,这种传统的古生态学分析不利用每个社区内相对丰富分布(RAD)中的信息。能够在社区变革中进行评估的方法是由S(物种丰富度),H(Shannon信息功能)和E(均匀性)分析提供。使用这种方法不仅可以在没有先验假设和容易识别的情况下被指定的社区,而且可以评估每个社区内的RAD,提供社区生长,随着时间的推移记录。瘀滞或自然的生态平衡,在数学上被定义为S和E之间的平衡,使得多样性(H)随时间保持不变。此静止要求,随着时间的数量(n)随时间变大,H保持不变。因此,在STAS中,H与HIN之间的回归将具有回归系数的0值((β(1H)),这里称为相对丰度分布指数,RADI。RADI的正值表示群落生长,负值表明社区衰退。在葡萄干湾核心6中,使用她分析从46个样品中鉴定了社区。与9ka类似,半RAdi是阳性的,表明普通海洋社区的生长仍然很大程度上是很大的海洋但具有略微阴性的半径,类似于8 ka。开始类似于6.4 ka,第3和第4个边缘海洋社区,形成高负radis,表明类似于1的急剧下降

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