When life first formed in earth's ocean, was it salty yet?
Current estimates suggest that last universal common ancestor of life on earth lived in hydrothermal vents 3.8–3.5 billion years ago.1  Petrologic examination of quartz formed near these vents during that time suggests that seawater had a higher salinity compared to current oceans 2 --

Our data are in agreement with six other data sets—from the 3.75 Ga Isua Greenstone Belt (W. Greenland), the 3.24 Ga Pilbara region (W. Australia), the ∼3.2 Ga Barberton Greenstone Belt (South Africa; 2), the ∼2.7 Ga Matagami area (Abitibi Greenstone Belt, Canada), and the Proterozoic (∼2.2 Ga) Ongeluk Formation (South Africa). The consistency of fluid inclusion data suggests that Archean and early Proterozoic seawater may have been more saline, and potentially stratified, compared to modern seawater.

Note: Ga (for gigaannum) – a unit of time equal to 109 years.


Weiss, M., Sousa, F., Mrnjavac, N. et al. The physiology and habitat of the last universal common ancestor. Nat Microbiol 1, 16116 (2016).
Weiershäuser, L., Spooner, E.T.C. Seafloor hydrothermal fluids, Ben Nevis area, Abitibi Greenstone Belt: Implications for Archean (∼2.7Ga) seawater properties. Precambrian Research, Volume 138, Issues 1–2, 2005, Pages 89-123.