Since its discovery over two decades ago, the deep subsurface biosphere has been considered to be the realm of single cell organisms, extending >3 km into the Earth's crust and comprising a significant fraction of the global biosphere 1,2,3,4 . The constraints of temperature, energy, O 2 and space seemed to preclude the possibility of more complex multi-cellular organisms from surviving at these depths. Here we report species of the phylum Nematoda that have been detected in or recovered from 0.9-3.6 km deep fracture water encountered in the deep mines of South Africa, but have not been detected in the mining water. These subsurface nematodes, including a new species Halicephalobus mephisto, tolerate high temperature, reproduce asexually and preferentially feed upon subsurface bacteria. 14 C data indicate that the fracture water in which the nematodes reside is 3-12 kyr old paleometeoric water. Our data suggest that nematodes should be found in other deep hypoxic settings where temperature permits and that they may control the microbial population density by grazing upon fracture surface biofilm patches. Our results expand the known Metazoan biosphere and demonstrate that deep ecosystems are more complex than previously accepted. The discovery of multi-cellular life in the deep subsurface of the Earth also has important implications for the search for subsurface life on other worlds in our solar system. .
Halicephalobus mephisto