| Allan Hills 77005 | |
|---|---|
Meteorite ALH-77005 | |
| Type | Achondrite (unique), lherzolite |
| Clan | Martian meteorite |
| Composition | ~55% olivine, ~35% pyroxene, ~8% maskelynite and ~2% opaques |
| Shock stage | S6 |
| Weathering grade | A |
| Country | Antarctica |
| Region | Allan Hills |
| Coordinates | 76°43′00″S 159°40′00″E / 76.71667°S 159.66667°E |
| Observed fall | No |
| Found date | 29 December 1977 (Japanese National Institute of Polar Research mission) |
| TKW | 482.5 g |
Allan Hills 77005 (also known as Allan Hills A77005, ALHA77005, ALH77005 and ALH-77005) is a Martian meteorite that was found in the Allan Hills of Antarctica in 1977 by a Japanese National Institute of Polar Research mission team and ANSMET. Like other members of the group of SNCs (shergottite, nakhlite, chassignite), ALH-77005 is thought to be from Mars.
On discovery, the mass of ALH-77005 was 482.5 g (1.064 lb). Initial geological examination determined that the meteorite was composed of ~55% olivine, ~35% pyroxene, ~8% maskelynite and ~2% opaques.
In March 2019, researchers reported the possibility of biosignatures in this Martian meteorite based on its microtexture and morphology as detected with optical microscopy and FTIR-ATR microscopy, and on the detection of mineralized organic compounds, suggesting that microbial life could have existed on the planet Mars. More broadly, and as a result of their studies, the researchers suggest Solar System materials should be carefully studied to determine whether there may be signs of microbial forms within other space rocks as well.