4.5 Editorial Material

Evolution of the Geological Environment and Exploration for Life on Mars

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Evaluation of small-sized mounds formation mechanisms in China's Zhurong landing region

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Summary: This study identified a special type of small-sized mounds and pits in the Zhurong landing region using high-resolution images acquired by the Tianwen-1 orbiter. The mounds are likely to be lava domes, while the pits may have been formed through the sublimation of subsurface volatiles.

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Recent Aqueous Activity on Mars Evidenced by Transverse Aeolian Ridges in the Zhurong Exploration Region of Utopia Planitia

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Summary: In this study, using data from China's Zhurong rover and high-resolution remote sensing, the researchers investigated transverse aeolian ridges in the Zhurong landing region of Utopia Planitia on Mars. They proposed a two-stage evolutionary scenario for the ridges and identified polygonal features with hydrated minerals on their surface for the first time. The study discusses possible formation mechanisms for these features and suggests they may be linked to recent aqueous activity and atmosphere-surface water exchange on Mars, providing insights into the hydrological cycle of Mars in its current cold and dry climate.

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Evolution History of Mesas in the Southern Utopia Planitia and Implications for the Ancient Oceans on Mars

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Evidence for marine sedimentary rocks in Utopia Planitia: Zhurong rover observations

Long Xiao et al.

Summary: Decades of research using remotely sensed data have provided evidence for the presence of an ocean on Mars in the northern lowlands, but controversy remained due to the lack of in situ analysis. The Tianwen-1/Zhurong rover, located near the Vastitas Borealis Formation (VBF), has conducted in situ analysis revealing sedimentary structures and features that support the existence of an ancient ocean on Mars.

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Modern water at low latitudes on Mars: Potential evidence from dune surfaces

Xiaoguang Qin et al.

Summary: Landforms on the Martian surface provide valuable insights into past surface processes, but the modern hydroclimatic conditions on Mars are still not well understood. This study reports the discovery of various surface features on salt-rich dunes in southern Utopia Planitia, suggesting the involvement of saline water from thawed frost/snow as the most likely cause. The findings shed light on the more humid conditions of the modern Martian climate and have important implications for future exploration missions searching for signs of extant life.

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An explosive mud volcano origin for the pitted cones in southern Utopia Planitia, Mars

Le Wang et al.

Summary: Pitted cones on the surface of Mars are cone-shaped structures with summit depressions, and they have various origins. In this study, pitted cones near the Zhurong rover's landing site in southern Utopia Planitia were investigated using recent images and digital elevation models. The results suggest that these pitted cones have morphological characteristics of explosive mud volcanoes. Future in-situ observations are expected to provide more insights into the sediments of the putative northern ocean and the Martian subsurface during the formation of pitted cones.

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An arid-semiarid climate during the Noachian-Hesperian transition in the Huygens region, Mars: Evidence from morphological studies of valley networks

Yutong Shi et al.

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Geomorphic contexts and science focus of the Zhurong landing site on Mars

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Summary: As part of the Tianwen-1 mission, the Zhurong rover successfully landed in southern Utopia Planitia, conducting in situ investigation to study the characteristics and evolution of the ancient Martian environment.

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Zhurong reveals recent aqueous activities in Utopia Planitia, Mars

Yang Liu et al.

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Layered subsurface in Utopia Basin of Mars revealed by Zhurong rover radar

Chao Li et al.

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Geological diversity and microbiological potential of lakes on Mars

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Chemical weathering over hundreds of millions of years of greenhouse conditions on Mars

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Geological Characteristics and Targets of High Scientific Interest in the Zhurong Landing Region on Mars

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