An interglacial period existed between the Sturtian (ca. 720∼ 660 Ma) and the Marinoan
glacial period (ca. 650∼ 635 Ma) in the Cryogenian. It is manifested as the Mn-bearing …

Abstract The Cryogenian interglaciation (ca. 660 Ma to 650 Ma) was an interlude between
the Sturtian glaciation (ca. 717 Ma to 660 Ma) and Marinoan glaciation (ca. 650 Ma to 635 …

Although extremely high Hg contents are known in the Lower Cambrian sedimentary
successions, the extent and spatial–temporal distribution of sedimentary Hg anomalies in …

An ice-free greenhouse interval (ca. 660∼ 650 Ma) occurred between the global Sturtian
(ca. 717 Ma∼ 660 Ma) and Marinoan glaciation (ca. 650 Ma∼ 635 Ma) during the …

Mercury (Hg) enrichment in stratigraphic successions is now widely used as a proxy for
volcanic inputs, often for the purpose of documenting a relationship between large igneous …

Ordovician-Silurian transition (OST) sections of South China contain extremely high mercury
(Hg) concentrations (> 1000 ppb) of uncertain provenance. The main hypotheses …

Abstract This study provides a 16.2-kyr record of mercury (Hg) deposition derived from a
lacustrine sedimentary sequence in Dahu Swamp, eastern Nanling Mountains. Results …

The widespread lower Cambrian black shales reflect a significant anoxic event during a
global transgression, recording synergistic changes in the marine environment and …

Abstract The Cryogenian-Ediacaran transition represents a pivotal geological period in the
evolution of global climate, ocean chemistry, and early organisms. The transition is …

There are differences in the response of long-term mercury (Hg) deposition to climate
change, so it is necessary to clarify the influencing factors of Hg deposition in different …