首页> 外文期刊>Earth and Planetary Science Letters: A Letter Journal Devoted to the Development in Time of the Earth and Planetary System >A novel biomarker-based proxy for the spring phytoplankton bloom in Arctic and sub-arctic settings - HBI T-25
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A novel biomarker-based proxy for the spring phytoplankton bloom in Arctic and sub-arctic settings - HBI T-25

机译:基于生物标记的基于生物标志物的春季浮游植物绽放的基于生物标记的代理,北极和次北极地区 - HBI T-25

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The spring phytoplankton bloom is a characteristic feature of mid-high latitudes in modern times, but can be challenging to identify in palaeo records. In the current study, we investigated the absolute and relative distributions of two diatom-derived tri-unsaturated highly branched isoprenoid (HBI) lipids, at least one of which has previously been suggested to be a possible proxy for the productive region of the marginal ice zone (MIZ) in the Polar Regions. Based on a comparison of their distributions in surface sediments from the Barents Sea and neighbouring regions with a range of oceanographic parameters, we identify, via principal component analysis, a strong association between the relative proportion of the two HBIs and satellite-derived spring chlorophyll a (chl a) concentration. Further, based on agglomerative hierarchical clustering, we identify two clusters of HBI biomarker ratios and spring chl a together with a potential threshold biomarker ratio (termed HBI TR25) for the spring phytoplankton bloom. A modified version of HBI TR25 (i.e. HBI T-25) provides a potentially more straightforward binary measure of the spring phytoplankton bloom. Analysis of HBI TR25 and HBI T-25 values in a series of short (spanning recent centuries) and long (Holocene) sediment cores from the region provides an initial evaluation of the applicability of this novel proxy in the palaeo record. Outcomes are mainly consistent with the findings from the surface sediments and with other proxy-based reconstructions, including estimates of past sea ice cover, which is well-known to influence primary production in the region. Indeed, we suggest that the new HBI T-25 phytoplankton bloom proxy may also represent an important new tool for characterising the MIZ in palaeo records, especially when used alongside well-established sea ice proxies, such as IP25 and PIP25. Despite the largely empirical nature of the study, we also provide a possible explanation for the observed biomarker ratio-
机译:春季Phytoplankton Bloom是近代中高纬度的特征,但在帕拉诺记录中可能具有挑战性。在目前的研究中,我们研究了两种硅藻衍生的三种不饱和高度分支等异戊二烯(HBI)脂质的绝对和相对分布,其中至少有一个已经建议是用于边缘冰的生产区的可能代理区域(Miz)在极地区域。基于对来自诸着海洋参数的邻近地区的地表沉积物中的地表沉积物的分布比较,我们通过主成分分析来识别两种HBI和卫星源泉叶绿素A之间的相对比例的强烈关联(CHL A)浓度。此外,基于附聚层聚类,我们将两种HBI生物标志物比和弹簧CHLA簇与弹簧浮游植物绽放的潜在阈值生物标志物比(称为HBI TR25)鉴定。 HBI TR25(即HBI T-25)的修改版本提供了春季浮游植物盛开的潜在更直接的二进制测量。来自该地区的一系列短(跨越几个世纪)和长(全新世)沉积物核心的HBI TR25和HBI T-25值的分析提供了对Palaeo记录中这部小型代理的适用性的初步评估。结果主要与表面沉积物的发现以及其他基于代理的重建的结果一致,包括过去海冰覆盖的估计,这是众所周知的影响该地区的主要生产。事实上,我们建议新的HBI T-25 Phytoplankton Bloom Proxy还可以代表一个重要的新工具,用于在古古纪录中表征MIZ,特别是当与成熟的海冰代理一起使用,例如IP25和PIP25。尽管该研究的经验性很大,但我们还提供了对观察到的生物标志物比率的可能解释 -

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