@article{239,
  author = {Gerta Keller and Wolfgang Stinnesbeck},
  title = {Near-K/T age of clastic deposits from Texas to Brazil: impact, volcanism and/or sea-level lowstand?},
  abstract = {<p>Near-K/T boundary clastic deposits from Texas, Mexico, Haiti, Guatemala and Brazil, often described as impact-generated tsunami deposits, are stratigraphically below well-defined K/T boundary horizons and appear not to be causally related to the K/T boundary event. Stratigraphic evidence indicates that their deposition began during the last 170{\textendash}200 kyr of the Maastrichtian, coincident with a major eustatic sea-level lowstand that lowered sea level by as much as 70{\textendash}100 m. Clastic deposition ended a few tens of thousands of years before the K/T boundary during a rapidly rising sea level. The presence of glass in clastic deposits in Haiti, northeastern Mexico and Yucatan suggests that the sea-level lowstand coincided with a time of major volcanism or pre-K/T boundary bolide impact.\&nbsp; <a href="https://geoweb.princeton.edu/research/keller/pubs/Keller_et_al-1996-Terra_Nova.pdf" target="_blank">PDF</a></p>
},
  year = {1996},
  journal = {Terra Nova},
  volume = {8},
  pages = {277{\textendash}285},
  month = {may},
  url = {https://doi.org/10.1111/j.1365-3121.1996.tb00757.x},
  doi = {10.1111/j.1365-3121.1996.tb00757.x},
  language = {eng},
}