Pre-Noachian
| Pre-Noachian | |
|---|---|
 MOLA colorized relief and elevation map of the Hesperia Planum region. Hesperia Planum is considered to show aspects of Mars' geological evolution from the Pre-Noachian to the Noachian periods. It showcases lowlands representing the Pre-Noachian landscape, alongside higher terrain indicative of the Noachian era. | |
| Usage information | |
| Celestial body | Mars |
| Time scale(s) used | Martian Geologic Timescale |
The Pre-Noachian is a geologic system and early time period on the planet Mars characterized by intense meteorite and asteroid impacts, volcanic and tectonic activity, and the potential existence of surface or subsurface water.[1] This era represents a crucial phase in Mars' history, witnessing the planet's formation, and the shaping of its geological landscape. However, the Pre-Noachian period remains elusive, being the least understood among Mars' four geological phases. Erosion and deposition have obscured much of the evidence from this time period on Mars.
The Pre-Noachian period created lowlands on the northern hemisphere of Mars, potentially serving as reservoirs for ancient Martian water during later periods. These lowlands might have formed through lava erosion caused by extensive volcanic activity during this era, as the Pre-Noachian time period experienced the highest level of volcanic activity among all Martian epochs.[1]
During the Pre-Noachian period, Mars' atmosphere was denser than it is today, with higher concentrations of carbon dioxide stemming from volcanic, asteroid, comet, and meteorite outgases. This may have contributed to a possible greenhouse effect on Mars and the formation of silicates, iron oxide, sulfates, carbonates, clays, and hydrates, created from extensive heat.[2] It is believed that as a result of meteorite outgassing, water vapor condensed into Mars' atmosphere. As the planet cooled, this water vapor precipitated onto the surface, forming oceans across Mars during subsequent time periods.[1] Over time, the gases retained by Mars' gravity during the Pre-Noachian period have gradually outgassed from the planet's atmosphere. This occurs as the molecules become too heavy and dense to be contained in a cooler environment, leading to their release into space.[1]
During this time, Mars had a distinct magnetic field because its core was active. As magma cooled in the planet's lower layers, it formed metals necessary to make the magnetic field.[3]
Description and name origin[edit]
The Pre-Noachian System and Period is named after Noachis Terra, a region of highlands west of the Hellas Planitia basin, and the pre comes from the word meaning before.[4] (See Description and name origin on the Wikipedia page for the Noachian era on Mars for more information)
Pre-Noachian chronology and stratigraphy[edit]
Martian time periods are based on geologic mapping of surface units from spacecraft images. A surface unit is a terrain with a distinct texture, color, albedo, spectral property, or set of landforms that distinguish it from other surface units and is large enough to be shown on a map. Mappers use a stratigraphic approach pioneered in the early 1960s for photogeologic studies of the Moon.[5] Although based on surface characteristics, a surface unit is not the surface itself or group of landforms. It is an inferred geologic unit (e.g., formation) representing a sheetlike, wedgelike, or tabular body of rock that underlies the surface.[6][7] A surface unit may be a crater ejecta deposit, lava flow, or any surface that can be represented in three dimensions as a discrete stratum bound above or below by adjacent units (illustrated right). Using principles such as superpositioning (illustrated left), cross-cutting relationships, and the relationship of impact crater density to age, geologists can place the units into a relative age sequence from oldest to youngest. Units of similar age are grouped globally into larger, time-stratigraphic (chronostratigraphic) units, called systems. For Mars, four systems are defined: the Pre-Noachian Noachian, Hesperian, and Amazonian. Geologic units lying below (older than) the Noachian are informally designated Pre-Noachian.[8] The geologic time (geochronologic) equivalent of the Pre-Noachian System is the Pre-Noachian Period. Rock or surface units of the Pre-Noachian System were formed or deposited during the Pre-Noachian Period.
System vs. Period[edit]
| Segments of rock (strata) in chronostratigraphy | Periods of time in geochronology | Notes (Mars) |
|---|---|---|
| Eonothem | Eon | not used for Mars |
| Erathem | Era | not used for Mars |
| System | Period | 3 total; 108 to 109 years in length |
| Series | Epoch | 8 total; 107 to 108 years in length |
| Stage | Age | not used for Mars |
| Chronozone | Chron | smaller than an age/stage; not used by the ICS timescale |
System and Period are not interchangeable terms in formal stratigraphic nomenclature, although they are frequently confused in popular literature. A system is an idealized stratigraphic column based on the physical rock record of a type area (type section) correlated with rocks sections from many different locations planetwide.[10] A system is bound above and below by strata with distinctly different characteristics (on Earth, usually index fossils) that indicate dramatic (often abrupt) changes in the dominant fauna or environmental conditions. (See Cretaceous–Paleogene boundary as example.)
At any location, rock sections in a given system are apt to contain gaps (unconformities) analogous to missing pages from a book. In some places, rocks from the system are absent entirely due to nondeposition or later erosion. For example, rocks of the Cretaceous System are absent throughout much of the eastern central interior of the United States. However, the time interval of the Cretaceous (Cretaceous Period) still occurred there. Thus, a geologic period represents the time interval over which the strata of a system were deposited, including any unknown amounts of time present in gaps.[10] Periods are measured in years, determined by radioactive dating. On Mars, radiometric ages are not available except from Martian meteorites whose provenance and stratigraphic context are unknown. Instead, absolute ages on Mars are determined by impact crater density, which is heavily dependent upon models of crater formation over time.[11] Accordingly, the beginning and end dates for Martian periods are uncertain, especially for the Hesperian/Amazonian boundary, which may be in error by a factor of 2 or 3.[8][12]
Boundaries and subdivisions[edit]
The lower boundary of the Pre-Noachian period on Mars is characterized by the emergence of significant geological activity and the initial shaping of the planet's surface during its early history. This boundary is defined by the presence of ancient cratered terrains, volcanic constructs, and impact ejecta deposits dating back to the earliest stages of Martian geological development. While the precise location of this boundary may vary depending on geological context and criteria used for its definition, it marks the beginning of Mars’ geological history as understood by scientists.
In the Pre-Noachian period, the eastern region of Mars featured ridged plains overlaying early to mid-Noachian aged cratered plateau materials. This period marked a significant phase in Mars’ geological history, preceding the Noachian era characterized by its own distinct geological features and processes.
The Pre-Noachian System is subdivided into two chronostratigraphic series: Lower Pre-Noachian and Upper Pre-Noachian. These series are delineated based on specific references or locations on Mars where surface units indicate distinctive geological episodes, identifiable by cratering age and stratigraphic position. For example, Hesperia Planum serves as the referent location for the Lower Pre-Noachian Series. The corresponding geologic time units for the two Pre-Noachian series are the Early Pre-Noachian and Late Pre-Noachian Epochs. It's important to note that an epoch is a subdivision of a period, and the terms are not synonymous in formal stratigraphy. The age of the Early Pre-Noachian/Late Pre-Noachian boundary remains uncertain, with estimates ranging from 4500 to 4100 million years ago based on crater counts.[13][14]
Stratigraphic terms are often confusing to geologists and non-geologists alike. One way to sort through the difficulty is by the following example: You can easily go to Cincinnati, Ohio and visit a rock outcrop in the Upper Ordovician Series of the Ordovician System. You can even collect a fossil trilobite there. However, you cannot visit the Late Ordovician Epoch in the Ordovician Period and collect an actual trilobite.
The Earth-based scheme of formal stratigraphic nomenclature has been successfully applied to Mars for several decades now but has numerous flaws. The scheme will no doubt become refined or replaced as more and better data become available.[15] (See mineralogical timeline below as example of alternative.) Obtaining radiometric ages on samples from identified surface units is clearly necessary for a more complete understanding of Martian history and chronology.[16]
Mars during the Pre-Noachian Period[edit]
During the Pre-Noachian period, Mars experienced significant geological and environmental dynamics. Intense volcanic activity sculpted the planet's surface through widespread eruptions, while impact cratering events left behind numerous craters across the Martian landscape. The atmosphere during this era was denser than in present times, likely containing higher concentrations of carbon dioxide and other gases, potentially contributing to a greenhouse effect. This atmospheric composition may have facilitated conditions conducive to the presence of liquid water on the surface, with evidence suggesting the existence of water bodies such as lakes, rivers, and possibly even oceans. Geological features such as valleys, channels, and basins formed during this period further support the notion of liquid water on ancient Mars. The Pre-Noachian period stands as a crucial era in Martian history, characterized by dynamic geological processes and the potential for liquid water, laying the groundwork for subsequent epochs of Martian evolution.[1][13]
References[edit]
- ^ a b c d e "The ages of Mars". Mars Express - European Space Agency (ESA). Retrieved 25 March 2024.
- ^ Dyar, M. D. (2013). "Mars mineralogy: A review of current terrestrial analogs and a proposed new framework". Planetary and Space Science. 86: 27–35. Bibcode:2013P&SS...86...27D. doi:10.1016/j.pss.2013.05.003.
- ^ Halliday, A. J.; Nimmo, F.; Wilson, M. J. R.; Anbar, A. D. (2010). "Mars: Evidence for a Dry Climate from Recent Mass Balance of Atmosphere and Ice". Earth and Planetary Science Letters. 294 (3–4): 538–546. doi:10.1016/j.epsl.2009.12.041.
- ^ Amos, Jonathan (10 September 2012). "Clays in Pacific Lavas Challenge Wet Early Mars Idea". BBC News.
- ^ See Mutch, T.A. (1970). Geology of the Moon: A Stratigraphic View; Princeton University Press: Princeton, NJ, 324 pp. and Wilhelms, D.E. (1987). The Geologic History of the Moon, USGS Professional Paper 1348; http://ser.sese.asu.edu/GHM/ for reviews of this topic.
- ^ Wilhelms, D.E. (1990). Geologic Mapping in Planetary Mapping, R. Greeley, R.M. Batson, Eds.; Cambridge University Press: Cambridge UK, p. 214.
- ^ Tanaka, K.L.; Scott, D.H.; Greeley, R. (1992). Global Stratigraphy in Mars, H.H. Kieffer et al., Eds.; University of Arizona Press: Tucson, AZ, pp. 345–382.
- ^ a b Nimmo, F.; Tanaka, K. (2005). "Early Crustal Evolution of Mars". Annual Review of Earth and Planetary Sciences. 33 (1): 133–161. Bibcode:2005AREPS..33..133N. doi:10.1146/annurev.earth.33.092203.122637.
- ^ International Commission on Stratigraphy. "International Stratigraphic Chart" (PDF). Retrieved 2009-09-25.
- ^ a b Eicher, D.L.; McAlester, A.L. (1980). History of the Earth; Prentice-Hall: Englewood Cliffs, NJ, pp 143–146, ISBN 0-13-390047-9.
- ^ Masson, P.; Carr, M.H.; Costard, F.; Greeley, R.; Hauber, E.; Jaumann, R. (2001). "Geomorphologic Evidence for Liquid Water". Chronology and Evolution of Mars. Space Sciences Series of ISSI. Vol. 96. p. 352. Bibcode:2001cem..book..333M. doi:10.1007/978-94-017-1035-0_12. ISBN 978-90-481-5725-9.
{{cite book}}:|journal=ignored (help) - ^ Hartmann, W.K.; Neukum, G. (2001). Cratering Chronology and Evolution of Mars. In Chronology and Evolution of Mars, Kallenbach, R. et al. Eds., Space Science Reviews, 96: 105–164.
- ^ a b Ehlmann, Bethany L.; Carter, John; Ernst, Carolyn M. (2017). "The stratigraphy and history of Mars' northern lowlands through mineralogy of impact craters: A comprehensive survey". Journal of Geophysical Research: Planets. 122 (6): 1226–1245. doi:10.1002/2017JE005276.
- ^ Rodriguez, J. Alexis P.; Dobrea, Eldar Noe; Kargel, Jeffrey S.; Baker, V. R.; Crown, David A.; Webster, Kevin D.; Berman, Daniel C.; Wilhelm, Mary Beth; Buckner, Denise (2020-04-24). "The Oldest Highlands of Mars May Be Massive Dust Fallout Deposits". Scientific Reports. 10 (1): 7257. Bibcode:2020NatSR..10.7257Z. doi:10.1038/s41598-020-64676-z. PMC 7189948. PMID 32332708. Retrieved 2024-03-26.
- ^ Tanaka, K.L. (2001). The Stratigraphy of Mars: What We Know, Don't Know, and Need to Do. 32nd Lunar and Planetary Science Conference, Abstract #1695. http://www.lpi.usra.edu/meetings/lpsc2001/pdf/1695.pdf.
- ^ Carr, 2006, p. 41.