Guangzhou Marine Geological Survey, China Geological Survey/ Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou), Guangzhou, China.
Institute of Marine and Environmental Sciences, University of Szczecin, Szczecin, Poland.
PeerJ. 2022 May 16;10:e13115. doi: 10.7717/peerj.13115. eCollection 2022.
Located in northwestern South China Sea (SCS), the Beibu Gulf constitutes an environmentally sensitive region shaped by land-ocean-atmosphere interactions in Asia between the western Pacific and eastern Indian Oceans. This study aims to provide a comprehensive view of the sub-fossil diatom biogeography, distribution pattern and oceanographic environmental controls with support of multivariate methods based on Beibu Gulf core-top samples. Cluster analysis of diatom assemblages divides the distribution pattern into four subclusters. Sea surface salinity (SSS), temperature (SST), trophic state (chlorophyll concentration in this study) and water depth constrain the diatom distribution pattern through canonical redundancy analysis although only partly support an interpretation of the relationship between these various variables. Chlorophyll has a strong correlation to diatom distribution, and responds to occurrence, while SSS and SST also have significant influence and indicate warm water invasion from the open SCS. Water depth is a subordinate factor in terms of Beibu Gulf diatom distribution. The ca. 25 m water-depth marks the upper extent of dominance in the northern Beibu Gulf. A strong mixing area with a complex diatom distribution exists below this water depth in the middle of Beibu Gulf. Coastal currents from north of SCS invade Beibu Gulf through Qiongzhou Strait and south of Hainan Island, as recorded by higher percentages of and at these sites. Our results provide a selection of evaluation method for a marine ecological red-line definition for sustainable development. This study highlights the perspective relationships between the spatial distribution of sub-fossil diatom assemblages in surface sediments and oceanographic variables, which could serve as a model for paleoenvironmental and paleoclimatic reconstruction in future marginal sea geoscience research for the Beibu Gulf, northwestern SCS.
北部湾位于中国南海西北部,是一个陆海气相互作用强烈的环境敏感区,位于西太平洋和东印度洋之间的亚洲地区。本研究旨在通过北部湾岩芯顶部样本的多元方法,提供一个关于亚化石硅藻生物地理学、分布模式和海洋环境控制的综合视图。硅藻组合的聚类分析将分布模式分为四个亚群。尽管仅部分支持对这些不同变量之间关系的解释,但通过典范冗余分析,海水盐度(SSS)、温度(SST)、营养状态(本研究中的叶绿素浓度)和水深限制了硅藻的分布模式。叶绿素与硅藻分布具有很强的相关性,并响应于其出现,而 SSS 和 SST 也具有显著的影响,表明温暖的海水从开阔的南海入侵。水深是北部湾硅藻分布的一个次要因素。在北部湾北部,约 25 米的水深标志着硅藻占主导地位的上限。在北部湾中部,水深较浅的地方存在一个强烈混合区,硅藻分布复杂。来自南海北部和海南岛南部的沿岸流通过琼州海峡入侵北部湾,这些地区的 和 比例较高。我们的结果为海洋生态红线的定义提供了一种可持续发展的评估方法选择。本研究强调了表层沉积物中亚化石硅藻组合的空间分布与海洋变量之间的关联关系,这可为未来北部湾、中国南海西北部边缘海地球科学研究中的古环境和古气候重建提供一个模型。