Coccolithophore assemblage changes over the past 9 kyrs BP from a climate hotspot in Tasmania, southeast Australia

IF 1.5 4区 地球科学 Q2 PALEONTOLOGY Marine Micropaleontology Pub Date : 2023-03-01 DOI:10.1016/j.marmicro.2023.102209
Bradley Paine, Linda Armbrecht, Christopher Bolch, Gustaaf M. Hallegraeff
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引用次数: 1

Abstract

Predicting phytoplankton responses to a changing climate on Tasmania's east coast is presently based on short-term plankton data sets (∼75 years). However, to better predict future phytoplankton composition, it is crucial to understand longer-term variations from geological records. A particularly important group are the coccolithophores given their vital contribution to the oceanic carbon pump.

Here, we expand the archive of coccolithophores in southeast Australian waters by analysing coccolith assemblages in a 268 cm-long marine sediment core collected off Maria Island, Tasmania, using light and scanning electron microscopy in combination with sedimentary ancient DNA (sedaDNA) techniques.

Coccoliths underwent a shift from a cold to warm-water adapted assemblage at ∼8.2 kyrs BP expressed by a transition in species dominance from the cold-water species Gephyrocapsa muellerae to the warmer-water species Emiliania huxleyi Type A. A period of coccolithophore community instability characterised by reduced diversity and species richness was also detected spanning ∼900 yrs. between 6 and 5 kyrs BP. The latter may be associated with a Mid-Holocene warm period in the Southern Ocean as well as sea-level rise changing the study site from a shallow coastal to deep water habitat.

Emiliania huxleyi coccoliths displayed the highest total relative abundance, but less prevalent larger taxa (Calcidiscus, Coccolithus, Helicosphaera) accounted for >50% of total estimated coccolith CaCO3 sequestration, indicating that relatively scarce, densely calcified species do the ‘heavy-lifting’ of this process. Analysis of sedaDNA revealed coccolithophores contributed ∼44% to the total palaeo eukaryote composition, underlining their importance as part of the marine ecosystem in the study region. The detection of oceanographic shifts and subsequent coccolithophore assemblage composition, including past transitions of species dominance, offer valuable insight into the biological future of southeast Australian waters.

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澳大利亚东南部塔斯马尼亚气候热点地区过去9年的球石团组合变化
目前,预测塔斯马尼亚东海岸浮游植物对气候变化的反应是基于短期浮游生物数据集(~ 75年)。然而,为了更好地预测未来浮游植物的组成,从地质记录中了解长期变化是至关重要的。一个特别重要的群体是球石藻,因为它们对海洋碳泵的贡献至关重要。在这里,我们利用光学和扫描电子显微镜结合沉积古DNA (sedaDNA)技术,分析了在塔斯马尼亚岛玛丽亚岛收集的268厘米长的海洋沉积物岩心中的球粒石组合,从而扩大了澳大利亚东南部水域的球粒石藻档案。在约8.2万年的BP,球石群经历了从适应冷水到适应温水组合的转变,表现为物种优势从冷水物种Gephyrocapsa muellerae到温暖水物种Emiliania huxleyi a型的转变。在约900年的时间里,还发现了以多样性和物种丰富度降低为特征的球石群不稳定时期。血压在6到5岁之间。后者可能与南大洋的中全新世暖期以及海平面上升将研究地点从浅海沿岸变为深水栖息地有关。huxleyi球粒岩显示出最高的总相对丰度,但不太普遍的大型分类群(Calcidiscus, Coccolithus, Helicosphaera)占估计的球粒岩CaCO3固存总量的50%,表明相对稀缺、密集钙化的物种承担了这一过程的“重任”。sedaDNA分析显示,粒石藻占古真核生物总组成的44%,强调了它们作为研究区域海洋生态系统一部分的重要性。对海洋变化和随后的球石团组合组成的检测,包括物种优势的过去转变,为了解澳大利亚东南部水域的生物未来提供了有价值的见解。
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来源期刊
Marine Micropaleontology
Marine Micropaleontology 地学-古生物学
CiteScore
3.70
自引率
15.80%
发文量
62
审稿时长
26.7 weeks
期刊介绍: Marine Micropaleontology is an international journal publishing original, innovative and significant scientific papers in all fields related to marine microfossils, including ecology and paleoecology, biology and paleobiology, paleoceanography and paleoclimatology, environmental monitoring, taphonomy, evolution and molecular phylogeny. The journal strongly encourages the publication of articles in which marine microfossils and/or their chemical composition are used to solve fundamental geological, environmental and biological problems. However, it does not publish purely stratigraphic or taxonomic papers. In Marine Micropaleontology, a special section is dedicated to short papers on new methods and protocols using marine microfossils. We solicit special issues on hot topics in marine micropaleontology and review articles on timely subjects.
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