If we could keep that gene from turning off then birds would be as big as their ancestors were!
Indeed. There is a rather cool project organized by the world-famous paleontologist
Jack Horner that is trying to cultivate the suppressed dinosaur genetics in chicken-stock to breed a small
dromaesaurian. I could explain the whole process in the exhaustive detail only a dinosaur enthusiast and bachelors in science can muster, but Horner himself presents it rather well here in a TED talk:
[youtube]0QVXdEOiCw8[/youtube]
Also weren't the big dinosaurs slowly dying out anyway?
There is little evidence for this. Dinosaur speciation was at it's height during the later stages of the Cretaceous, as any peek into a dinosaur encyclopedia or trip to museum will confirm. Some have argued that this is just a geological bias, because Cretaceous rock fossilizes better then those rock of other strata, but this is not generally accepted. Dinosaurs were diversifying at an explosive rate during the late Cretaceous - if anything, the global cooling and subsequent dramatization of seasons during the
Campanian and
Maastrichtian Cretaceous stage made them adapt even faster.
The only true declination in diversity in the animals at the time were among the
pterosaurs - a clade or order of creatures that are actually not dinosaurs, despite what many people believe. They belong to the distinct order of pterosaumorpha, whereas dinosaurs belonged to the clade Dinosauria. The reason for the pterosaur's decline and loss of the dominion of the skies was due to... more dinosaurs. Birds, in fact. By the end of the Maastrichtian stage of the Late Cretaceous, there was only around 6 species of pterosaurs left in the world - all belonging to the family
Azhdarchidae, the most well known species being the gigantic
Quetzalcoatlus northropi:
Compare that to pterosaur populations from earlier times in the world, with thousands of known species from dozens of families. As
Watsisname mentioned, birds ARE dinosaurs. So in light of this, one could say that the dinosaurs had solidified their claim to global domination one step further with their close relatives, the birds, by pushing the rivaling pterosaurs into extinction (and possibly out of the skies altogether - there is some debate as to validity of the claim that Quetzalcoatlus and other Azdarchids could even fly). The only biome the dinosaurs hadn't claimed at that point were the seas. I believe I had provided a good link discussing this sort of thing here:
http://www.bbc.com/future/story/20170918-what-if-the-dinosaurs-hadnt-died-out
And did the impact bring about flowering plants or was that due to changes in climate that were already happening?
Angiosperms (or any plant that flowers) have there roots (pun intended

) way back in the Triassic Period (251.9 million to 201.3 million years ago - the Triassic is the first period of the
Mesozoic Era, which ended in the Cretaceous K-T extinction) when dinosaurs were still evolving from small, lizard-like archosauria. They diversified into recognizable species as we might see today in the early Cretaceous around 120 million years ago during the
Aptian stage of that period. The point is, dinosaurs were well=adapted to eat flowering plants and their close relatives. Angiosperms did eventually replace
conifers as the dominant trees from 100 to 60 millio years ago (from the
Cenomanian to the Maastrichtian stage, roughly). This may have influenced dinosaur size and evolution, perhaps reducing overall dinosaur size by a percentage. Certainly such plant-guzzlers like the famous and truly huge long-necked
sauropods shrunk somewhat in size after the 100 million year mark, suspiciously correlative with the rise of the angiosperms. The Chicxulub impact at the end of the Cretaceous hit the angiosperms just as hard as it hit the dinosaurs - many species went extinct, and like the dinosaurs - many descendants and derivatives are alive today.
Interesting that there were no ice ages back then and all land was concentrated on one supercontinent.
Yes, there were no ice-ages back then, and significantly less seasonal variance - but this is dependent on the time in question. The entire
Jurassic period (the period between the Triassic and Cretaceous) was universally hot and dry, with a wet season/drought season ratio and aaverage temperature 3 degrees Celsius above our current temperature. The poles were ice-free. The super-continent that you are referring to,
Pangaea, had already broken up 175 million years ago during the
Toarcian stage of the Early Jurassic into the continents of
Gondwana (South America, Africa and India), Antartica-Australia, Eurasia and North America. By the end of the Late Jurassic, the world looked like this:
During Early to mid Cretaceous period (roughly 145 million to 100 million years ago), the world entered one of its hottest periods ever, along with an accompanying humidity caused by a further break-up in continents and lowered sea-levels - leading to a tropical atmosphere. The average temperature was 4-6 degrees higher then the global average today. Seasons began to become apparent, though only in certain latitudes - Antarctica and Australia had drifted into the south pole and became trapped in a winter/summer seasonal cyclic rather reminiscent of today's temperate seasons. Dinosaurs, pterosaurs, early-birds and giant amphibians all lived there as they did for millions of years before. Just Google "Antarctic Dinosaurs".
India here split from Antarctica/Australia and migrated north. Africa and South America also separated, and North America was divided by the
Western Interior Seaway (also known as the Skull Creek Seaway, or Cretaceous Sea) into to two separate landmasses (
Laramidia in the west, and
Appalachia in the east) that throughout the period would join and split more then three times, promoting great evolutionary diversity among the dinosaurs that lived there.
Starting at the
Coniacian stage of the Cretaceous period (89.8 million years to 86.3 years ago) and continuing until the Campanian stage, the sea levels rose and fell, causing some seasonal chaos. Temperatures did rise as far a 8 degrees above the current maximum, and various marine extinctions took place. The dinosaurs endured and flourished. Then, as the Campanian drew to a close and the Maastrichtian stage began, temperatures stabilized, the sea-levels fell again, and an annual season-cycle much like our own now began. No-where could this be seen more vividly then in North America, which now basically resembled our modern understanding of it (most of the other continents were the same in this detail).
Dinosaurs migrated to WELL above the arctic circle, as the
Prince Creek findings prove. Herbivores like duck-bills and horned ceratopsids no doubt sought the rich summer greenery that the temperate seasons provided, with tyrannosaurs and dromaesaurids predators following them.
Okay, I think I've bored you enough - but hopefully you, as well as anyone else who reads this, will gain a better understanding of the complexities of the Mesozoic world.