This study was supported by the National Key RD the National Natural Science Foundation of China (NSFC 41430962); the NSFC-Shandong Joint Fund for Marine Science Research Centers (U1606401); the National Program on Global Change and Air-Sea Interaction (GASI-GEOGE-03); the Australia-New Zealand International Ocean Discovery Program Consortium (ANZIC), which provided Legacy/Special Analytical Funding (ANZIC is supported by the Australian government through the Australian Research Council's LIEF funding scheme [LE140100047], the Australian and New Zealand consortium of universities and government agencies); and the Ocean Drilling Program, which was sponsored by the U.S. National Science Foundation (NSF) and participating countries under management of Joint Oceanographic Institutions (JOI), Inc.

中文翻译：

---

自 4.0 Ma 以来北太平洋沉积物中记录的增强风尘通量的机制：亚洲内部尘源区的干旱或湿度？

本研究得到国家重点研发、国家自然科学基金（NSFC 41430962）的支持；国家自然科学基金-山东省海洋科学研究中心联合基金（U1606401）；全球变化和海空相互作用国家计划（GASI-GEOGE-03）；澳大利亚-新西兰国际海洋发现计划联盟 (ANZIC)，该联盟提供遗产/特别分析资金​​（ANZIC 由澳大利亚政府通过澳大利亚研究委员会的 LIEF 资助计划 [LE140100047]、澳大利亚和新西兰大学联盟和政府机构）; 以及由美国国家科学基金会 (NSF) 和联合海洋研究所 (JOI), Inc. 管理的参与国赞助的海洋钻探计划。