Hi, Cubscout. No, I'm not a student of John's, though he and I are old friends (in both senses of the word old
. I like and respect John, so recently invited him to participate in a National Geographic project that I was putting together, and we enjoyed visiting during the meetings for that project. John and I tend to agree closely on pterosaur aerodynamics and flight mechanics, but not on their morphology. Paul MacCready's take on pterosaurs is more similar to mine than John's is.
John strongly believes that they all had a very broad wing attaching to the ankle and consequently, a relatively low aspect ratio that was best suited for convective lift. Interestingly enough, there's no unambiguous evidence in the fossil record to support that configuration, so his preference is a bit surprising because convective lift is strongest inland, and of the hundreds of species presently known, only a very few were inland feeders -- the overwhelmingly vast majority were marine feeders where convection is weak. A high aspect ratio similar to that of an albatross or frigate bird was more suitable for extracting lift from wave lee shear, dynamic soaring, and the other energy processes available far at sea.
And since none of the preserved pterosaur wing membranes have the trailing edge of the membrane in the vicinity of the elbow located more than 40% of the length of the humerus behind the elbow, it appears that most (if not all) species did indeed have the narrow wing and higher aspect ratio. As an aside, the two types that I spend most of my time on were both inland freshwater feeders that spent most of their time about 200 miles from the nearest seaway. Those two types have been found from the Big Bend country of Southwest Texas north to Alberta far from the shore of the Western Interior Seaway, and the fossil evidence gleaned from their remains strongly implies (but does not prove) that they did not have a wing/hindlimb connection of any sort. They were high aspect ratio types (about 16.5 to 17.1) with wings suited for extracting lift from cloud streets, microturbulence, and the rolls along the lee side of trees and lake banks on the windward side of lakes.