<html><head><meta http-equiv="content-type" content="text/html; charset=utf-8"></head><body dir="auto"><div dir="ltr">Hi,<div style="word-wrap: break-word; -webkit-nbsp-mode: space; line-break: after-white-space;" class=""><div class=""><br class=""></div><div class="">Does anyone have a pdf of this paper? <div class=""><div class=""><span style="font-family: Geneva, Tahoma, sans-serif; font-size: 10.199999809265137px; text-indent: -40.79999923706055px; background-color: rgb(255, 255, 255);" class=""><br class=""></span></div><div class=""><span style="font-family: Geneva, Tahoma, sans-serif; font-size: 10.199999809265137px; text-indent: -40.79999923706055px; background-color: rgb(255, 255, 255);" class="">Shamrai, I. A. (1963). Nekotorye formy verkhnemelovykh i paleogenovykh kokkolitov i disko_asterov na yuge russkol platformy [Certain forms of Upper Cretaceous and Paleogene coccoliths and discoasters from the southern Russian Platform]. </span><i style="font-family: Geneva, Tahoma, sans-serif; font-size: 10.199999809265137px; text-indent: -40.79999923706055px;" class="">Izvestiya Vysshikh Uchebnykh Zavedeniy Geologiya i Razvedka. </i><span style="font-family: Geneva, Tahoma, sans-serif; font-size: 10.199999809265137px; text-indent: -40.79999923706055px; background-color: rgb(255, 255, 255);" class=""></span><b style="font-family: Geneva, Tahoma, sans-serif; font-size: 10.199999809265137px; text-indent: -40.79999923706055px;" class="">6</b><span style="font-family: Geneva, Tahoma, sans-serif; font-size: 10.199999809265137px; text-indent: -40.79999923706055px; background-color: rgb(255, 255, 255);" class="">(4): 27-40</span></div></div></div><div class=""><span style="font-family: Geneva, Tahoma, sans-serif; font-size: 10.199999809265137px; text-indent: -40.79999923706055px; background-color: rgb(255, 255, 255);" class=""><br class=""></span></div><div class="">Thanks,</div><div class=""><br class=""></div><div class="">Richard</div></div></div><br><br><div dir="ltr">Sent from my iPhone</div></body></html>