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Estonian Journal of Earth Sciences最新文献

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An integrative biostratigraphic, chemostratigraphic, and sequence stratigraphic perspective of the Ordovician–Silurian boundary on Anticosti Island (Canada) 加拿大Anticosti岛奥陶系—志留系界线的生物地层学、化学地层学和层序地层学综合研究
IF 1.1 4区 地球科学 Q4 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2023-01-01 DOI: 10.3176/earth.2023.28
J. Zimmt, S. M. Holland, M. Cappello, D. S. Jones, J. Jin, J. Husson, B. Schoene, C. Mitchell, M. Melchin, S. Finnegan, A. Desrochers
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引用次数: 1
Lower–Middle Ordovician brachiopods from the Eastern Cordillera of Peru: biostratigraphical and palaeobiogeographical significance 秘鲁东部科迪勒拉地区中下奥陶统腕足类:生物地层和古生物地理意义
IF 1.1 4区 地球科学 Q4 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2023-01-01 DOI: 10.3176/earth.2023.16
J. Colmenar, J. C. Gutiérrez-Marco, C. Chacaltana
Lower–Middle Ordovician brachiopods are well known from the Central Andean Basin of Argentina and Bolivia, but relatively little data comes from its northern prolongation in the Altiplano and the Eastern Cordillera of Peru. Here we present information about brachiopods collected from the San José Formation (Fm) from several sections located at the northeast of the Apurímac River valley in the surroundings of Kimbiri city in the Eastern Cordillera. From northwest to southeast the sections and their locations are: Libertad, in the mountain trail between this hamlet and the city of Pichari; Catarata and Nueva Alianza, in the mountain trail between Oroya and the last hamlet; and Kimbiri ( K ) , in the trail parallel to the Kashiroveni stream north of the village of Kimbiri Alto. In these localities the San José Fm lies unconformably on Neoproterozoic rocks, reaching the maximum thickness of about 700 m. This shale-dominated formation comprises a biostratigraphically almost complete succession of the upper Tremadocian to lower Sandbian strata and contains graptolites, trilobites, brachiopods, molluscs, echinoderms and ostracods, as well as some conodonts and other microfossils. The upper part of the San José Fm is unconformably overlain by a thick sandy and diamictic succession, known as the Kimbiri Fm. About 30 fossiliferous levels have been found
中下奥陶统腕足动物在阿根廷和玻利维亚的安第斯盆地中部广为人知,但在其北部延伸的Altiplano和秘鲁的东科迪勒拉地区的资料相对较少。在这里,我们介绍了在东部科迪勒拉Kimbiri市周围Apurímac河谷东北部几个部分的San joss组(Fm)中收集的腕足类动物的信息。从西北到东南,这些路段和它们的位置是:Libertad,在这个村庄和Pichari市之间的山路上;卡塔塔和新阿里安萨,在奥罗亚和最后一个村庄之间的山路上;和Kimbiri (K),在Kimbiri Alto村以北与Kashiroveni河平行的小径上。在这些地区,圣何塞湖不整合地位于新元古代的岩石上,最大厚度约为700米。该组以页岩为主,生物地层上几乎完整地承继了上特拉马多纪至下沙边地层,包含笔石、三叶虫、腕足动物、软体动物、棘皮动物和介形虫,以及一些牙形刺和其他微化石。圣约瑟层的上部不整合地覆盖着一层被称为金比里层的厚砂和含砾层。已经发现了大约30个化石层
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引用次数: 0
An evo-devo perspective on no Ordovician land plants 非奥陶纪陆生植物的进化视角
IF 1.1 4区 地球科学 Q4 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2023-01-01 DOI: 10.3176/earth.2023.31
P. Strother
Molecular phylogenetic studies of land plant (embryophyte) origins have begun to tease apart those evolutionary contributions derived from prior algal genes and those de novo genes that evolved during a charophyte–embryophyte transition. Applying the concept of genomic assembly in plant evolution to the fossil record leads to a paradigm shift in the interpretation of the Ordovician record of land plants. Traditional phylogenetic thinking requires fossil species taxa to occupy nodes on a phylogeny. An evo-devo approach can view character evolution separately from species taxa, freeing up fossil spores and tissue fragments to become clues to underlying developmental pathways or gene regulatory networks. This results in a re-assess ment of what is meant by the presence of land plants in the Ordovician landscape. The new model helps to reconcile discrepancies between molecular time-trees and the “missing” record of fossil plants during the Ordovician Period.
陆生植物(胚胎植物)起源的分子系统发育研究已经开始梳理出那些来自先前藻类基因的进化贡献,以及那些在绿叶植物-胚胎植物过渡过程中进化的新生基因。将植物进化中的基因组组装概念应用于化石记录,将导致奥陶纪陆地植物记录解释的范式转变。传统的系统发育思想要求化石物种分类群在系统发育中占据节点。进化-发展方法可以从物种分类群中分离出特征进化,释放出化石孢子和组织碎片,从而成为潜在发育途径或基因调控网络的线索。这导致了对奥陶纪景观中陆地植物存在的意义的重新评估。这个新模型有助于调和分子时间树和奥陶纪时期“缺失”的植物化石记录之间的差异。
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引用次数: 0
Ichnogenus Trypanites in the Ordovician of Estonia (Baltica) 爱沙尼亚(波罗的海)奥陶纪的鱼属锥虫
IF 1.1 4区 地球科学 Q4 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2023-01-01 DOI: 10.3176/earth.2023.48
U. Toom, J. Kuva, D. Knaust
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引用次数: 0
Diversification and speciation among Laurentian brachiopods during the GOBE: insights from basinal and regional analyses GOBE时期Laurentian腕足动物的多样化和物种形成:来自盆地和区域分析的见解
IF 1.1 4区 地球科学 Q4 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2023-01-01 DOI: 10.3176/earth.2023.69
A. Stigall, S. M. Censullo, S. Hennessey, J. Bauer, A. Lam, D. Wright
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引用次数: 0
Recent advances in the Ordovician stratigraphy of the Baltic Palaeobasin and Tornquist margin of Baltica 波罗的海古盆地与托恩奎斯特边缘奥陶系地层研究进展
IF 1.1 4区 地球科学 Q4 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2023-01-01 DOI: 10.3176/earth.2023.54
T. Meidla, L. Ainsaar, O. Hints, S. Radzevičius
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引用次数: 0
Ordovician scientometrics 奥陶系科学计量学
IF 1.1 4区 地球科学 Q4 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2023-01-01 DOI: 10.3176/earth.2023.56
A. Mazoni, R. Costas, C. Zabini
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引用次数: 0
Changes in shelf phosphorus burial during the Hirnantian glaciation and its implications 海南天冰期陆架磷埋藏变化及其意义
IF 1.1 4区 地球科学 Q4 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2023-01-01 DOI: 10.3176/earth.2023.19
J. Müller, M. Joachimski, O. Lehnert, P. Männik, Y. Sun
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引用次数: 0
Palaeozoic carbon isotope excursions and carbonate component analysis 古生代碳同位素偏移与碳酸盐组分分析
IF 1.1 4区 地球科学 Q4 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2023-01-01 DOI: 10.3176/earth.2023.36
I. A. Martin, L. Ainsaar, A. Lepland
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引用次数: 0
Latest Ordovician age of the Spinachitina fragilis Chitinozoan Biozone in Baltoscandia Baltoscandia地区Spinachitina fragilis几丁虫生物带的最新奥陶纪时代
IF 1.1 4区 地球科学 Q4 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2023-01-01 DOI: 10.3176/earth.2023.51
J. Nõlvak, Y. Liang, O. Hints
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引用次数: 0
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Estonian Journal of Earth Sciences
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