Third (equatorial) desert belt during Mesozoic era?

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In summary, this claim is from an article discussing the possible mechanism responsible for the existence of three desert belts at some point during the Mesozoic, but it is not clear what the author is asking about.
  • #1
onomatomanic
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Hi board,

I've just been reading up on the basics of meteorology, and http://en.wikipedia.org/wiki/Atmospheric_circulation" this claim:
In the extremely hot climates of the Mesozoic, indications of a third desert belt at the Equator has [sic] been found; it was perhaps caused by convection.
Unfortunately, no further information or references are provided, and the only google hits for "third desert belt" point right back to the article.

I can't make sense of it on my own; naively, the mechanism that is responsible for today's equatorial rainforests (maximum insolation -> air is heated -> air rises -> condensation -> precipitation) should function irrespective of whether the climate is, globally, extremely hot or extremely cold, no?

Any elucidation (including "it's nonsense") would be appreciated!
 
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  • #2
Don't forget that during periods of the mesozoic the continenets were inm much different places. What exactly are you asking about?

Maps of Earth's mesozoic period.

http://www.dinosauria.com/dml/maps.htm
 
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  • #3
Evo said:
What exactly are you asking about?

That's just it, I can't give you any context for that claim, I'd just like to understand it. To me, "third desert belt at the equator" sounds like they are referring to the simultaneous existence of three desert belts at some point during the Mesozoic, one centered on 0 degrees latitude, and the other two (presumably) in the familiar places, i.e. stretching from the http://en.wikipedia.org/wiki/Subtropical_ridge" towards the equator.

One would assume that they corrected for continental drift, otherwise, the claim becomes trivial. *shrug*

So, I'm mainly hoping that someone has heard of something like this before and can supply me with the missing context, so that I can then answer your question. :wink:
 
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  • #4
According to http://www.ldeo.columbia.edu/~polsen/nbcp/modeldis.html" "virtually all of the models depict a "Hot House" Pangea with a dry equatorial zone, except were large mountain ranges and plateaus are specified." For example:

Allen. J. R. L., Hoskins . B . J., Sellwood. B. W., Spicer, R. A., Valdes, P. J. (eds.), 1994, Palaeoclimates and their modeling; with special reference to the Mesozoic era. Chapman & Hall. London, 140 p.


Parrish, J. T., 1993, Climate of the supercontinent Pangea. Journal of Geology. 101: 215-233.

Chandler, M. A., 1994, Depiction of modern and Pangean deserts: evaluation of GCM hydrological diagnostics for paleoclimate studies. GSA Spec. Pap. 288, 117-138

etc.

However, as the aforementioned article points out "in fact, this [equatorial desert]is in direct conflict with the recent "discovery" that Late Triassic Pangea had tropical precipitation and evaporation gradients were not especially different than today's with a distinct wet equatorial region, even deep within Pangea."

Olsen, P.E. and D.V. Kent, 2000, High resolution early Mesozoic Pangean climatic transect in lacustrine environments, in Bachmann, G. and Lerche, I. (eds.), Epicontinental Triassic, Volume 3, Zentralblatt fur Geologie und Palaontologie, VIII: 1475-1496.

Kent, D. V. and Olsen, P. E., 2000, Magnetic polarity stratigraphy and paleolatitude of the Triassic--Jurassic Blomidon Formation in the Fundy basin (Canada): implications for early Mesozoic tropical climate gradients. Earth And Planetary Science Letters, v. 179, no. 2. p. 311-324.


You might want to search Google Scholar for "Mezozoic equatorial desert climate" for a further 2,130 hits.
 
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  • #5
Excellent, I thought it might just be a matter of getting the search terms right. Thanks!

Without having looked at the papers, the excerpt you posted sounds more like there would have been a single vast desert belt, stretching from ~30 degrees North to ~30 degrees South. Will read up and report back.
 

FAQ: Third (equatorial) desert belt during Mesozoic era?

What was the climate like in the Third (equatorial) desert belt during the Mesozoic era?

The Third (equatorial) desert belt during the Mesozoic era was hot and dry, with little to no rainfall. The average temperature was around 30-40 degrees Celsius, and there were frequent sandstorms.

What types of plants and animals lived in the Third (equatorial) desert belt during the Mesozoic era?

The Third (equatorial) desert belt during the Mesozoic era was home to a variety of plants and animals, including cacti, succulents, and other drought-resistant plants. Animals that lived in this region during this time included dinosaurs, pterosaurs, and early mammals.

How did the Third (equatorial) desert belt during the Mesozoic era impact the evolution of plants and animals?

The harsh conditions of the Third (equatorial) desert belt during the Mesozoic era forced plants and animals to adapt to survive. Many plants developed efficient water storage systems and animals evolved features such as thick skin and ability to conserve water. This led to the diversification and evolution of unique species in this region.

Was the Third (equatorial) desert belt during the Mesozoic era completely devoid of life?

No, the Third (equatorial) desert belt during the Mesozoic era was not completely devoid of life. While the conditions were extreme, there were still plants and animals that were able to survive and thrive in this region. However, the diversity and abundance of life may have been lower compared to other regions.

How did the Third (equatorial) desert belt during the Mesozoic era compare to deserts today?

The Third (equatorial) desert belt during the Mesozoic era was similar to modern-day deserts in terms of climate and environment. However, due to the different geological and environmental conditions during the Mesozoic era, the specific plants and animals that inhabited this region may have been different from those found in deserts today.

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