SW VandeCarr said:
I think it's not so much losing oviparity but the transformation to viviparity. Even humans produce eggs. I think we are pretty sure the process begins with egg retention followed by a progression toward a placental viviparity. We also now believe that both early reptiles and mammals had a common amniote ancestor, which makes mammals very old indeed, but still later than the previous glacial period (the Karoo (Permian) ~260-350 mya). It's reasonable to believe that the early mammals were oviparous and that monotremes are a surviving remnant of oviparous mammals. I agree with you that viviparous mammals need not have been very numerous for a long time, perhaps just developing in those regions with seasonal sub-freezing temperatures. If there was a major short cold period at the KT boundary, many oviparous mammals may have been killed off.
I conjecture another reason viviparity may have evolved. Maybe some early mammals live in an area that was “highly disturbed”. The region was prone to catastrophic events or rapid erosion that were very local. An example would be the inner banks of a river, where the erosion is very large.
Laying an egg in such a disturbed region would be very risky. If an egg were layed on the inner banks of a river, the egg could be washed away during a flood. So a viviparous animal in such a disturbed environment would have an advantage over oviparous animals living in such an environment.
Viviparous behavior could have first evolved in cold regions, to prevent the eggs from being “frozen” or “maimed” by the cold. However, the access of disturbed regions could explain how it spread out of cold areas.
This conjecture places mammals right next to early angiosperms. Early angiosperms were weeds that specialized in disturbed regions. Most angiosperms grow quicker than other plants because angiosperm leaves can draw water and carbon dioxide faster than other leaves. In the Mesozoic, most angiosperms lived in temporary areas where they had to grow quickly.
So I have this image of mammals grazing on flowers on an inner bank of a riverbed. The riverbed is eroding away. A pregnant mammal frantically runs to get to the next inner bank. The flower “tries” to grow and seed quicker. The “flower” may even trick the pregnant mammal to carry a seed.
Here is a 2004 article that shows that both birds and mammals helped to spread seeds from the earliest angiosperms. Also, this 2004 article makes the point that the earliest angiosperms grew in river valleys in areas of great erosion.
http://www.life.umd.edu/faculty/wilkinson/BIOL608W/Tiffney2004.pdf
“(c) the Mesozoic was dominated by large herbivorous
dinosaurs, possible sources of diffuse, whole-plant dispersal; (d) simultaneously, several
groups of small vertebrates, including lizards and, in the later Mesozoic, birds
and mammals, could have established more specific vertebrate-plant associations, but
supporting evidence is rudimentary; and (e) the diversification of small mammals and
birds in the Tertiary established a consistent basis for organ-level interactions, allowing
for the widespread occurrence of biotic dispersal in gymnosperms and angiosperms.”
“Angiosperms appeared and diversified in the later portions of the Early Cretaceous
through the Late Cretaceous. The initial radiation involved shrubby or
perhaps herbaceous plants growing in disturbed sites, particularly along rivers
(Wing & Boucher 1998, Friis et al. 1999).” There are viviparous plants. The seeds germinate while attached to the mother plant. One such plant is the mangrove. Interestingly, the mangrove lives in highly disturbed regions.
http://en.wikipedia.org/wiki/Mangrove
“In this harsh environment, mangroves have evolved a special mechanism to help their offspring survive. Mangrove seeds are buoyant and therefore suited to water dispersal. Unlike most plants, whose seeds germinate in soil, many mangroves (e.g. red mangrove) are viviparous, whose seeds germinate while still attached to the parent tree.”This is a 1960 article that claims that angiosperms evolved in the early Creteceous.
http://earth.geology.yale.edu/~ajs/1960/ajs_258A_11.pdf/284.pdf
It is concluded that no bona fide remains, either megafossil or microfossil, have yet been described from rocks older than early Cretaceous sediments.
However, here is an article from 1999 that claims that there are Jurassic microfossils.
http://www.sciencedirect.com/science/article/pii/003466679290167F
“Two species of angiosperm-like pollen are described from an outcrop of lower Oxfordian Oxford Clay at Normandy, France. An Oxfordian age is established by ammonites (Quenstedtoceras mariae zone) and substantiated by associated age-diagnostic dinoflagellates. The angiosperm-like taxa are determined to be in place by their state of preservation and unique morphology.”