Large tides may have been a key factor in the evolution of bony fish and tetrapods
Pioneering research, published in Proceedings of the Royal Society A, into deep-time tides during the Late Silurian – Devonian periods (420 Ma -380 Ma), suggests that large tides may have been a key environmental factor in the evolution of bony fish and early tetrapods, the first vertebrate land-dwellers.
The study is a detailed development of a theory previously published in the same journal (Balbus 2014), which suggested that the Moon’s particular mass and orbital location are optimised for creating large tidal ranges and isolating tidal pools, which in turn may have been a biological impetus for the development of limbs in fish stranded between very high tides.
Researchers from Bangor University's School of Ocean Sciences and Oxford University (UK) and Uppsala University, (Sweden) have been the first to produce detailed numerical simulations to address the question of whether large tides occurred during this critical period. These are also the first calculations to relate tidal hydrodynamics to an evolutionary biological event.
The numerical simulations were computed using palaeogeographic reconstructions of the Earth’s continents in an established state-of-the-art numerical tidal model. The simulation results show tidal variations in excess of four meters occurring around an area known as the South China block, which is the site of the origin and diversification of the earliest bony fish group, and has produced the earliest important fossils for this group. Geological evidence also points to tidal environments being closely associated with this class of fossils.
These first-of-their-kind results stimulate the need for more detailed tidal simulations of the ancient Earth. In particular, the researchers believe that the method used in this study can be used with a variety of palaeogeographic reconstructions at other time periods, to explore the tidal influence upon the origin and diversification of other early vertebrates, and perhaps the opposite as well: what might have been the role of tides in precipitating marine extinction events?