@article{9,
  author = {Norman MacLeod and Gerta Keller},
  title = {Hiatus distributions and mass extinctions at the Cretaceous/Tertiary boundary},
  abstract = {<p>Much disagreement over the interpretation of data bearing on various Cretaceous/Tertiary (K/T) extinction scenarios results from a failure to view these data within their appropriate stratigraphic context. Combined biostratigraphic and chronostratigraphic analyses of K/T boundary sequences have revealed systematic differences in patterns of sediment accumulation within continental-shelf and deep-sea depositional settings. Although virtually all deep-sea boundary sequences are marked by intervals of nondeposition or hiatus formation during the latest Cretaceous and earliest Tertiary, many continental shelf-slope sequences appear to be temporally complete over this same interval. This differential pattern of sediment accumulation can be related to the latest Maastrichtian-earliest Danian sea-level rise, during which deep-sea sediment- accumulation rates would be expected to drop as the locus of sediment deposition migrated across the continental shelf. Our data suggest that the abrupt shifts in carbon-isotope abundances, single-peak Ir anomalies, and apparently instantaneous mass extinctions of marine plankton{\textemdash}which are routinely reported from deep-sea K/T boundary sequences and used to support a causal relation between Late Cretaceous bolide impacts and K/T mass extinctions{\textemdash}may be artifacts of a temporally incomplete (or extremely condensed) deep-sea stratigraphic record.\&nbsp; <a href="https://geoweb.princeton.edu/research/keller/pubs/MacLoed_Keller_1991_GSApubs.pdf" target="_blank">PDF</a></p>
},
  year = {1991},
  journal = {Geology},
  volume = {19},
  pages = {497-501},
  url = {http://geology.gsapubs.org/content/19/5/497.abstract},
  doi = {10.1130/0091-7613(1991)019<0497:HDAMEA>2.3.CO;2},
  language = {eng},
}