15. BASE OF LARGE GEPHYROCAPSA AND ASTRONOMICAL CALIBRATION OF EARLY PLEISTOCENE SAPROPELS IN SITE 967 AND HOLE 969D: SOLVING THE CHRONOLOGY OF THE VRICA SECTION (CALABRIA, ITALY) 1
15. BASE OF LARGE GEPHYROCAPSA AND ASTRONOMICAL CALIBRATION OF EARLY PLEISTOCENE SAPROPELS IN SITE 967 AND HOLE 969D: SOLVING THE CHRONOLOGY OF THE VRICA SECTION (CALABRIA, ITALY) 1
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发表时间：
1998
期刊：
影响因子：
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通讯作者：
L. Lourens;F. Hilgen;I. Raffi
中科院分区：
文献类型：
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作者：
L. Lourens;F. Hilgen;I. Raffi
海洋钻探计划 (ODP) 967 号站点和 969D 孔中更新世早期钙质浮游生物生物年代学和腐泥的天文校准，旨在解决意大利弗里卡上新世/更新世边界层型剖面中现有的年代学问题。这些 ODP 地点与 Vrica 和 Singa 剖面之间详细的腐泥相关性，经钙质浮游生物生物地层学证实，表明 Vrica 剖面是连续的，并且大型 Gephyrocapsa 的底部在全球范围内是历时的。
Calcareous plankton biochronology and the astronomical calibration of sapropels are presented for the early Pleistocene in Ocean Drilling Program (ODP) Site 967 and Hole 969D with the aim to solve the existing chronology problem in the Pliocene/ Pleistocene boundary stratotype section of Vrica, Italy. Detailed sapropel correlations between these ODP sites and the Vrica and Singa sections, corroborated by calcareous plankton biostratigraphy, indicate that the Vrica section is continuous and that the base of the large Gephyrocapsa is diachronous on a global scale.