Evolution and extinction in the marine realm: some constraints imposed by phytoplankton

Marine planktonic microbes survived climatic instabilities in the past

In the geological past, changes in climate and tectonic activity are thought to have spurred the tempo of evolutionary change among major taxonomic groups of plants and animals. However, the extent to which these historical contingencies increased the risk of extinction of microbial plankton species remains largely unknown. Here, I analyse fossil records of marine planktonic diatoms and calcareous nannoplankton over the past 65 million years from the world oceans and show that the probability of species' extinction is not correlated with secular changes in climatic instability. Further supporting these results, analyses of genera survivorship curves based on fossil data concurred with the predictions of a birth-death model that simulates the extinction of genera through time assuming stochastically constant rates of speciation and extinction. However, my results also show that these marine microbes responded to exceptional climatic contingencies in a manner that appears to have promoted net diversification. These results highlight the ability of marine planktonic microbes to survive climatic instabilities in the geological past, and point to different mechanisms underlying the processes of speciation and extinction in these micro-organisms.

Phytoplankton growth after a century of dormancy illuminates past resilience to catastrophic darkness

Photosynthesis evolved in the oceans more than 3 billion years ago and has persisted throughout all major extinction events in Earth's history. The most recent of such events is linked to an abrupt collapse of primary production due to darkness following the Chicxulub asteroid impact 65.5 million years ago. Coastal phytoplankton groups (particularly dinoflagellates and diatoms) appear to have been resilient to this biotic crisis, but the reason for their high survival rates is still unknown. Here we show that the growth performance of dinoflagellate cells germinated from resting stages is unaffected by up to a century of dormancy. Our results clearly indicate that phytoplankton resting stages can endure periods of darkness far exceeding those estimated for the Cretaceous-Paleogene extinction and may effectively aid the rapid resurgence of primary production in coastal areas after events of prolonged photosynthesis shut-down.

Extinctions in heterogeneous environments and the evolution of modularity

Extinctions of local subpopulations are common events in nature. Here, we ask whether such extinctions can affect the design of biological networks within organisms over evolutionary timescales. We study the impact of extinction events on modularity of biological systems, a common architectural principle found on multiple scales in biology. As a model system, we use networks that evolve toward goals specified as desired input–output relationships. We use an extinction–recolonization model, in which metapopulations occupy and migrate between different localities. Each locality displays a different environmental condition (goal), but shares the same set of subgoals with other localities. We find that in the absence of extinction events, the evolved computational networks are typically highly optimal for their localities with a nonmodular structure. In contrast, when local populations go extinct from time to time, we find that the evolved networks are modular in structure. Modular circuitry is selected because of its ability to adapt rapidly to the conditions of the free niche following an extinction event. This rapid adaptation is mainly achieved through genetic recombination of modules between immigrants from neighboring local populations. This study suggests, therefore, that extinctions in heterogeneous environments promote the evolution of modular biological network structure, allowing local populations to effectively recombine their modules to recolonize niches.

Towards a new evolutionary synthesis

New concepts and information from molecular developmental biology, systematics, geology and the fossil record of all groups of organisms, need to be integrated into an expanded evolutionary synthesis. These fields of study show that large-scale evolutionary phenomena cannot be understood solely on the basis of extrapolation from processes observed at the level of modern populations and species. Patterns and rates of evolution are much more varied than had been conceived by Darwin or the evolutionary synthesis, and physical factors of the earth's history have had a significant, but extremely varied, impact on the evolution of life.

Quantitative estimates of changes in marine and terrestrial primary productivity over the past 300 million years

Changes in marine primary production over geological time have influenced a network of global biogeochemical cycles with corresponding feedbacks on climate. However, these changes continue to remain largely unquantified because of uncertainties in calculating global estimates from sedimentary palaeoproductivity indicators. I therefore describe a new approach to the problem using a mass balance analysis of the stable isotopes (18O/16O) of oxygen with modelled O2 fluxes and isotopic exchanges by terrestrial vegetation for 300, 150, 100 and 50 million years before present, and the treatment of the Earth as a closed system, with respect to the cycling of O2. Calculated in this way, oceanic net primary productivity was low in the Carboniferous but high (up to four times that of modern oceans) during the Late Jurassic, mid-Cretaceous and early Eocene greenhouse eras with a greater requirement for key nutrients. Such a requirement would be compatible with accelerated rates of continental weathering under the greenhouse conditions of the Mesozoic and early Tertiary. These results indicate possible changes in the strength of a key component of the oceanic carbon (organic and carbonate) pump in the geological past, with a corresponding feedback on atmospheric CO2 and climate, and provide an improved framework for understanding the role of ocean biota in the evolution of the global biogeochemical cycles of C, N and P.

A theoretical integration of Cambrian explosion and post-Permian quiescence

Trophic dynamics is internally causative. Each trophic level is causative in initiating changes in trophic flow either as a supplier towards the upper level or as a consumer towards the lower. Resource presentation followed by its subsequent exploitation makes suppliers causative, while resource exploitation followed by its subsequent presentation makes consumers causative. Trophic dynamics of supplier domination gradually alternates with that of consumer domination while being punctuated by occasional mass extinctions due to depletion of the resources towards the lowest trophic level. The Cambrian explosion could be associated with trophic dynamics of supplier domination, whereas the post-Permian quiescence with that of consumer influencing supplier domination.