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Production, exportation and preservation of silicoflagellates in Alfonso Basin, Gulf of California

机译:加利福尼亚湾阿方索盆地硅鞭毛藻的生产,出口和保存

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Limited areas of sea floor have the physiochemical conditions that allow for the formation and preservation of high resolution (yearly or close to yearly) laminated sediments that can function as a historic proxy for past oceanographic and climate conditions. We evaluated and established the fidelity of the sedimentary record in recording these signals by analyzing silicoflagellates production, changes in species composition, skeletal settling and their subsequent burial in bottom sediments at Alfonso Basin. The data series from December 2005 to February 2008 showed similar tendencies in both the vertical flux and overlying euphotic zone (Z(eu)) production of silicoflagellates. Both series were numerically dominated by Octactispulchra with maxima values being recorded for the mixed water column period. Observed differences occurred during the studied years in both magnitude and in flux composition. The presence of a mixed assemblage with (warm-temperate-cold) species such as Dictyocha fibula var. robusta, Dictyocha epiodon and Distephanus speculum could be explained by a synchronization of trends between a predominantly positive Pacific Decadal Oscillation and a positive North Pacific Gyre Oscillation climate phases that were the background conditions underlying the early 2006 through 2007 El Nino event. A Morisita's similarity index value of 97.5% between winter trap and Z(eu) samples combined with an annualized settling factor of 0.45, suggests that Alfonso Basin is a favorable settling environment for silicoflagellates. However, core-top sediments showed an attenuation of record fidelity (burial factor = 0.25) resulting in a modified record for the production and settling of skeletons. O. pulchra that were not preserved in sediments as the dominant species and with this removal, the signal was also lost of the highest silicoflagellate production season (Mixing-cyclonic eddy periods) from the sedimentary record of the Alfonso Basin. (C) 2016 Elsevier B.V. All rights reserved.
机译:海床的有限区域具有能够形成和保存高分辨率(每年或接近每年)的层状沉积物的理化条件,这些沉积物可以作为过去海洋学和气候条件的历史代表。我们通过分析硅鞭毛虫的产生,物种组成的变化,骨骼的沉降及其随后在阿方索盆地底部沉积物中的埋葬,评估并建立了记录这些信号的沉积记录的保真度。从2005年12月到2008年2月的数据系列在硅鞭毛虫的垂直通量和上覆富营养区(Z(eu))生产中都显示出相似的趋势。这两个系列在数值上均以Octactispulchra为主,并记录了混合水柱期间的最大值。在研究年份中,观测到的幅度和通量组成均存在差异。与(温-温-冷)物种,如腓肠ct腓骨变种的混合组合的存在。罗布斯塔(Robusta),Di足纲(Dictyocha epiodon)和狄氏(Distephanus)窥镜可以解释为太平洋年代际涛动和北太平洋回旋涛动积极的气候阶段之间呈同步趋势,这是2006年初至2007年厄尔尼诺事件的背景条件。冬季圈闭和Z(eu)样品之间的Morisita相似度值为97.5%,年沉降系数为0.45,这表明阿方索盆地是硅鞭藻类的有利沉降环境。然而,核心顶部的沉积物显示出记录保真度的降低(埋葬系数= 0.25),从而导致了骨架的生产和沉降记录的修改。没有被保留在沉积物中作为主要种的O. pulchra,通过这种去除,也从阿方索盆地的沉积记录中丢失了硅鞭毛虫最高生产季节(旋风涡旋期)的信号。 (C)2016 Elsevier B.V.保留所有权利。

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