Testing the limits of Paleozoic chronostratigraphic correlation via high-resolution (<500 k.y.) integrated conodont, graptolite, and carbon isotope (δ¹³Ccarb) biochemostratigraphy across the Llandovery–Wenlock (Silurian) boundary: is a unified Phanerozoic time scale achievable?

Bradley D. Cramer, David Loydell, Christian Samtleben, Axel Munnecke, Dimitri Kaljo, Peep Mannik, Tonu Martma, Lennart Jeppsson, Mark A. Kleffner, James E. Barrick, Craig A. Johnson, Poul Emsbo, Michael M. Joachimski, Torsten Bickert, Matthew R. Saltzman

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Testing the limits of Paleozoic chronostratigraphic correlation via high-resolution (<500 k.y.) integrated conodont, graptolite, and carbon isotope (δ¹³Ccarb) biochemostratigraphy across the Llandovery–Wenlock (Silurian) boundary: is a unified Phanerozoic time scale achievable?

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Earth and Planetary Sciences

INIS

Testing the limits of Paleozoic chronostratigraphic correlation via high-resolution (<500 k.y.) integrated conodont, graptolite, and carbon isotope (δ13Ccarb) biochemostratigraphy across the Llandovery–Wenlock (Silurian) boundary: is a unified Phanerozoic time scale achievable?

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Earth and Planetary Sciences

INIS

Testing the limits of Paleozoic chronostratigraphic correlation via high-resolution (<500 k.y.) integrated conodont, graptolite, and carbon isotope (δ¹³Ccarb) biochemostratigraphy across the Llandovery–Wenlock (Silurian) boundary: is a unified Phanerozoic time scale achievable?