22.
VELLEKOOP J., SMIT J., VAN DE SCHOOTBRUGGE B., WEIJERS J.W.H., GALEOTTI S., SINNINGHE DAMSTÉ J.S. & BRINKHUIS H. 2015. Palynological evidence for prolonged cooling along the Tunisian continental shelf following the K–Pg boundary impact. Palaeogeogr., Palaeoclimatol., Palaeoecol., 426: 216–228.