Larger benthic foraminifera and strontium isotope stratigraphy of the Palaeocene limestones in the Guru area, south Xizang (Tibet): An attempt to build a high-resolution biozonation for the eastern Neo-Tethys

Larger benthic foraminifera (LBF) are one of the most important microfossil groups for Palaeogene biostratigraphy, particularly for shallow-marine carbonate deposits. During the Palaeocene, LBF thrived throughout the Neo-Tethyan Ocean, especially in the eastern Neo-Tethys. However, previous studies...

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Published inPalaeoworld Vol. 34; no. 4; p. 200903
Main Authors Ma, Xue-Song, Zhang, Qing-Hai, Ding, Lin, Zhang, Qian
Format Journal Article
LanguageEnglish
Published Elsevier B.V 01.08.2025
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Abstract Larger benthic foraminifera (LBF) are one of the most important microfossil groups for Palaeogene biostratigraphy, particularly for shallow-marine carbonate deposits. During the Palaeocene, LBF thrived throughout the Neo-Tethyan Ocean, especially in the eastern Neo-Tethys. However, previous studies on Palaeocene LBF biostratigraphy in this area are relatively poor. This paper presents a detailed stratigraphic study of LBF and strontium isotope from the Palaeocene limestones at Guru, south Tibet. About 68 species of 29 genera were identified, among which 19 species are reported for the first time from south Tibet. Following an Oppel zone approach and adopting some key index fossils that are widely accepted in the Neo-Tethys, four Shallow Benthic Zones (SBZ) ranging from SBZ 2 to SBZ 5 were recognised. Based on detailed LBF changes in each SBZ, we tentatively divide SBZ 2 (uppermost Danian–upper Selandian), SBZ 3 (upper Selandian–middle Thanetian), and SBZ 5 (upper Thanetian) into 3, 3, and 2 sub-biozones, respectively. The 87Sr/86Sr ratios from 42 bulk carbonate samples were measured to construct an independent age framework for the Palaeocene limestones. Integration of LBF and 87Sr/86Sr data yielded a high-resolution stratigraphy and provided absolute age controls for each SBZ. Ages of SBZ 2, SBZ 3, SBZ 4, and SBZ 5 were estimated to be ∼62–60 Ma, ∼60–57.4 Ma, ∼57.4–57 Ma, and ∼57–56 Ma, respectively. Our newly built Palaeocene LBF biostratigraphy at Guru needs further testing from other areas in the Neo-Tethyan realm, and is open for refinement and correction in the future.
AbstractList Larger benthic foraminifera (LBF) are one of the most important microfossil groups for Palaeogene biostratigraphy, particularly for shallow-marine carbonate deposits. During the Palaeocene, LBF thrived throughout the Neo-Tethyan Ocean, especially in the eastern Neo-Tethys. However, previous studies on Palaeocene LBF biostratigraphy in this area are relatively poor. This paper presents a detailed stratigraphic study of LBF and strontium isotope from the Palaeocene limestones at Guru, south Tibet. About 68 species of 29 genera were identified, among which 19 species are reported for the first time from south Tibet. Following an Oppel zone approach and adopting some key index fossils that are widely accepted in the Neo-Tethys, four Shallow Benthic Zones (SBZ) ranging from SBZ 2 to SBZ 5 were recognised. Based on detailed LBF changes in each SBZ, we tentatively divide SBZ 2 (uppermost Danian–upper Selandian), SBZ 3 (upper Selandian–middle Thanetian), and SBZ 5 (upper Thanetian) into 3, 3, and 2 sub-biozones, respectively. The 87Sr/86Sr ratios from 42 bulk carbonate samples were measured to construct an independent age framework for the Palaeocene limestones. Integration of LBF and 87Sr/86Sr data yielded a high-resolution stratigraphy and provided absolute age controls for each SBZ. Ages of SBZ 2, SBZ 3, SBZ 4, and SBZ 5 were estimated to be ∼62–60 Ma, ∼60–57.4 Ma, ∼57.4–57 Ma, and ∼57–56 Ma, respectively. Our newly built Palaeocene LBF biostratigraphy at Guru needs further testing from other areas in the Neo-Tethyan realm, and is open for refinement and correction in the future.
ArticleNumber 200903
Author Zhang, Qing-Hai
Zhang, Qian
Ding, Lin
Ma, Xue-Song
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  givenname: Qing-Hai
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– sequence: 4
  givenname: Qian
  surname: Zhang
  fullname: Zhang, Qian
  organization: State Key Laboratory of Tibetan Plateau Earth System, Environment and Resources (TPESER), Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100101, China
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Keywords larger benthic foraminifera
Neo-Tethyan Ocean
Palaeocene
Shallow Benthic Zone
strontium isotope
south Tibet
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  year: 2008
  ident: 10.1016/j.palwor.2024.200903_b0250
  article-title: SBZ 2–6 larger foraminiferal assemblages from the Apulian and Pre-Apulian domains
  publication-title: Atti del Museo Civico di Storia Naturale di Trieste
– volume: 575
  year: 2021
  ident: 10.1016/j.palwor.2024.200903_b0170
  article-title: Larger benthic foraminiferal response to the PETM in the Potwar Basin (Eastern Neotethys, Pakistan)
  publication-title: Palaeogeography, Palaeoclimatology, Palaeoecology
  doi: 10.1016/j.palaeo.2021.110450
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Snippet Larger benthic foraminifera (LBF) are one of the most important microfossil groups for Palaeogene biostratigraphy, particularly for shallow-marine carbonate...
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elsevier
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StartPage 200903
SubjectTerms larger benthic foraminifera
Neo-Tethyan Ocean
Palaeocene
Shallow Benthic Zone
south Tibet
strontium isotope
Title Larger benthic foraminifera and strontium isotope stratigraphy of the Palaeocene limestones in the Guru area, south Xizang (Tibet): An attempt to build a high-resolution biozonation for the eastern Neo-Tethys
URI https://dx.doi.org/10.1016/j.palwor.2024.200903
Volume 34
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