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Tarsals of Early Pinnipedimorphs (Mammalia: Carnivora) from the Lower Miocene, Japan, and Their Early Diversity in the Western North Pacific 日本下中新世早期鳍足类动物(哺乳动物:食肉目)的Tarsals及其在北太平洋西部的早期多样性
IF 0.9 4区 地球科学 Q3 PALEONTOLOGY Pub Date : 2022-07-01 DOI: 10.2517/PR200030
Wataru Tonomori, H. Taru
Abstract. New tarsals (astragalus and entocuneiform) of fossil pinnipeds from the lower Miocene (Burdigalian) Oi Formation in Mie Prefecture, Japan, belonging to early pinnipedimorphs (i.e., enaliarctines or basal odobenids) and cf. Odobenidae gen. et sp. indet. were discovered. A comparison of early pinnipedimorph astragali conclusively indicated that at least three species were represented in the western North Pacific during the early Miocene (Burdigalian). Early pinnipedimorphs clearly showed considerable diversification in the eastern North Pacific during the early Miocene, and our study demonstrates that the early pinnipedimorphs in the western North Pacific also started to diversify around the same time.
摘要日本三重县下中新世(Burdigalian)Oi组鳍足类化石的新跗骨(黄芪和内楔形),属于早期鳍足类动物(即依那拉汀类或基底odobenids),参见Odobenidae gen.et sp.indet。被发现。对早期鳍足类动物Astralali的比较最终表明,在中新世早期(Burdigalian),北太平洋西部至少有三个物种。中新世早期,北太平洋东部的早期鳍足类动物明显表现出相当大的多样性,我们的研究表明,北太平洋西部的早期鳍鳍足类也在同一时间开始多样化。
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引用次数: 0
Fossil Benthic Foraminifera in the Nakdong River Delta (Southeast Korea) during the Early to Middle Holocene 全新世早期至中期洛东江三角洲底栖有孔虫化石
IF 0.9 4区 地球科学 Q3 PALEONTOLOGY Pub Date : 2022-07-01 DOI: 10.2517/PR200037
H. Takata, Seok-Hwi Hong, D. Yoo, Jin-Cheul Kim, D. Cheong, B. Khim
Abstract. We investigated early to middle Holocene benthic foraminifera from four borehole cores in the Nakdong River Delta (southeast Korea) to document faunal associations and the transition of benthic foraminifera in coastal areas along the Tsushima Warm Current. We recognized four varimax factor assemblages. The varimax factor 1 assemblage (characterized by Pseudoparrella naraensis with Eilohedra nipponica) is common throughout core ND-02, which is seaward in the delta, whereas the varimax factor 2 assemblage (characterized by Haynesina sp. A) is dominated by low evenness in core 16ND-C02, which is landward in the delta. The varimax factor 4 assemblage (characterized by Buccella frigida) is generally common at the bottom and/or top part of the studied cores, whereas the varimax factor 3 assemblage (characterized by Elphidium somaense) tends to be common in the upper part of the three cores in the delta's seaward area. Both the contrasting high diversity and low diversity with low evenness of benthic foraminifera (varimax factor 1 and 2 assemblages, respectively) were present between the seaward and landward portions of the delta during the same period (∼7–6 ka), respectively. The combination of these contrasting faunas tended to appear in the delta with the intensification of the Tsushima Warm Current during ∼8–6 ka in addition to the sea-level rise. Common taxa in the Nakdong River Delta are largely neritic species of the temperate region in the East Asian margin, whereas some upper bathyal species, such as Angulogerina ikebei, Bolivina decussata, and E. nipponica, were subordinated in the delta's seaward portion. Such faunal features in the Nakdong River Delta are distinguishable from other coastal areas in the Japanese Islands.
摘要我们从Nakdong河三角洲(韩国东南部)的四个钻孔岩芯中调查了全新世早期至中期的底栖有孔虫,以记录对马暖流沿岸沿海地区的动物群组合和底栖有孔动物的转变。我们识别了四个方差因子组合。varimax因子1组合(以纳氏假鹦鹉藻和日本Eilohedra nipponica为特征)在三角洲向海的ND-02岩芯中很常见,而varimax系数2组合(以海燕属(Haynesina sp.A)为特征)则以三角洲向陆的16ND-C02岩芯的低均匀度为主。varimax因子4组合(以Buccella frigida为特征)通常在所研究岩芯的底部和/或顶部常见,而varimax系数3组合(以Elphidium somanense为特征)往往在三角洲向海区域的三个岩芯的上部常见。在同一时期(~7-6ka),三角洲向海和向陆部分之间分别存在底栖有孔虫的高多样性和低多样性与低均匀性(分别为方差因子1和2组合)。这些对比鲜明的动物群的组合往往出现在三角洲,除了海平面上升外,对马暖流在~8-6ka期间增强。Nakdong河三角洲的常见分类群主要是东亚边缘温带的浅海物种,而一些上半深海物种,如Anguloerina ikebei、Bolina decussata和E.nipponica,则隶属于三角洲的向海部分。Nakdong河三角洲的这种动物群特征与日本群岛的其他沿海地区不同。
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引用次数: 0
Late Cretaceous Dimorphic Scaphitid Ammonoid Genus Yezoites from the Circum-North Pacific Regions 环北太平洋地区晚白垩世二形舟形菊石属叶子岩
IF 0.9 4区 地球科学 Q3 PALEONTOLOGY Pub Date : 2022-07-01 DOI: 10.2517/PR200049
K. Tanabe
Abstract. Yezoites is a Late Cretaceous (Cenomanian–Campanian) small to very small dimorphic ammonoid genus belonging to the Scaphitidae, whose microconchs have a pair of long lateral lappets at the aperture. Based on examination of previously described material including type and figured specimens and newly recovered ones, five species of Yezoites are described herein from the circum-North Pacific regions (Japan, Sakhalin, Kamchatka, Alaska, Oregon, and California); i.e., Y. perrini (Anderson), Y. seabeensis (Cobban and Gryc), and Y. puerculus (Jimbo) from the Turonian, and Y. pseudoaequalis (Yabe) and Y. matsumotoi (Tanabe) from the Coniacian. Of these species, both microconchs and macroconchs are recognized in Y. puerculus and Y. pseudoaequalis, whereas only microconchs are known in the other three species. These Yezoites species characteristically occur in very fine-grained sandstone to silty mudstone facies suggesting an intermediate between nearshore and offshore environments, and can be used supplementarily for biozonation and correlation of the Turonian and Coniacian deposits in the North Pacific regions.
摘要Yezoites是晚白垩世(Cenomanian-Campanian)的一个小到非常小的二形菊石属,属于Scaphitidae,其微钩在开口处有一对长的侧向翻领。基于对先前描述的材料(包括模式和图形标本以及新发现的标本)的检查,本文描述了环北太平洋地区(日本、萨哈林、堪察加半岛、阿拉斯加、俄勒冈州和加利福尼亚州)的五种叶子岩;即来自土仑阶的P.perrini(Anderson)、Y.seaeensis(Cobban和Gryc)和Y.puerculus(Jimbo),以及来自科尼亚阶的Y.pseudoaequalis(Yabe)和Y.matsumotoi(Tanabe)。在这些物种中,小弯钩和大弯钩都在puerculus和Y.pseudoaequalis中被识别,而在其他三个物种中只知道小弯钩。这些Yezoite物种的特征是出现在非常细粒的砂岩到粉砂质泥岩相中,表明其处于近岸和近海环境之间,可补充用于北太平洋地区土仑和科尼亚阶矿床的生物分带和对比。
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引用次数: 2
A Sidneyia-Like Euarthropod from the Guanshan Biota (Cambrian Series 2, Stage 4), Eastern Yunnan, Southwest China 滇东关山生物群中一种似悉尼虫的真节肢动物(寒武纪2系4期)
IF 0.9 4区 地球科学 Q3 PALEONTOLOGY Pub Date : 2022-07-01 DOI: 10.2517/PR200047
Jun Zhao, Yu-jing Li, P. Selden, Pei-yun Cong, Zhixin Yang
Abstract. Sidneyia inexpectans was first excavated in Laurentia, and since then Sidneyia and Sidneyia-like euarthropods have been reported from different continents. Here we describe a new Sidneyia-like euarthropod from the Guanshan biota and, its preserved dorsal exoskeleton and appendages resemble those of S. inexpectans. The discovery in the Guanshan biota provides a new data point of Sidneyia-like euarthropod in Cambrian Stage 4 and a second occurrence on the South China plate.
摘要首次在劳伦蒂亚发掘出无经验的悉尼虫,从那时起,不同大陆都有类似悉尼虫和悉尼虫的真节肢动物的报道。在这里,我们描述了关山生物群中一种新的类似悉尼蛛的真节肢动物,其保存的背侧外骨骼和附肢类似于无经验蛛。关山生物群的发现为寒武系第4期似悉尼节肢动物的发现提供了新的数据点,为华南板块的第二次发现提供了依据。
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引用次数: 0
Pterophyllum pachyrachis (Bennettitales) from the Upper Jurassic to Lower Cretaceous Tetori Group, Fukui Prefecture, Central Japan 日本中部福井县上侏罗统至下白垩统Tetori群的pachyrachis蕨类
IF 0.9 4区 地球科学 Q3 PALEONTOLOGY Pub Date : 2022-04-01 DOI: 10.2517/pr200023
T. Yamada, M. Nishino
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引用次数: 0
Tropical Radiolarian Biostratigraphy from the Early to Late Miocene at ODP Site 714 in the Tropical Indian Ocean 热带印度洋ODP遗址714早至晚中新世热带放射虫生物地层
IF 0.9 4区 地球科学 Q3 PALEONTOLOGY Pub Date : 2022-04-01 DOI: 10.2517/pr200017
S. Kamikuri
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引用次数: 0
Kimuriella gen. nov. (Bennettitales), a Whole-Plant Bennettite from the Oxfordian (Upper Jurassic) Tochikubo Formation of Shidazawa, Minamisōma, Fukushima Prefecture, Northeast Japan Kimuriella gen. 11 . (Bennettitales),一种来自日本东北部福岛县Shidazawa的牛津(上侏罗统)Tochikubo组的全植物bennetite
IF 0.9 4区 地球科学 Q3 PALEONTOLOGY Pub Date : 2022-04-01 DOI: 10.2517/pr200020
C. Pott, H. Takimoto
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引用次数: 0
Latest Olenekian (Early Triassic) Ammonoids from the Uppermost Part of the Osawa Formation (Inai Group) in the South Kitakami Belt, Northeast Japan 日本东北北上南带大泽组上段(稻井群)最新奥连纪(早三叠世)菊石
IF 0.9 4区 地球科学 Q3 PALEONTOLOGY Pub Date : 2022-04-01 DOI: 10.2517/pr200027
M. Ehiro
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引用次数: 2
Tohokubelus gen. nov., the Oldest Belemnite from the Olenekian (Lower Triassic) of Northeast Japan Tohokubelus gen. nov.,日本东北部奥连基纪(下三叠世)最古老的belennite
IF 0.9 4区 地球科学 Q3 PALEONTOLOGY Pub Date : 2022-04-01 DOI: 10.2517/pr200036
S. Niko, M. Ehiro
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引用次数: 4
Fossil Lateral Arm Plates of Stegophiura sladeni (Echinodermata: Ophiuroidea: Ophiurida) from the Middle Pleistocene of Japan 日本更新世中期蛇床虫的侧臂板化石
IF 0.9 4区 地球科学 Q3 PALEONTOLOGY Pub Date : 2022-04-01 DOI: 10.2517/pr200039
M. Okanishi, Shota Mitsui, B. Thuy
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引用次数: 2
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