H Zhuo, Y Wang, H Shi, M He, W Chen, H Li… - Quaternary Science …, 2015 - Elsevier
Multiple successions of buried fluvial channel systems were identified in the Quaternary section of the mid-shelf region of the northern South China Sea, providing a new case study …
MA Mauffrey, R Urgeles, S Berné, J Canning - Quaternary Science Reviews, 2017 - Elsevier
Abstract After the Messinian Salinity Crisis (MSC), the Ebro Margin, like other Mediterranean deltaic margins, rebuilt through progradation and increasingly significant aggradation. The …
Sediments from the continental shelf/coastal region bear significant signals of sea-level, climate change as well as local tectonic information. This study presents a high-resolution …
J Liu, X Shi, Q Liu, S Ge, Y Liu, Z Yao… - Journal of …, 2014 - Wiley Online Library
Sediments from the continental shelf are sensitive to sea level, climatic changes, and local tectonic history. In this study, we carried out a high‐resolution magnetostratigraphic …
X Li, J Ge, X Zhao, K Qi, BG Jones, X Fang - Marine Geology, 2024 - Elsevier
The Quaternary sediments in the northwestern South China Sea (NW-SCS) provide valuable information about provenance, climate and sea level changes. However, the …
L Yi - Global and Planetary Change, 2023 - Elsevier
Antarctic bottom water production is one of the most important components in oceanic circulation, yet its long-term impact on Earth's climate remains poorly known. In this study …
MA Louvari, H Drinia, G Kontakiotis, L Di Bella… - Journal of Marine …, 2019 - Elsevier
A high-resolution palaeoenvironmental investigation was conducted on the benthic foraminiferal record of two continuous sediment cores (DEH 5, DEH 1) in order to reconstruct …
Abstract The South Evoikos Basin is a marginal basin in the Aegean Sea which receives little terrigenous supply and its sedimentation is dominated by hemipelagic processes. Late …
Sites of ice-stream discharge to the continental slope build trough-mouth fans from glacigenic debris flows (GDFs), subglacial meltwater flows, and suspended sediment. Thus …