@article{236,
  author = {G. Lu and G. Keller},
  title = {Planktic foraminiferal faunal turnovers in the subtropical Pacific during the late Paleocene to early Eocene},
  abstract = {<p>Planktic foraminiferal analysis of sedimentary samples at 25-cm intervals (81 k.y.) at DSDP Site 577 provides a high resolution data base for deep-sea biostratigraphy and faunal changes during the late Paleocene to early Eocene. There are three major faunal turnovers, each of which occurred over a time period of 200 to 400 k.y., near the P3a/P3b, P6a/P6b and PSIP9 boundaries. These turnovers are characterized by rapid changes in species richness, large numbers of first and last appearances, and significant changes in the relative abundances of species. A chronological sequence of datum levels and faunal events of foraminifera tied to magnetostratigraphy provides biostratigraphic control at 1 m.y. intervals for the late Paleocene to early Eocene, with faunal and isotopic events near the PaleoceneiEocene boundary providing isochronous stratigraphic markers.\&nbsp; \&nbsp;<a href="https://geoweb.princeton.edu/research/keller/pubs/Lu-1995-JForamR.pdf" target="_blank">PDF</a></p>
},
  year = {1995},
  journal = {The Journal of Foraminiferal Research},
  volume = {25},
  pages = {97{\textendash}116},
  month = {apr},
  url = {https://doi.org/10.2113/gsjfr.25.2.97},
  doi = {10.2113/gsjfr.25.2.97},
  language = {eng},
}