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Global comparative basin hypsometric analysis of Earth and Mars: Implications for early Mars climate
DOI: 10.1016/j.epsl.2025.119226 Bibcode: 2025E&PSL.65319226F

Fang, J.; Luo, W.; Howard, A. D. +3 more

While there is a consensus that water played at least some role in the formation of various Martian landforms, including valley networks (VNs), the specific mechanisms and climate conditions are still debated. Basin hypsometric curves, reflecting elevation distributions, offer insights into past processes and climates. Our study presents a global-…

2025 Earth and Planetary Science Letters
MEx 0
The hydrology of the Jezero crater paleolake: Implications for the climate and limnology of the lake system from hydrological modeling
DOI: 10.1016/j.epsl.2024.118690 Bibcode: 2024E&PSL.63518690H

Horvath, David G.; Andrews-Hanna, Jeffrey C.

The lake stages in Jezero are consistent with semiarid climates The Jezero lake was a throughflow lake driven by significant surface runoff Hydrological conditions do not favor large-scale evaporite deposition Similar climates at Jezero and Gale produce contrasting lacustrine environments

2024 Earth and Planetary Science Letters
MEx 1
Periodic Bedrock Ridges at Oxia Planum and Chryse Planitia, Mars: Evidence for widespread aeolian erosion of an ancient surface by regional paleowinds
DOI: 10.1016/j.epsl.2023.118522 Bibcode: 2024E&PSL.62618522F

Fawdon, Peter; Grindrod, Peter M.; Balme, Matthew R. +4 more

Periodic Bedrock Ridges (PBRs) are repeating, symmetrical, wind-transverse, bedrock-abraded linear ridges that occur on Mars as parallel sets. Here, we extend our previous survey of PBRs at Oxia Planum - the landing site of ESA's ExoMars Rosalind Franklin rover - to include three additional sites along the margins of the circum-Chryse basin to und…

2024 Earth and Planetary Science Letters
ExoMars-16 MEx 1
The evolution of Martian fissure eruptions and their plumbing systems
DOI: 10.1016/j.epsl.2023.118382 Bibcode: 2023E&PSL.62118382P

Pieterek, Bartosz; Jones, Thomas J.

On Earth, the investigation of fissure eruptions and their deposits provide fundamental insights into the evolution of the subsurface volcanic plumbing system. On Mars, we have limited evidence of the spatiotemporal evolution of fissure-fed volcanic systems, and thus the processes operating within their subsurface-feeding dykes remain poorly under…

2023 Earth and Planetary Science Letters
MEx 3
Assessing the role of clay and salts on the origin of MARSIS basal bright reflections
DOI: 10.1016/j.epsl.2022.117370 Bibcode: 2022E&PSL.57917370M

Orosei, Roberto; Caprarelli, Graziella; Pettinelli, Elena +7 more

Anomalously bright basal reflections detected by MARSIS at Ultimi Scopuli have been interpreted to indicate the presence of water-saturated materials or ponded liquid water at the base of the South Polar Layered Deposits (SPLD). Because conventional models assume basal temperatures (≤200 K) much lower than the melting point of water, this interpre…

2022 Earth and Planetary Science Letters
MEx 13
Aeolian disruption and reworking of TARs at the Zhurong rover field site, southern Utopia Planitia, Mars
DOI: 10.1016/j.epsl.2022.117785 Bibcode: 2022E&PSL.59517785L

Lu, Yu; Wu, Bo; Edgett, Kenneth S. +6 more

China's Zhurong rover explored four crescent-shaped TARs during the first 107 sols. The crust formed by accumulation and induration of aeolian dust makes TARs light-toned in orbiter images. Two TARs degraded into smaller megaripples due to a change of wind regime. TARs might share similar formation and evolution mechanisms with megaripples.

2022 Earth and Planetary Science Letters
MEx 9
Has the impact flux of small and large asteroids varied through time on Mars, the Earth and the Moon?
DOI: 10.1016/j.epsl.2021.117362 Bibcode: 2022E&PSL.57917362L

Benedix, Gretchen K.; Lagain, Anthony; Kreslavsky, Mikhail +6 more

The impact flux over the last 3 Ga in the inner Solar System is commonly assumed to be constant through time due to insufficient data to warrant a different choice for this range of time. However, asteroid break-up events in the main belt may have been responsible for cratering spikes over the last ∼2 Ga on the Earth-Moon system. Due to its proxim…

2022 Earth and Planetary Science Letters
MEx 8
Insights into the subsurface structure of wrinkle ridges on Mars
DOI: 10.1016/j.epsl.2022.117759 Bibcode: 2022E&PSL.59517759K

Karagoz, Oguzcan; Kenkmann, Thomas; Wulf, Gerwin

Wrinkle ridges are important landforms on Mars and other planetary bodies and result from horizontal tectonic shortening. This study provides insights into the subsurface of selected wrinkle ridge sites, based on exposures provided by steep escarpments and crater slopes that crosscut wrinkle ridges. We mapped the complex fold and fault patterns an…

2022 Earth and Planetary Science Letters
MEx 4
Did Martian valley networks substantially modify the landscape?
DOI: 10.1016/j.epsl.2020.116482 Bibcode: 2020E&PSL.54716482G

Grau Galofre, Anna; Jellinek, A. Mark; Bahia, Rickbir Singh +2 more

Valley networks are ancient drainage systems incised on the southern hemisphere of Mars, and stand as evidence that liquid water once sculpted its surface. The duration of valley network activity and the sources of water are key questions in deciphering the timing of water stability on early Mars, but remain poorly constrained. In this study we ad…

2020 Earth and Planetary Science Letters
MEx 9
Martian fan deposits: Insights on depositional processes and origin from mass balance survey
DOI: 10.1016/j.epsl.2019.116049 Bibcode: 2020E&PSL.53316049V

Hynek, Brian M.; Williams, Rebecca M. E.; Di Achille, Gaetano +2 more

Fan deposits located at the mouths of Martian valleys have been interpreted as indicators of wet conditions during Mars history. However, the processes, time and amount of water needed to carve the valleys and form the fans are still debated. Here we present a detailed morphometric and mass balance analysis of valleys and fan-shaped deposits using…

2020 Earth and Planetary Science Letters
MEx 2