Evolution Runs Faster on Short Timescales
quantamagazine.org
quantamagazine.org
Beyond that, what worked for trilobites largely works for horseshoe crabs.
Consider if something is getting larger by say 1% per thousand years, well over 1 million years that's simply unsustainable without becoming ~21,000x as large and thus a very different organism. Further conditions may change promoting periods of shrinking which means the average is going to trend to ever smaller changes per period of time.
AKA, fox sizes might drift up and down some over time, the average is going to stay near their current size unless say wolves died out. At which point they may quickly get larger and replace wolves, but they would not keep growing indefinitely and end up the size of great whales as they are now constrained by the 'wolf' niche. Further, foxes may end up spiting, you have foxes that look about the same, and foxes that look a lot like wolves.
Now if you chart sizes as say 10,11,12,11,10,9 then the transition between those stages is a 'fast' + or - 1, but the net result is only -1 over 6 steps or -1/6th.
The same thing is likely going on with less obvious features, but they are less intuitive.
I was just looking at Taylor expansions today (guid uniqueness...birthday problem), so, this kind of reminds me of that. First you evolve, then you evolve the ability to evolve, then you evolve the ability to evolve the ability to evolve, etc. So maybe there's a formula.
Species experience perturbations in their genetic expression constantly but these only evolve into stable changes when the environment changes to require it.
Rabbit hole warning: Björn Kurtén the Finnish paleontologist whose work on horse fossils was cited early in the OA turns out to be a very interesting character. He wrote what he described as a 'paleonovel' about encounters between CroMagnon and Neandertal people...
Also the dig at the molecular clock is pointless - we have always known that there are many unknowns involved when using a "standard mutation rate" to calculate the time since the divergence between two species. That is nothing new, and the estimates we have are consequently constantly being revised. The time-dependent rate is a good addition to our methodologies, but it isn't the revolution advertised here.
(Oh and by the way, the original paper is from 2005.)
When selective pressures/shocks arise, there is a wider amount of genetic variance that can adapt to the new environment... a larger menu of options for survival, and this pressure acts as a feedback loop, further promoting that more mutations in that direction. Think of the pressures that led to the growth of the giraffe's neck. Perhaps it is this combination... allowing time for a species to thrive and have genetic diversity and shocks which select for and promote the evolutionary path
It seems to me that this is a two stage process.
1. Variation is introduced at a fairly constant rate by mutation. 2. Variation is filtered out by natural selection based on how well it fits the environment.
The shocks occur when the environment changes so that the criteria for fit change and new variations survive for the long term.
So when we look at evolution we see a rate of change driven by the rate of mutation.
When we look at the long term we see a rate of change driven by the environment.
Is this all that surprising?
I was surprised this was surprising.
I think the issue is local optima.
Does not seem to me to be like that.
This makes sense.
...you guys ^^