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Morphometric analysis of coccolithophore genus Reticulofenestra: Insights into taxonomy and evolution during late Eocene to early Oligocene 网状球石藻属的形态测量学分析:始新世晚期至渐新世早期的分类与演化
IF 1.5 4区 地球科学 Q2 PALEONTOLOGY Pub Date : 2025-01-10 DOI: 10.1016/j.marmicro.2024.102435
Ruigang Ma , David Bord , Xiaobo Jin , Chuanlian Liu
The coccolithophore Reticulofenestra is key to understanding late Cenozoic climate change, but taxonomic identification remains challenging. This study uses morphometric and mixture analysis to evaluate taxonomic criteria for late Eocene to early Oligocene Reticulofenestra. The method enables a systematic comparison between the taxonomic morphotypes and the components recognized through Gaussian mixture modeling of parameters of distal shield length, circularity, and central opening ratio. At the species level, a total of nine morphotypes were studied from 6700 data points collected across three study sites in the mid–low latitude Atlantic–Indian Oceans. The results demonstrate that length and circularity effectively distinguish groups, validating their uses as primary taxonomic criteria. Nevertheless, central opening ratio exhibits high intra–group variability, limiting its standalone application. In addition, our integrated data reveal three evolutionary phases: (1) initial diversification during late Eocene cooling; (2) extinction following peak diversity after the Eocene–Oligocene Transition; and (3) early Oligocene stabilization reflecting adaptation in smaller species. This work provides statistical references for the validation of semi-quantitative morphologic descriptions, which may help establish a robust framework for identifying this ecologically vital lineage and enhance our understanding of phytoplankton responses to past environmental changes. Future genomic studies will be crucial for elucidating genotype-phenotype-environment relationships in Reticulofenestra evolution.
球石藻Reticulofenestra是了解晚新生代气候变化的关键,但分类鉴定仍然具有挑战性。本研究采用形态计量学和混合分析方法,对晚始新世至早渐新世网状蕨的分类标准进行了评价。该方法能够将分类形态与通过远端屏蔽长度、圆度和中心开口比参数高斯混合建模识别的组分进行系统比较。在物种水平上,从中低纬度大西洋-印度洋三个研究地点收集的6700个数据点中,共研究了9种形态。结果表明,长度和圆度可以有效地区分类群,验证了它们作为主要分类标准的用途。然而,中心开孔率表现出较高的组内变异性,限制了其单独应用。此外,我们的综合数据揭示了三个演化阶段:(1)始新世晚期冷却时期的初始多样化;(2)始新世-渐新世过渡后的生物多样性高峰灭绝;(3)早渐新世稳定,反映了小物种的适应性。本研究为验证半定量的形态描述提供了统计参考,有助于建立一个强大的框架来识别这一生态重要的谱系,并增强我们对浮游植物对过去环境变化的响应的理解。未来的基因组研究将是阐明网纹蝶进化中基因型-表型-环境关系的关键。
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引用次数: 0
High-resolution Danian–Selandian benthic foraminifera-based paleoenvironmental reconstruction and response to sequence stratigraphy: Inferences from the Elles section, El Kef Basin, Tunisia 突尼斯El Kef盆地Elles剖面的高分辨率Danian-Selandian底栖有孔虫古环境重建及层序地层学响应
IF 1.5 4区 地球科学 Q2 PALEONTOLOGY Pub Date : 2025-01-01 DOI: 10.1016/j.marmicro.2024.102433
Sherif Farouk , Islam El-Sheikh , Sreepat Jain , Fayez Ahmad , Zaineb Elamri , Jenö Nagy , Khaled Al-Kahtany , Youssef S. Bazeen
High-resolution (123 samples) benthic foraminiferal distribution patterns were analyzed for paleoenvironmental reconstruction from a section located at the southern edge of the El Kef Basin (El Haria Formation; Tunisia) spanning the Danian–Selandian interval (planktic foraminifera P1a–P4b zones). Five distinct clusters were identified, each representing different paleoenvironments and depths ranging from inner neritic to upper bathyal, with significant variations in species diversity, paleoproductivity, and bottom water oxygenation. The Dan-C2 hypothermal event is characterized by moderately oxygenated bottom waters, high species diversity, and lowered paleoproductivity within an upper bathyal setting. The LDE is marked by high species diversity, higher paleoproductivity, moderately oxygenated bottom waters, abundance of epifaunal species, and shallowing to middle neritic depths. The Danian-Selandian boundary records (a) a sudden abundance of the inner neritic infaunal species Bulimina strobila, (b) an increase in species diversity, (c) moderately‑oxygenated bottom waters, (d) a positive δ13C excursion, and (e) deepening, from inner to middle neritic settings. Four transgressive-regressive (T-R) cycles based on benthic foraminiferal assemblage-derived bathymetry, P% and the transfer function-based estimate mirror each other, and distinctly mirror paleodepth changes, correlating with global eustatic cycles but also reflecting local tectonic influences.
对El Kef盆地南缘(El Haria组)剖面的123个高分辨率底栖有孔虫分布模式进行了古环境重建分析;突尼斯)跨越达尼安-塞兰地间隔(浮游有孔虫P1a-P4b带)。研究区划分出5个不同的群落,每个群落代表了不同的古环境和深度,从内浅海到深海,在物种多样性、古生产力和底水氧合方面存在显著差异。Dan-C2低温事件的特征是底部含氧适中,物种多样性高,古生产力较低。物种多样性高,古生产力高,底水含氧适中,层外物种丰富,浅海至中浅海深。Danian-Selandian边界记录了(a)内浅海动物物种Bulimina strobila的突然丰富,(b)物种多样性的增加,(c)适度含氧的底水,(d) δ13C正偏移,(e)从内浅海环境到中浅海环境的加深。基于底栖有孔虫组合测深、P%和基于传递函数估算的4个海侵-海退(T-R)旋回相互反映,明显反映了古深度变化,与全球起伏旋回相关,但也反映了局部构造影响。
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引用次数: 0
Non-pollen palynomorphs as indicators of local environmental conditions in a Neotropical Estuary (Northeast Brazil) 巴西东北部新热带河口非花粉型孢粉形态对当地环境条件的指示作用
IF 1.5 4区 地球科学 Q2 PALEONTOLOGY Pub Date : 2025-01-01 DOI: 10.1016/j.marmicro.2024.102424
Pietro Martins Barbosa Noga , Anne de Vernal , Daniela Mariano Lopes da Silva , Doriedson Ferreira Gomes
Non-pollen palynomorphs (NPPs) are organic-walled microfossils derived from diverse aquatic and terrestrial organisms, frequently observed in palynological studies. This study documents the distribution of NPPs in surface sediment samples from the two main rivers of Camamu Bay (Northeast Brazil), analyzed to explore their response to estuarine environmental and nutritional gradients. Using standard palynological techniques, 69 NPP taxa were identified, spanning 40 divisions, including dinoflagellates, foraminiferal linings, chlorophytes, cyanobacteria, ciliates, amoebozoans, scolecodonts, zoological fragments, and fungal spores. Assemblages were dominated by fungal spores across most stations. Distinct environmental gradients were reflected in NPP distribution, for instance upstream stations with low salinity (3 psu) and high nutrient ratios favored chlorophytes, while downstream stations with higher salinity (up to 35 psu) and lower N:P ratios (<40 μM) were dominated by foraminiferal linings. Multivariate statistic analyses revealed that salinity and nutrient stoichiometry were significant drivers of assemblage composition. These findings highlight the utility of NPPs as indicators of environmental and biogeochemical conditions, particularly in low-latitude estuarine systems, and underscore their potential applications in paleoecological reconstruction.
非花粉孢粉微化石(NPPs)是来源于水生和陆生生物的有机壁微化石,在孢粉学研究中经常观察到。本研究记录了巴西卡马木湾(Camamu Bay)两条主要河流表层沉积物样品中核动力物质的分布,并分析了它们对河口环境和营养梯度的响应。使用标准孢粉学技术,共鉴定出69个NPP分类群,跨越40个门类,包括鞭毛虫、有孔虫、绿藻、蓝藻、纤毛虫、变形虫、scolecodonts、动物碎片和真菌孢子。大多数站点的组合以真菌孢子为主。NPP分布具有明显的环境梯度,低盐度(3 psu)和高营养比的上游站站有利于绿藻,而高盐度(高达35 psu)和低N:P比(<40 μM)的下游站站则以有孔虫为主。多变量统计分析表明,盐度和营养化学计量学是群落组成的重要驱动因素。这些发现突出了核电厂作为环境和生物地球化学条件指标的效用,特别是在低纬度河口系统中,并强调了它们在古生态重建中的潜在应用。
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引用次数: 0
Benthic foraminiferal population dynamics at the Goban Spur off Southwest Ireland reveal glacial-interglacial bottom water ventilation and organic flux variability over the last 420,000 years 爱尔兰西南部戈班峡的底栖有孔虫种群动态揭示了过去42万年来冰期-间冰期底水通风和有机通量的变化
IF 1.5 4区 地球科学 Q2 PALEONTOLOGY Pub Date : 2025-01-01 DOI: 10.1016/j.marmicro.2024.102432
Stanislaus Glenndy Fabian , Stephen J. Gallagher , David De Vleeschouwer
Benthic foraminiferal assemblages from Deep Sea Drilling Project (DSDP) Site 548 on the Goban Spur off southwestern Ireland shed light on the changes in bottom water oxygenation and organic matter flux to the sea floor during the late Quaternary. Correlations of benthic foraminiferal δ18O values, the relative abundance of Neogloboquadrina pachyderma (%NP), and Ice Rafted Debris (IRD) concentration to global and regional and North Atlantic datasets suggest the upper 60 m of DSDP Site 548 extend to 420,000 years. Downcore variations of >63 μm benthic foraminifera assemblages, abundance, and diversity reveal changes in dissolved oxygen concentration and organic fluxes to the seafloor related to glacial-interglacial cyclicity. Cassidulina laevigata and low dissolved oxygen indicator taxa such as Bolivina spp. and Globobulimina spp. characterised colder climates associated with lighter benthic δ13C values, suggesting minimal organic flux and/or weaker bottom water ventilation. In contrast, warmer interglacials are typified by heavier benthic δ13C, increased %CaCO3, common high dissolved oxygen indicator taxa such as Globocassidulina subglobosa and phytodetritus sensitive taxa such as Alabaminella weddellensis and Epistominella exigua, suggest a more ventilated bottom water and increased organic fluxes to the seafloor, possibly associated with the invigoration of the Mediterranean Outflow Water (MOW).
深海钻探项目(DSDP)在爱尔兰西南部Goban Spur的548站点的底栖有孔虫组合揭示了晚第四纪底水氧合和海底有机质通量的变化。底栖有孔虫δ18O值、厚皮虫(Neogloboquadrina pachyderma)的相对丰度(%NP)和冰筏碎屑(IRD)浓度与全球、区域和北大西洋数据集的相关性表明,DSDP站点548的上60 m延伸至42万年。63 μm底栖有孔虫组合、丰度和多样性的岩心变化揭示了溶解氧浓度和与冰期-间冰期旋回有关的海底有机通量的变化。Cassidulina laevigata和低溶解氧指示分类群(如Bolivina spp.和Globobulimina spp.)表现出较冷的气候特征,与较轻的底栖δ13C值相关,表明有机通量最小和/或底水通风较弱。相比之下,温暖间冰期的特征是底栖生物δ13C升高,CaCO3 %增加,常见的高溶解氧指示类群如Globocassidulina subglobosa和植物碎屑敏感类群如Alabaminella weddellensis和Epistominella exigua,表明底部水更通风,海底有机通量增加,可能与地中海流出水(MOW)的增强有关。
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引用次数: 0
Paleoecological and paleoenvironmental insights from Ornatorotaliidae (larger foraminifera) 大有孔虫Ornatorotaliidae的古生态和古环境研究
IF 1.5 4区 地球科学 Q2 PALEONTOLOGY Pub Date : 2025-01-01 DOI: 10.1016/j.marmicro.2024.102423
Andrea Benedetti , Antonino Briguglio , Lorenzo Consorti , Cesare Andrea Papazzoni
The present study deals with the ecology and phylogenetic relationships among species of the genera Ornatorotalia, Granorotalia, and Risananeiza belonging to the Family Ornatorotaliidae. The microfacies analyses allowed us to assign each taxon to its life paleoenvironment within the shallow-water carbonate setting, and to make a comparison with extant species belonging to the family Calcarinidae. While different species of Ornatorotalia and Granorotalia thrived only in the inner ramp, Risananeiza spp. possibly inhabited also deeper environments up to the middle ramp. The phylogenetic relationships among genera and species are here briefly discussed, nonetheless it's still impossible to identify any unambiguous ancestor of this group.
本文研究了鸟类科鸟类属(Ornatorotalia)、Granorotalia和Risananeiza的生态学和系统发育关系。微相分析使我们能够将每个分类单元分配到浅水碳酸盐环境中的生活古环境中,并与属于Calcarinidae的现有物种进行比较。不同种类的Ornatorotalia和Granorotalia只在坡道内侧繁殖,而Risananeiza可能也在坡道中部较深的环境中生长。这里简要地讨论了属和种之间的系统发育关系,尽管如此,仍然不可能确定这个群体的任何明确的祖先。
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引用次数: 0
Controls on barium incorporation into tests of benthic foraminifera from the Aegean Sea (Eastern Mediterranean Sea) – Towards a species-specific Ba/Ca calibration 爱琴海(东地中海)底栖有孔虫试验中钡掺入的控制。针对特定物种的Ba/Ca校准
IF 1.5 4区 地球科学 Q2 PALEONTOLOGY Pub Date : 2025-01-01 DOI: 10.1016/j.marmicro.2024.102431
Jassin Petersen , Gerhard Schmiedl , Jacek Raddatz , André Bahr , Jörg Pross , Meryem Mojtahid
We have analysed Ba/Ca ratios of live and dead benthic foraminifera (Uvigerina mediterranea and Melonis affinis) from core tops of seven sites located in the Aegean Sea by laser ablation ICP-MS. There are no significant Ba/Ca differences in live and dead specimens of U. mediterranea. For M. affinis we apply a threshold criterion for extremely high Ba/Ca in live specimens in order to highlight the overall uniform Ba/Ca signal. The Ba/Ca intra-test variability varies between 16 and 24 % relative standard deviation per specimen. It is attributed to biomineralisation processes i.e., vital effects. The Ba/Ca ratios of M. affinis are significantly higher than those of U. mediterranea throughout most of the sites and their respective samples from different sediment depths. The influence on Ba/Ca of both species by biomineralisation processes and/or microhabitat effects remains open. Linking the Ba/Ca ratios to measured Ba concentration of bottom waters from one of the studied sites, shows partition coefficients of DBa = 0.34, and DBa = 0.49 for U. mediterranea and M. affinis, respectively. We could not identify trends of Ba/Ca ratios to observed/ modelled gradients of relevant environmental factors between the seven analysed sites, such as primary productivity and associated Corg fluxes or TOC concentrations. Despite the demonstrated limited proxy potential in these parts of the Aegean Sea, we suggest that it is possible to employ Ba/Ca of infaunal benthic species in order to reconstruct export productivity in deep-sea areas with a less complex linkage between primary productivity and nutrient distribution in bottom waters.
我们用激光烧蚀ICP-MS分析了爱琴海7个地点岩心顶部活底栖有孔虫(地中海Uvigerina mediterranea和Melonis affinis)的Ba/Ca比值。在活的和死的地中海鳗标本中Ba/Ca没有显著的差异。对于M. affinis,我们应用了活标本中极高Ba/Ca的阈值标准,以突出整体均匀的Ba/Ca信号。Ba/Ca测试内变异性在每个样品的相对标准偏差为16%至24%之间变化。它归因于生物矿化过程,即生命效应。在大多数地点和不同沉积物深度的样品中,affinis的Ba/Ca比值显著高于U. mediterranea。生物矿化过程和/或微生境效应对两种物种Ba/Ca的影响尚不明确。将其中一个研究地点的Ba/Ca比率与底部水域测量的Ba浓度联系起来,显示地中海和affinis的分配系数分别为DBa = 0.34和DBa = 0.49。我们无法确定七个分析地点之间Ba/Ca比率与观测/模拟的相关环境因子梯度的趋势,例如初级生产力和相关的碳通量或TOC浓度。尽管在爱琴海这些地区的替代潜力有限,但我们认为,在初级生产力与海底营养分布之间的联系不那么复杂的情况下,有可能利用动物底栖生物物种的Ba/Ca来重建深海地区的出口生产力。
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引用次数: 0
Evolutionary, paleoecological and taphonomic aspects of new agglutinated foraminifer Devonodendron scopulum from the Frasnian of Holy Cross Mts, Poland 波兰圣十字山Frasnian新凝集有孔虫Devonodendron scopulum的进化、古生态和地语学方面
IF 1.5 4区 地球科学 Q2 PALEONTOLOGY Pub Date : 2024-12-22 DOI: 10.1016/j.marmicro.2024.102434
Grzegorz Racki
Regularly bifurcated tubiform (tree-like) microfossils, although illustrated three decades ago from the Frasnian of the Holy Cross Mts (southern Poland), have not been studied in detail until now. In this paper, the distinctive microproblematic is interpreted as a calcite-cemented agglutinated foraminifer belonging to Devonodendron scopulum sp. et gen. nov., appearing in a major radiation after the Givetian Revolution. Based on the study of isolated three-dimensional specimens, this Devonian species is the best documented of the early branching foraminifera. It resembles living arborescent representatives of the family Schizamminidae (such as Schizammina arborescens and S. andamana), but also the family Dendrophryidae (Psammatodendron arborescens), which has already been reported in the fossil record (Cretaceous; questionable Silurian). However, in light of genetic studies of modern monothalamids, phylogenetic inferences based on such simple morphology are risky. The tree-like branching system of this species suggests erect attached and filter feeding life habit. Devonodendron scopulum shows a pronounced microhabitat selectivity, being dominantly restricted to mid-slope metazoan-microbial mud-mounds. The buildups provided microniches for flourishing a very abundant and diverse calcareous microbiota, including taxa with known (Nanicella) and presumed (Eifeliflabellum) foraminiferal affinities. The environment was characterized by a specific diagenetic setting for the fossilization of micritic-organic tubular tests due to rapid microbially mediated lithification and overwhelming recrystallization processes. As a result, microfossils are largely preserved as stacked homogeneous rhomboidal calcite plates. Many specimens in some sites are actually just coalesced sparry calcite ‘pseudomorphs’ mimicking the original test morphology.
规律分叉的管状(树状)微化石,虽然在三十年前从圣十字山(波兰南部)的弗拉斯尼安发现,但直到现在还没有被详细研究过。在本文中,这一独特的微问题被解释为一种方解石胶结的有孔虫,属于Devonodendron scopulum sp. et gen. 11 .,出现在Givetian革命后的一次主要辐射中。基于对孤立的三维标本的研究,这个泥盆纪物种是早期分支有孔虫中记录最好的物种。它类似于Schizamminidae科(如Schizammina arborescens和S. andamana)的现存乔木代表,但也类似于已经在化石记录中报道的树科(Psammatodendron arborescens)。可疑的志留纪)。然而,鉴于现代单丘脑的遗传研究,基于这种简单形态的系统发育推断是有风险的。该物种的树状分支系统表明直立附着和滤食的生活习惯。泥盆子具有明显的微生境选择性,主要局限于中坡后生动物-微生物泥丘。这些积累为丰富多样的钙质微生物群提供了微生态环境,包括已知的(Nanicella)和推定的(Eifeliflabellum)有孔虫类群。由于快速的微生物介导的岩化作用和压倒性的再结晶过程,该环境的特点是为微晶有机管状试验的石化提供了特定的成岩环境。因此,微化石大部分以堆积均匀的菱形方解石板的形式保存下来。在一些地点的许多标本实际上只是合并的亮晶方解石“假晶”,模仿原始的测试形态。
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引用次数: 0
Eocene to Early Miocene dinoflagellate cysts from the southern Gulf of Mexico 墨西哥湾南部始新世至中新世早期的鞭毛藻囊肿
IF 1.5 4区 地球科学 Q2 PALEONTOLOGY Pub Date : 2024-12-01 DOI: 10.1016/j.marmicro.2024.102422
Alessandro-Cesare Bruno, Javier Helenes
This paper documents the Eocene to Miocene dinoflagellate cyst assemblages found at Site 94 in the southern part of the Gulf of Mexico. Four unique dinoflagellate cyst assemblages representing depositional periods from the Early Eocene to the Early Miocene are defined in this study. The Early to Middle Eocene assemblage presents the highest average concentrations of dinoflagellate cysts, is dominated by Operculodinium, and contains few heterotrophic taxa. The Early Oligocene assemblage has medium concentration and is dominated by Deflandrea. The Late Oligocene also has high average concentrations of dinoflagellate cysts, is dominated by Homotryblium, and contains few heterotrophic taxa. The Early Miocene assemblage has lower average concentrations of dinoflagellate cysts, is dominated by Pyxidinopsis, and lacks heterotrophic taxa. Our palynological data is related to significant regional paleogeographic and paleoceanographic changes. Namely, the Early to Middle Eocene free flow of tropical water masses from the south and the Late Eocene restriction of this flow by a land bridge connecting northern South America to Cuba in the north. The Oligocene gradual return of the tropical water masses and finally, the Early Miocene emergence of the Florida Platform when the Gulf of Mexico reached modern oceanographic conditions. The stratigraphic ranges of selected dinoflagellate cysts fit in age with previous microfossil data from the site and allowed us to define the Early Oligocene - Late Oligocene transition. The presence of well-preserved dinoflagellate cysts allowed the identification of 60 species and the discovery of three new species: Achomosphaera psilata sp. nov., Carpatella reticulata sp. nov., and Hystrichosphaeropsis gulficum sp. nov.
本文记录了墨西哥湾南部94号遗址发现的始新世至中新世鞭毛藻囊群。本研究确定了四个独特的鞭毛藻囊组合,代表了早始新世至早中新世的沉积时期。早至中始新世组合中鞭毛藻包囊平均浓度最高,以包鞭毛藻为主,异养类群较少。早渐新世组合浓度中等,以偏陆系为主。晚渐新世也有高平均浓度的鞭毛藻囊,以同鞭毛藻为主,异养类群较少。早中新世组合中鞭毛藻囊的平均浓度较低,以Pyxidinopsis为主,缺乏异养分类群。我们的孢粉学数据与显著的区域古地理和古海洋变化有关。即,早始新世至中始新世热带水团从南部自由流动,晚始新世由连接南美洲北部和古巴北部的陆桥限制这种流动。渐新世热带水团逐渐回归,最终,早中新世佛罗里达台地出现,墨西哥湾达到现代海洋条件。所选择的鞭毛藻囊的地层范围与该地点先前的微化石数据相吻合,使我们能够确定早渐新世-晚渐新世的过渡。保存完好的鞭毛藻包囊鉴定了60个物种,并发现了3个新种:Achomosphaera psilata sp. nov.、Carpatella reticulata sp. nov.和Hystrichosphaeropsis gulficum sp. nov.。
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引用次数: 0
Unraveling the palaeoecology of Paralia sulcata-dominated assemblages from Late Miocene marine deposits of Patagonia (South Atlantic, Argentina) 巴塔哥尼亚(阿根廷南大西洋)晚中新世海相沉积中以Paralia sulcata为主的集合体的古生态学研究
IF 1.5 4区 地球科学 Q2 PALEONTOLOGY Pub Date : 2024-11-21 DOI: 10.1016/j.marmicro.2024.102421
Aylén Allende Mosquera , Rocío Fayó , Camilo Andrés Vélez-Agudelo , Marcela Alcira Espinosa , José Ignacio Cuitiño
The study of fossil diatom assemblages constitutes an effective tool for inferring past water conditions. Several studies from around the world suggest the Miocene was a key period in the evolutionary history of diatoms. However, Miocene diatom assemblages from the southwestern Atlantic Ocean are nearly unknown. This study aims to provide a palaeoenvironmental interpretation of the analysed succession. Additionally, to highlight temporal and regional changes, the assemblage is compared with known modern and fossil assemblages from Patagonia and other regions of the world. Finally, we provide a detailed description of the extinct diatom taxa recognised throughout the sedimentary succession. A total of 36 diatom taxa were recognised in the 25 analysed samples. Despite the evidence from sedimentology and macro-palaeontology indicating temporal changes from inner shelf to estuarine environments, the diatom assemblages are dominated by the coastal marine Paralia sulcata sensu lato throughout the succession. An important freshwater input into the coastal system is interpreted from our results reflecting more humid climatic conditions when compared with modern diatom assemblages from the same location. In addition, four extinct species were recognised: Thalassiosira cf. yabei, Pseudopodosira westii, Rhaphoneis diamantella, and Lancineis rectilatus. The presence of R. diamantella and L. rectilatus in the analysed deposits would imply an expansion of their geological range.
硅藻化石组合研究是推断过去水体状况的有效工具。世界各地的一些研究表明,中新世是硅藻进化史上的一个关键时期。然而,大西洋西南部的中新世硅藻群几乎无人知晓。本研究旨在对所分析的演替进行古环境解释。此外,为了突出时间和区域变化,我们还将该组合与巴塔哥尼亚和世界其他地区的已知现代和化石组合进行了比较。最后,我们对整个沉积演替中已灭绝的硅藻类群进行了详细描述。在分析的 25 个样本中,共确认了 36 个硅藻类群。尽管沉积学和大型古生物学的证据表明,从内陆架到河口环境发生了时间变化,但在整个演替过程中,硅藻群仍以近岸海洋硅藻(Paralia sulcata sensu lato)为主。与同一地点的现代硅藻群相比,我们的研究结果反映了更潮湿的气候条件,从而解释了淡水对沿岸系统的重要输入。此外,我们还发现了四个已灭绝的物种:Thalassiosira cf. yabei、Pseudopodosira westii、Rhaphoneis diamantella 和 Lancineis rectilatus。R. diamantella 和 L. rectilatus 出现在分析的沉积物中,这意味着它们的地质分布范围有所扩大。
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引用次数: 0
Ocean gateways and circulation dynamics: Unveiling the deep water-mass properties in the western equatorial Pacific since the Middle Miocene 海洋门户和环流动力学:揭示中新世以来西赤道太平洋的深层水团特性
IF 1.5 4区 地球科学 Q2 PALEONTOLOGY Pub Date : 2024-11-20 DOI: 10.1016/j.marmicro.2024.102420
Himanshu Bali, Anil K. Gupta
Tectonically driven adjustments in the ocean gateways, such as the constriction and closure of the Central American Seaway (CAS), have been linked to the significant variations in deep water circulations across the Atlantic and Pacific Oceans in the Miocene. The changes in these tectonic gateways had substantial consequences on the Atlantic Meridional Overturning Circulation (AMOC), the Antarctic Circumpolar Current (ACC) and consequently Antarctic ice sheet growth, and deep water circulation pathways across the ocean basins. The timing of the closure of the deep water connection between the Atlantic and Pacific Oceans, through CAS, and related changes in deep water circulation in the western Pacific are still debatable. We examined foraminiferal relative abundances of epibenthic genus Cibicidoides (a synonym of Cibicides) and its stable isotopic ratios to decipher the timing of tectonically controlled changes in deep water circulation since the Middle Miocene at ODP Site 807, western equatorial Pacific. Our findings, correlated with previously published data, suggest the North Component Water (NCW) incursion from the Atlantic to the western Pacific (Site 807) via CAS between ∼12.5 and ∼ 9.5 Ma. An abrupt decrease in benthic foraminifer Cibicidoides kullenbergi at ∼9.5 Ma suggests the initiation of a significant shift in the deep water mass, coinciding with the major δ13C divergence between the Atlantic and Pacific oceans.
中新世时期大西洋和太平洋深水环流的显著变化与构造驱动的海洋通道调整有关,如中美洲海道(CAS)的收缩和关闭。这些构造通道的变化对大西洋经向翻转环流(AMOC)、南极环极洋流(ACC)产生了重大影响,从而导致了南极冰盖的增长,并影响了整个大洋盆地的深水环流路径。通过南极环流关闭大西洋和太平洋之间深水联系的时间以及西太平洋深水环流的相关变化仍有争议。我们研究了赤道西太平洋 ODP 807 号地点有孔虫属 Cibicidoides(Cibicides 的异名)的有孔虫相对丰度及其稳定同位素比值,以破译中新世以来受构造控制的深水环流变化的时间。我们的研究结果与之前公布的数据相关,表明北成分水(NCW)在 12.5 至 9.5 马年之间通过中科院从大西洋侵入西太平洋(807 号站点)。底栖有孔虫 Cibicidoides kullenbergi 在 9.5 Ma ∼突然减少,表明深海水团开始发生重大转变,与大西洋和太平洋之间的主要 δ13C 分异相吻合。
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Marine Micropaleontology
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