oa Comparing Changes in Function and Structure Between the Golan and Other Marine Ecosystems Following the Kpg Mass Extinction

References

1. de Oca, C.S.M., Rodrigo-Gámiz, M., Martínez-Ruiz, F., Rodríguez-Tovar, F.J., Castro, J.M., Quijano, M.L. and Pancost, R.D., 2021. Minor changes in biomarker assemblages in the aftermath of the Cretaceous-Paleogene mass extinction event at the Agost distal section (Spain).Palaeogeography, Palaeoclimatology, Palaeoecology, 569, p.110310.
   [Google Scholar]
2. Hull, P.M. and Norris, R.D., 2011. Diverse patterns of ocean export productivity change across the Cretaceous‐Paleogene boundary: New insights from biogenic barium.Paleoceanography, 26(3).
   [Google Scholar]
3. Hull, P.M. and Darroch, S.A., 2013. Mass extinctions and the structure and function of ecosystems.The Paleontological Society Papers, 19, pp.115–156.
   [Google Scholar]
4. Rosenberg, Y.O., Ashckenazi-Polivoda, S., Abramovich, S., Thibault, N., Chin, S., Feinstein, S., Bartov, Y. and Amrani, A., 2021. Resilience of primary and export productivity in a eutrophic ecosystem following the Cretaceous-Paleogene mass extinction.Global and Planetary Change, 196, p.103371.
   [Google Scholar]
5. Sepúlveda, J., Wendler, J.E., Summons, R.E. and Hinrichs, K.U., 2009. Rapid resurgence of marine productivity after the Cretaceous-Paleogene mass extinction.Science, 326(5949), pp.129–132.
   [Google Scholar]
6. Sepúlveda, J., Alegret, L., Thomas, E., Haddad, E., Cao, C. and Summons, R.E., 2019. Stable isotope constraints on marine productivity across the Cretaceous‐Paleogene mass extinction.Paleoceanography and Paleoclimatology, 34(7), pp.1195–1217.
   [Google Scholar]