Chemostratigraphy of the Jurassic System: applications, limitations and implications for palaeoceanography
Current chemostratigraphical studies of the Jurassic System primarily involve the use of one sedimentary component (marine organic carbon), one divalent transition metal substituted in carbonate (manganese), and two isotopic tracers: strontium-isotope ratios ( Sr/...
Váldodahkkit: | Jenkyns, H, Jones, C, Grocke, DR, Hesselbo, S, Parkinson, D |
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Materiálatiipa: | Journal article |
Almmustuhtton: |
2002
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Geahča maid
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Chemostratigraphy of the Jurassic System: Applications, limitations and implications for palaeoceanography
Dahkki: Jenkyns, H, et al.
Almmustuhtton: (2002) -
Chemostratigraphy of the Jurassic System: applications, limitations and implications for palaeoceanography
Almmustuhtton: (2002) -
Nitrogen isotope evidence for water mass denitrification during the early Toarcian (Jurassic) oceanic anoxic event
Dahkki: Jenkyns, H, et al.
Almmustuhtton: (2001) -
PALAEOCEANOGRAPHY OF MESOZOIC RIBBON RADIOLARITES
Dahkki: Jenkyns, H, et al.
Almmustuhtton: (1982) -
Molybdenum-isotope chemostratigraphy and paleoceanography of the Toarcian Oceanic Anoxic Event (Early Jurassic)
Dahkki: Dickson, A, et al.
Almmustuhtton: (2017)