Original paper
Integrated Neogene biochemostratigraphy at DSDP Site 296 on the Kyushu–Palau Ridge in the western North Pacific
Matsui, Hiroki; Horikawa, Keiji; Chiyonobu, Shun; Itaki, Takuya; Ikehara, Minoru; Kawagata, Shungo; Wakaki-Uchimura, Hitomi; Asahara, Yoshihiro; Seki, Osamu; Okazaki, Yusuke
Newsletters on Stratigraphy Volume 53 Number 3 (2020), p. 313 - 331
published: Jun 15, 2020
published online: Sep 20, 2019
manuscript accepted: Jul 26, 2019
manuscript revision received: Jul 22, 2019
manuscript revision requested: Jun 29, 2019
manuscript received: May 24, 2019
ArtNo. ESP026005303003, Price: 29.00 €
Abstract
We revisited the stratigraphy at Deep Sea Drilling Project (DSDP) Site 296, which has promise as a reference sequence for the mid-latitude western North Pacific. We constructed the biostratigraphy (calcareous nannofossils, planktic foraminifera, and radiolaria) and chemostratigraphy (strontium isotope ratios, and stable oxygen and carbon isotope ratios) to reveal continuous sedimentation at Site 296 through the past 20 million years (Myr). The biostratigraphy of calcareous nannofossils comprised 27 biohorizons from biozones NN2 to NN21 (early Miocene to Pleistocene), which are consistent with the biohorizons of planktic foraminifera and radiolaria. The uninterrupted sedimentation throughout the past 20 Myr was further supported by strontium isotope stratigraphy aligned to nannofossil datums and by correlation of stable isotope data from benthic foraminifera with an isotopic compilation from the Pacific Ocean. The refined age–depth model showed low sedimentation rates (<2 cm/kyr) through most of the Miocene and higher sedimentation rates (2–4 cm/kyr) during the Plio–Pleistocene, and potentially identified the “biogenic bloom” event from the late Miocene to early Pliocene. The continuity of sedimentation through the middle Miocene contrasts with the shipboard biostratigraphy, which inferred a hiatus (erosion or non-deposition) during the middle Miocene. Thus, the revised stratigraphy at Site 296 provides a key to correlation with other deep-sea sites in the North Pacific. Our revised age–depth model provides a framework for future studies of important climatic events during the Miocene, including the Miocene Climatic Optimum, the middle Miocene Climatic Transition, and the late Miocene global cooling under the influence of the past Kuroshio Current.
Keywords
DSDP Site 296 • western North Pacific • Miocene • biostratigraphy • chemostratigraphy