Showing posts with label global warming. Show all posts
Showing posts with label global warming. Show all posts

Sunday, June 22, 2014

Bear-ly Sustainable: Can Polar Bears Find Refuge in the Genome of Brown Bears?

Tobias Bidon
Ok today I want to write about a more contemporary topic - the genetic legacy of bears. And I want to direct your attention to a paper dealing with the complicated genetic history of modern bears - abstract here and the more accessible science daily article: Evolutionary history of bears: It's complicated. Of course you should go read the articles yourself but what the gist of the story is that the genetic history resulting in the "species" or better yet "species groups" of modern bears is vastly complicated with numerous inbreeding occurrences and hybridization events. It appears many, if not most, bear species are kissing cousins. Central to the story is Beringia, the now submerged land bridge joining Asia and North America. According to the research Beringia may have served as a bit of mixing grounds from which the modern trajectories of bears into Asia and the Americas have since went their respective ways. Of course the bear family is just one of several carnivorous mammal families (felids, canids) that readily hybridizes. There is even a wikipedia web page on the subject of ursid hybrids. This topic of course delves deeply into the surprisingly murky definition of what constitutes a species. The long and short of it from what I gather is that the definition of what constitutes a species depends on who you ask.

Now just thinking about bear hybridization events should get you thinking about the well documented hybridization of polar and brown bears. Two species that are closely related and overlap enough in range and habit that matings do and have occurred quite often it seems.

Polar/Brown hybrid. wiki
Rothschild Museum
Thinking out loud after reading these articles and with the prospect of polar/brown bear hybridization events occurring more frequently in an Arctic under the influence of AGW I wondered: instead of going extinct, might the genome of polar bears find refuge in northern populations of brown bears? That is if through increased meetings due to lack of sea ice, the polar bear gets absorbed by the larger brown bear population shifting it's range north - could such an admixture reverse in the future if climatic conditions shift back to a regime more ameliorative to polar bears? Granted that they are so close genetically anyways - why couldn't the polar bear reemerge in several thousand years from a stock of hybridized polar/brown bears? The lack of color, streamlined form, ice gripping claws, and carnivorous dentition being selected for  in such a scenario and the polar bear reemerging... why not? I think it is an interesting notion, interesting enough to write a blog post about anyways.


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Friday, October 12, 2012

"Global Weirding" in the Cretaceous

Geophysical fluids dynamic model of equatorial current showing persistent eddies (c)Earth Sci-Rev 2012 Oct


Well here in 'Merica we are in the midst of the great presidential race of Mitt vs Obama 2012, which of course will decide the fate of this country and therefore the world at large. Once again the country is divided on numerous issues; genital politics- who gets to marry who and what women can do with their fetuses; the role of big government vs small government; and how to recapture a robust middle class. However it has not escaped the notice of some that the issue of climate warming or "climate weirding" (which I prefer) has elicited nary a mention from either side. Perhaps both sides have been advised to not mention such a pressing issue- to either outright deny its existence or promise to curb it may be akin to political suicide at this pass. Even the Obama advisors who helped catapult Obama into presidency in '08 largely on a platform of green job growth may now realize all to well that any remedy we can muster to soothe our climate gods is akin to putting a bandaid on an amputated leg. It's too late.

(c) Mike Luckovich Atlanta Journal Constitution


This is for shame because if North America continues with drought conditions it will not be long some think before this country starts to see the food shortages and hence food riots that other countries are already experiencing. And when people are rioting on the streets for food or water the issues of who gets to marry who and even who gets to hire who will fall by the wayside. We will all be too hungry to really care.

Algerian food riots 2008. Guardina.co.uk (c)


Of course I could be wrong, we can all hope. But climate change, often dramatic, in the context of geological time is the rule rather than the exception.

A new paper written by William W. Hay and Sascha Floegel, New thoughts about the cretaceous climates and oceans, synthesizes much of the current thought regarding this critical juncture in earth's history.

Abstract

Several new discoveries suggest that the climate of the Cretaceous may have been more different from that of today than has been previously supposed. Detailed maps of climate sensitive fossils and sediments compiled by Nicolai Chumakov and his colleagues in Russia indicate widespread aridity in the equatorial region during the Early Cretaceous. The very warm ocean temperatures postulated for the Mid-Cretaceous by some authors would likely have resulted in unacceptable heat stress for land plants at those latitudes, however, and may be flawed.
Seasonal reversals of the atmospheric pressure systems in the Polar Regions are an oversimplification. However, seasonal pressure difference between 30° and 60° latitude become quite pronounced, being more than 25 hPa in winter and less than 10 hPa in summer. This results in inconstant winds, affecting the development of the gyre-limiting frontal systems that control modern ocean circulation. The idea of Hasegawa et al. (2011) who suggest a drastic reduction in the size of the Hadley cells during the warm Cretaceous greenhouse is supported by several numerical climate simulations. Rapid contraction of the Hadley cell such that its sinking dry air occurs at 15° N latitude rather than 30° N is proposed to occur at a threshold of 1,000 ppmv CO2 in the atmosphere. This change will probably be reached in the next century.

Now longtime readers of da' Salad should recall my first paleo-myth where I discussed the myth of the enduring, unchanging tropical rain forest. It now appears that not only is the tropical equator belt not a safe womb of biological diversity, it is actually a crucible of evolution. And the high extinction and diversification rates for equatorial regions do fall in line with this model. 

The distribution of modern deserts is strongly influenced by the Hadley cell and it is no coincidence that most major deserts occur at about 30 degrees north or south of the equator, also known as the subtropical convergence belt. However work by Hasegawa shows that this zone shifted poleward during the Cretaceous thermal maxim to between 31 and 41 degrees north of the equator followed by a rapid retraction equatorward to between 22 and 30 degrees north of equator during the mid Cretaceous. What Hasegawa and the authors in the above study suggest to be the threshold for this equatorward retraction of the subtropical convergence is CO2 levels above 1,000 ppmv a level we are projected to reach by the next century. Scary stuff. Imagine the tropical latitudes, where a good portion of humanity lives, inexorably transformed into desert wastelands. More temperate latitude countries would essentially be crushed by the burden of either importing food into these areas, which is already happening to an extent, or finding ways to either thwart or absorb these populations looking for food. Scary stuff.

Well let's shift gears from environmental doomsday scenarios into ideas about what this on and off again Mesozoic arid belt meant biogeographically for dinosaurs. plants and other organisms. What questions does it raise? What should we be looking for? What were these arid equatorial Mesozoic ecosystems like? More to come....






Perinencia


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