The Biological Big Bang: The First Oceans of Primordial Planets at 2-8 Million Years Explain Hoyle/Wickramasinghe Cometary Panspermia

TL;DR

This paper proposes that primordial planets with oceans formed early in the universe's history, providing a natural environment for life to originate and spread via comets, supporting the cometary panspermia hypothesis.

Contribution

It introduces a hydrogravitional-dynamics cosmology model explaining early planet formation and the origin of life, challenging standard cosmology and supporting panspermia.

Findings

Primordial planets formed at 300 Kyr after the big bang.

First organic chemistry and life originated in these planets' oceans between 2-8 million years.

Complex life on Earth supports the cosmological model proposed.

Abstract

Hydrogravitional-dynamics (HGD) cosmology of Gibson/Schild 1996 predicts that the primordial H-He^4 gas of big bang nucleosynthesis became proto-globular-star-cluster clumps of Earth-mass planets at 300 Kyr. The first stars formed from mergers of these 3000 K gas planets. Chemicals C, N, O, Fe etc. created by stars and supernovae then seeded many of the reducing hydrogen gas planets with oxides to give them hot water oceans with metallic iron-nickel cores. Water oceans at critical temperature 647 K then hosted the first organic chemistry and the first life, distributed to the 10^80 planets of the cosmological big bang by comets produced by the new (HGD) planet-merger star formation mechanism. The biological big bang scenario occurs between 2 Myr when liquid oceans condensed and 8 Myr when they froze. HGD cosmology explains, very naturally, the Hoyle/Wickramasinghe concept of cometary panspermia by giving a vast, hot, nourishing, cosmological primordial soup for abiogenesis, and the means for transmitting the resulting life forms and their evolving chemical mechanisms widely throughout the universe. A primordial astrophysical basis is provided for astrobiology by HGD cosmology. Concordance {\Lambda}CDMHC cosmology is rendered obsolete by the observation of complex life on Earth.