Calc alkaline volcanism-aided phytoplankton growth and organic matter production of the Cenomanian-Turonian Eagle Ford Formation of South Texas.

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Title: Calc alkaline volcanism-aided phytoplankton growth and organic matter production of the Cenomanian-Turonian Eagle Ford Formation of South Texas.
Authors: Chakrabarty, Puloma1,2,3 (AUTHOR) pulomac@g.ucla.edu, Basu, Asish R.1 (AUTHOR)
Source: International Geology Review. May2026, Vol. 68 Issue 10, p1185-1206. 22p.
Subject Terms: *Phytoplankton, *Volcanism, *Organic compounds, *Geological time scales, *Anoxic waters, *Black shales
Geographic Terms: Texas
Abstract: The kerogen-rich Eagle Ford (EF) black shales of south Texas formed in the Late Cretaceous, overlapping the Cenomanian-Turonian (C-T) boundary and the Oceanic Anoxic Event 2 (OAE2). This study proposes a continuous calc-alkaline volcanogenic model of oil-generation for the EF by petrographic, geochemical, and geochronological studies of sub-surface and surface EF shale cores. Biotite, alkali feldspar phenocrysts, andesitic rock fragments and swelling clays observed, and X-ray diffraction (XRD) analyses of bulk samples indicate continuous volcanism during EF deposition. Zircons yield U-Pb ages of 93.2 ± 1.66 Ma, 94.13 ± 1.25 Ma and 93.7 ± 1.9 Ma, consistent with the C-T age of deposition. The εHf(i) of zircons averaged at +1.23, indicating a crustal component in the arc volcanism. In the 187Os/188Osinitial at 93 Ma, the time of EF deposition is 2.47–5.11 indicating a continental-crustal origin of the osmium (Os). Continuous arc volcanism during the EF deposition of volcanic-silicic sediments and carbonates was simultaneously a part of the Cretaceous global continental arc flare-ups, responsible for greenhouse conditions and anoxia during black shales deposition. We conclude that the black shale of the EF is dominated by lamalginites (unicellular solitary or colonial phytoplankton), produced during algal blooms falling as 'marine snow' augmented by calc-alkaline volcanism at the C-T boundary. [ABSTRACT FROM AUTHOR]
Database: Energy & Power Source
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An: 193598879
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  Label: Title
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  Data: Calc alkaline volcanism-aided phytoplankton growth and organic matter production of the Cenomanian-Turonian Eagle Ford Formation of South Texas.
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  Data: <searchLink fieldCode="AR" term="%22Chakrabarty%2C+Puloma%22">Chakrabarty, Puloma</searchLink><relatesTo>1,2,3</relatesTo> (AUTHOR)<i> pulomac@g.ucla.edu</i><br /><searchLink fieldCode="AR" term="%22Basu%2C+Asish+R%2E%22">Basu, Asish R.</searchLink><relatesTo>1</relatesTo> (AUTHOR)
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  Data: <searchLink fieldCode="JN" term="%22International+Geology+Review%22">International Geology Review</searchLink>. May2026, Vol. 68 Issue 10, p1185-1206. 22p.
– Name: Subject
  Label: Subject Terms
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  Data: *<searchLink fieldCode="DE" term="%22Phytoplankton%22">Phytoplankton</searchLink><br />*<searchLink fieldCode="DE" term="%22Volcanism%22">Volcanism</searchLink><br />*<searchLink fieldCode="DE" term="%22Organic+compounds%22">Organic compounds</searchLink><br />*<searchLink fieldCode="DE" term="%22Geological+time+scales%22">Geological time scales</searchLink><br />*<searchLink fieldCode="DE" term="%22Anoxic+waters%22">Anoxic waters</searchLink><br />*<searchLink fieldCode="DE" term="%22Black+shales%22">Black shales</searchLink>
– Name: SubjectGeographic
  Label: Geographic Terms
  Group: Su
  Data: <searchLink fieldCode="DE" term="%22Texas%22">Texas</searchLink>
– Name: Abstract
  Label: Abstract
  Group: Ab
  Data: The kerogen-rich Eagle Ford (EF) black shales of south Texas formed in the Late Cretaceous, overlapping the Cenomanian-Turonian (C-T) boundary and the Oceanic Anoxic Event 2 (OAE2). This study proposes a continuous calc-alkaline volcanogenic model of oil-generation for the EF by petrographic, geochemical, and geochronological studies of sub-surface and surface EF shale cores. Biotite, alkali feldspar phenocrysts, andesitic rock fragments and swelling clays observed, and X-ray diffraction (XRD) analyses of bulk samples indicate continuous volcanism during EF deposition. Zircons yield U-Pb ages of 93.2 ± 1.66 Ma, 94.13 ± 1.25 Ma and 93.7 ± 1.9 Ma, consistent with the C-T age of deposition. The εHf(i) of zircons averaged at +1.23, indicating a crustal component in the arc volcanism. In the 187Os/188Osinitial at 93 Ma, the time of EF deposition is 2.47–5.11 indicating a continental-crustal origin of the osmium (Os). Continuous arc volcanism during the EF deposition of volcanic-silicic sediments and carbonates was simultaneously a part of the Cretaceous global continental arc flare-ups, responsible for greenhouse conditions and anoxia during black shales deposition. We conclude that the black shale of the EF is dominated by lamalginites (unicellular solitary or colonial phytoplankton), produced during algal blooms falling as 'marine snow' augmented by calc-alkaline volcanism at the C-T boundary. [ABSTRACT FROM AUTHOR]
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RecordInfo BibRecord:
  BibEntity:
    Identifiers:
      – Type: doi
        Value: 10.1080/00206814.2026.2627317
    Languages:
      – Code: eng
        Text: English
    PhysicalDescription:
      Pagination:
        PageCount: 22
        StartPage: 1185
    Subjects:
      – SubjectFull: Phytoplankton
        Type: general
      – SubjectFull: Volcanism
        Type: general
      – SubjectFull: Organic compounds
        Type: general
      – SubjectFull: Geological time scales
        Type: general
      – SubjectFull: Anoxic waters
        Type: general
      – SubjectFull: Black shales
        Type: general
      – SubjectFull: Texas
        Type: general
    Titles:
      – TitleFull: Calc alkaline volcanism-aided phytoplankton growth and organic matter production of the Cenomanian-Turonian Eagle Ford Formation of South Texas.
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            NameFull: Chakrabarty, Puloma
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            NameFull: Basu, Asish R.
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            – D: 15
              M: 05
              Text: May2026
              Type: published
              Y: 2026
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              Value: 68
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              Value: 10
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            – TitleFull: International Geology Review
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