日本地球惑星科学連合2024年大会

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[E] ポスター発表

セッション記号 B (地球生命科学) » B-CG 地球生命科学複合領域・一般

[B-CG05] Frontier in diversity and ecology of protists and microfossils

2024年5月31日(金) 17:15 〜 18:45 ポスター会場 (幕張メッセ国際展示場 6ホール)

コンビーナ:堀 利栄(愛媛大学大学院理工学研究科 地球進化学)、氏家 由利香(高知大学)、仲村 康秀(島根大学エスチュアリー研究センター)、Baumgartner Oliver Baumgartner(University of Lausanne)


17:15 〜 18:45

[BCG05-P07] バウ石灰岩(マレーシア,ボルネオ島北西部)から産したジュラ紀新世放散虫化石と海綿骨針化石

*柏木 健司1、福元 結1、柿崎 喜宏2 (1.富山大学理学部自然環境科学科、2.室戸ユネスコ世界ジオパーク)

キーワード:バウ石灰岩、ジュラ紀新世、放散虫、Vulpess、海綿骨針、rhaxella sorbyana

The Bau Limestone in northwestern Borneo Island, Malaysia, is one of the representative reef complexes deposited in shallow water near the equator during the Late Jurassic. The Bau Limestone is located at the gateway between the Paleo-Pacific Ocean and the Tethys Sea at that time, and is of great interest from the viewpoint of paleoceanography, which led to many paleontological studies (ex., foraminifers and brachiopods) during the 1960s and '70s. Based on the fossil occurrences, strontium and carbon isotopic stratigraphy (Kakizaki et al., 2013), and stratigraphic relationships with the strata above and below, the age of the Bau Limestone has been estimated to be roughly Late Jurassic to Early Cretaceous.
Four calcarenite samples collected from the reef slope sediments of ca. 15 m thick yield small amounts of radiolarians and abundant sponge spicules; A-66, Stichocapsa convexa (Yao, 1979); A-68, Cenosphaera spp., Gorgansium sp. Pantanellium spp., Vallupus sp.; A-76, Archaeodictyomitra apiarium (Rüst, 1885), Gongylothorax favosus (Dumitrica, 1970), Holocryptocanium barbui (Dumitrica, 1970), Pseudodictyomitra carpatica (Lozyniak, 1969), Zhamoidellum sp. aff. Z. ovum (Dumitrica, 1970), Zhamoidellum sp. A; A-77, badly-preserved and pyritized radiolarians. Based on the UAZone of Baumgartner et al. (1995), the occurrence range of radiolarians falls within UAZone 10-13, which is assigned to the Kimmeridgian-Tithonian interval of the Late Jurassic. Vallupus sp. from sample A-68 belongs to the Vallupinae, which shows a restricted occurrence range of the Late Jurassic and the acme in the Tithonian of latest Jurassic (Matsuoka, 1995). Calcarenite bearing radiolarians and sponge spicules in Bau Limestone probably indicates Tithonian in age.
Among the sponge spicules from four samples, a kidney-shaped those with a distinct hilum were abundant, which were identified as Rhaxella sorbyana (Blake). This morphotype from Jurassic and Cretaceous strata has been often described for rhaxes. A total of 226 individuals from the Bau Limestone showed a height of 89-196 μm and a width of 68-166 μm, with a strong positive correlation between height and width. Although the surfaces of most of the specimens were more or less corroded, 21 specimens among them showed surface ornamentation with numerous knobs connected by radially-extending bars. Rhaxella sorbyana is similar in geometry of its surface ornamentation and overall outline to oval to subspherical selenaster sponge spicules of recent Placospongiidae.