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dc.contributor.authorKikuchi, Kazukien
dc.contributor.authorNaruse, Hajimeen
dc.contributor.alternative成瀬, 元ja
dc.date.accessioned2024-02-19T05:14:04Z-
dc.date.available2024-02-19T05:14:04Z-
dc.date.issued2024-03-01-
dc.identifier.urihttp://hdl.handle.net/2433/287035-
dc.description.abstractA convolutional neural network (CNN) was used to construct a semantic segmentation model to examine the abundance of Phycosiphon incertum by identifying the trace fossil regions in core section images. The abundance of trace fossils provides information about the past activities of benthic animals affected by paleoenvironmental conditions. To quantify the intensity of bioturbation, it is necessary to extract regions of trace fossils and measure the proportion of bioturbated and the observed area of the outcrop section. In this study, a U-Net-type CNN model was used with residual connections and attention mechanisms to identify the trace fossil Phycosiphon. The model was trained to recognize the relationships between core section images from the International Ocean Discovery Program Expedition 362 Site U1480 and manually annotated trace fossil images. After training, the model successfully classified the pixels of the background, outcrop, and Phycosiphon for core section images other than the training data set. The bioturbation intensity estimated from the image predicted by the model was nearly equal to that from the ground truth image. A long-term (approximately past 10 Myr) variation in Phycosiphon abundance was estimated by applying the model to the core section images at Site U1480. Phycosiphon abundance negatively correlated with the number of sandstone layer intercalations, but it was not affected by the sediment accumulation rates. These findings may reflect resistance of Phycosiphon producers to environmental stress. The model developed in this study can be used for other ichnotaxa to reveal the general tendency of variation in bioturbation intensity and ichnodiversity.en
dc.language.isoeng-
dc.publisherElsevier BVen
dc.rights© 2024. This manuscript version is made available under the CC-BY-NC-ND 4.0 license.en
dc.rightsThe full-text file will be made open to the public on 1 March 2026 in accordance with publisher's 'Terms and Conditions for Self-Archiving'.en
dc.rightsThis is not the published version. Please cite only the published version. この論文は出版社版でありません。引用の際には出版社版をご確認ご利用ください。en
dc.rights.urihttps://creativecommons.org/licenses/by-nc-nd/4.0/-
dc.subjectIchnologyen
dc.subjectSubmarine-fan depositsen
dc.subjectIODP Exp.362en
dc.subjectU-Neten
dc.subjectSemantic segmentationen
dc.subjectDeep learningen
dc.titleAbundance of trace fossil Phycosiphon incertum in core sections measured using a convolutional neural networken
dc.typejournal article-
dc.type.niitypeJournal Article-
dc.identifier.jtitleSedimentary Geologyen
dc.identifier.volume461-
dc.relation.doi10.1016/j.sedgeo.2023.106570-
dc.textversionauthor-
dc.identifier.artnum106570-
dcterms.accessRightsembargoed access-
datacite.date.available2026-03-01-
datacite.awardNumber20J01599-
datacite.awardNumber20H01985-
datacite.awardNumber.urihttps://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-20J01599/-
datacite.awardNumber.urihttps://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-20H01985/-
dc.identifier.pissn0037-0738-
dc.identifier.eissn1879-0968-
jpcoar.funderName日本学術振興会ja
jpcoar.funderName日本学術振興会ja
jpcoar.awardTitle白亜紀/古第三紀境界の大量絶滅に伴う深海底生動物群集の行動様式の進化過程の解明ja
jpcoar.awardTitleタービダイトは地震・津波を記録するのか?: 深層学習逆解析による解明ja
出現コレクション:学術雑誌掲載論文等

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