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Children of time: the geological recency of intelligence and its implications for SETI

Published online by Cambridge University Press:  01 December 2023

Giovanni Mussini*
Affiliation:
Department of Earth Sciences, University of Cambridge, Downing St., Cambridge CB2 3EQ, UK
*
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Abstract

Of all species on Earth, only one – Homo sapiens – has developed a technological civilization. As a consequence, estimates of the number of similar civilizations beyond Earth often treat the emergence of human-like intelligence or ‘sophonce’ as an evolutionary unicum: a contingent event unlikely to repeat itself even in biospheres harbouring complex brains, tool use, socially transmitted behaviours and high general intelligence. Here, attention is drawn to the unexpected recency and temporal clustering of these evolutionary preconditions to sophonce, which are shown to be confined to the last ≤102 million years. I argue that this pattern can be explained by the exponential biotic diversification dynamics suggested by the fossil record, which translated into a nonlinearly expanding range of cognitive and behavioural outcomes over the course of Earth's history. As a result, the probability of sophonce arising out of a buildup of its enabling preconditions has been escalating throughout the Phanerozoic. The implications for the Silurian hypothesis and the search for extraterrestrial intelligence (SETI) are discussed. I conclude that the transition from animal-grade multicellularity to sophonce is likely not a rate-limiting step in the evolution of extraterrestrial technological intelligences, and that while H. sapiens is probably the first sophont to evolve on Earth, on macroevolutionary grounds it is unlikely to be the last.

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Type
Research Article
Creative Commons
Creative Common License - CCCreative Common License - BY
This is an Open Access article, distributed under the terms of the Creative Commons Attribution licence (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted re-use, distribution and reproduction, provided the original article is properly cited.
Copyright
Copyright © The Author(s), 2023. Published by Cambridge University Press
Figure 0

Figure 1. The temporal and phylogenetic distribution of maximal EQ values and likely CCE exaptations in (from top to bottom) catarrhines, platyrrhines, cetaceans, proboscideans, psittaciforms, corvids, decapods and octopods. Tree bifurcations indicate approximate divergence dates between the lineages marked by icons on the right. Tieplots show the presence of exaptations to sophonce in their respective lineages; for each lineage, maximum EQ values (Jerison, 1973) are represented by shading (legend in the top-left corner). In non-vertebrates to which EQ measures are inapplicable, branches are marked by N/A. Data from Ni et al. (2019); Montgomery et al. (2013); Benoit et al. (2019); Ksepka et al. (2020); Prum et al. (2015); Whalen and Landman (2022).

Figure 1

Figure 2. Classic plots of biodiversity and encephalization values through geological time. (a) The diversification of complex life through the Phanerozoic, plotted as logarithm of family-level richness for all organisms, terrestrial and marine (maximum curve). Redrawn from Benton (1995). (b) The nonlinear increase in maximum encephalization quotient (EQ) levels during the Phanerozoic. The ‘living fossils’ Branchiostoma, Petromyzon and Latimeria serve as proxies for the maximum level of encephalization at various intervals of the Palaeozoic, based on phylogenetic bracketing and resemblance to extinct taxa. Cenozoic data points (taxon names not shown) include Plesiadapis, Tetonius, Heptodon, Homacodon, Necrolemur, Leontinia, Argyrocetus, Homo abilis, H. erectus and H. sapiens. The regression line (dashed) follows the equation ln EQ = 0.0135 × (531 − t)−6.23. Redrawn from Russell (1983). In both diagrams, the vertical dashed line marks the beginning of a sharp Cenozoic uptick in both diversity and maximum encephalization levels. Legend: C, Cambrian; O, Ordovician; S, Silurian; Crb, Carboniferous; P, Permian; Tr, Triassic; Jur, Jurassic; Cret, Cretaceous; Pg, Palaeogene; Ne, Neogene.