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Ślady starożytnego oceanu odkryte na Marsie – oznacza to „wyższy potencjał życia”

Skompilowany z 28 zdjęć, ten widok został wykonany z sondy NASA Curiosity Mars po tym, jak łazik wspiął się na strome zbocze struktury geologicznej zwanej „Greenhue Pied”. W oddali powyżej obrazu widać dno krateru Gale, w pobliżu obszaru zwanego Aeolis Dorsa, który według badaczy był kiedyś ogromnym oceanem. Źródło: NASA/JPL-Caltech/MSSS

Nowe dowody na starożytny Ocean Północny w[{” attribute=””>Mars has been uncovered in a recently released set of topography maps. These maps offer the strongest case yet that the planet once experienced sea-level rise consistent with an extended warm and wet climate, which was far different than the harsh, frozen landscape that exists today.

“What immediately comes to mind as one the most significant points here is that the existence of an ocean of this size means a higher potential for life,” said Benjamin Cardenas, assistant professor of geosciences at Penn State and lead author on the study recently published in the Journal of Geophysical Research: Planets. “It also tells us about the ancient climate and its evolution. Based on these findings, we know there had to have been a period when it was warm enough and the atmosphere was thick enough to support this much liquid water at one time.”

Whether Mars had an ocean in its low-elevation northern hemisphere has long been debated in the scientific community, Cardenas explained. Using topography data, the research team was able to show definitive evidence of a roughly 3.5-billion-year-old shoreline with substantial sedimentary accumulation, at least 900 meters (3,000 feet) thick, that covered hundreds of thousands of square kilometers.

Niedawno wydany zestaw map topograficznych dostarcza nowych dowodów na istnienie starożytnego północnego oceanu na Marsie. Mapy są jak dotąd najsilniejszym argumentem, mówi Benjamin Cardenas, profesor nadzwyczajny nauk o Ziemi w Penn State, że planeta kiedyś widziała wzrost poziomu morza zgodnie z przedłużającym się ciepłym, wilgotnym klimatem, a nie surowymi, mroźnymi krajobrazami, które istnieją dzisiaj. Źródło: Pensylwania

„Wielką i nową rzeczą, którą zrobiliśmy w tym artykule, jest myślenie o Marsie w kategoriach jego warstw i zapisu osadów” – powiedział Cardenas. „Na Ziemi rysujemy historię cieków wodnych, patrząc na osady, które osadzały się w czasie. Nazywamy tę warstwę ideą, że woda transportuje osady i można mierzyć zmiany na Ziemi, rozumiejąc sposób, w jaki osady się nawarstwiają. już tu zrobiłem — ale to Mars” .

Korzystając z oprogramowania opracowanego przez US Geological Survey, zespół badawczy stworzył mapy z danymi z National Aeronautics and Space Administration ([{” attribute=””>NASA) and the Mars Orbiter Laser Altimeter. They discovered over 6,500 kilometers (4,000 miles) of fluvial ridges and grouped them into 20 systems to show that the ridges are likely eroded river deltas or submarine-channel belts, the remnants of an ancient Martian shoreline.

Elements of rock formations, such as ridge-system thicknesses, elevations, locations, and possible sedimentary flow directions helped the team understand the evolution of the region’s paleogeography. Now known as Aeolis Dorsa, the area that was once ocean contains the densest collection of fluvial ridges on the planet, Cardenas explained.

Traces of Martian Ocean

There has long been debate in the scientific community about whether Mars had an ocean in its low-elevation northern hemisphere. Using topography data, a Penn State led research team was able to show definitive evidence of a roughly 3.5-billion-year-old shoreline with substantial sedimentary accumulation, at least 900 meters thick, that covered hundreds of thousands of square kilometers. Credit: Benjamin Cardenas / Penn State

“The rocks in Aeolis Dorsa capture some fascinating information about what the ocean was like,” he said. “It was dynamic. The sea level rose significantly. Rocks were being deposited along its basins at a fast rate. There was a lot of change happening here.”

On Earth, the ancient sedimentary basins contain the stratigraphic records of evolving climate and life, explained Cardenas. If researchers want to locate a record of life on Mars, an ocean as big as the one that once covered Aeolis Dorsa would be the most logical place to start.

“A major goal for the Mars Curiosity rover missions is to look for signs of life,” Cardenas said. “It’s always been looking for water, for traces of habitable life. This is the biggest one yet. It’s a giant body of water, fed by sediments coming from the highlands, presumably carrying nutrients. If there were tides on ancient Mars, they would have been here, gently bringing in and out water. This is exactly the type of place where ancient Martian life could have evolved.”

Cardenas and his colleagues have mapped what they have determined are other ancient waterways on Mars. An upcoming study in the Journal of Sedimentary Research shows various outcrops visited by the Curiosity rover were likely sedimentary strata from ancient river bars. Another paper published in Nature Geoscience applies an acoustic imaging technique used to view stratigraphy beneath the Gulf of Mexico’s seafloor to a model of Mars-like basin erosion. The researchers determined that fluvial ridges, landforms found widely across Mars, are likely ancient river deposits eroded from large basins similar to Aeolis Dorsa.

“The stratigraphy that we’re interpreting here is quite similar to stratigraphy on Earth,” Cardenas said. “Yes, it sounds like a big claim to say we’ve discovered records of large waterways on Mars, but in reality, this is relatively mundane stratigraphy. It’s textbook geology once you recognize it for what it is. The interesting part, of course, is it’s on Mars.”

Reference: “Paleogeographic Reconstructions of an Ocean Margin on Mars Based on Deltaic Sedimentology at Aeolis Dorsa” by Benjamin T. Cardenas and Michael P. Lamb, 12 October 2022, Journal of Geophysical Research: Planets.
DOI: 10.1029/2022JE007390

The other coauthor on the JGR: Planets paper is Michael P. Lamb, professor of geology at Caltech. The work was funded by the National Aeronautics and Space Administration (NASA).

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