Had a quick read through the five papers. These are my personal highlights, not by any means complete. I still suggest to anyone who's really interested to read the actual papers, they're quite fascinating!
Atmosphere
Near-symmetry between ingress and egress structure
Pressure profile consistent with Earth-based observations
Strong temperature inversion within the first 20 km from the ground with horizontal variations (stronger at ingress, where it goes all the way down to the surface, than egress)
Surface pressure of 9-12 microbar: no big atmospheric mass change in recent years
Air temperature adjacent to surface is 42-48 K, close to saturation temperature of N2
First 1800 km of height are dominated by N2, with abundant minor species (methane, acetylene, ethylene, ethane)
Over 20 haze layers, the most visible of which are at 10, 30, 90 and 190 km from the ground. Haze density near surface is 0.8 particles per centimetre cube
10^23 and 5 x 10^25 molecules of nitrogen and methane are lost due to Jeans escape every second, respectively (146 and 42000 tons a year, if my calculations are correct). If these rates have been constant throughout Pluto's history (which doesn't seem to be the case), Pluto has lost 6 cm of nitrogen and 28 m of methane
Hazes could be due to gravity waves produced via orographic forcing (winds at speeds of <10 m/s blowing across the mountains and being lifted up in the atmosphere)
Interaction with solar wind
Solar wind speed is 403 km/s. Very high density and pressures are likely due to a strong interplanetary shock that was felt by New Horizons 5 days prior to flyby
Measurements at 20 RP (Plutonian radii) inbound show the solar wind is not slowing down (<1%), suggesting no pickup of heavy ions and therefore that few atmospheric molecules are escaping upstream and becoming ionized
At 9.6 RP behind Pluto (tailward), solar wind is slowed by 20% according to SWAP, and PEPSSI detects an enhancement of keV ions
This suggests the region of Pluto-Sun interaction extends >400 RP tailward but only 6 RP upstream. However, considering probable compressed state of this region at the moment of flyby, it is likely that it usually extends up to 25 RP upstream
Dust counter (SDC) detected 102 events between 5 days prior to flyby and 5 days after flyby, however only one is very likely (95%) to be a dust impact
Considering SDC carved 0.83 km^3 during this period, the resulting density of dust is one particle every 1.2 km^3, slightly more than what was observed in the previous months leading to flyby
SDC detects grains bigger than 1.4 micrometers
Geology
Sputnik Planum covers 870,000 km^2 and is 3-4 km below surrounding uplands. It is fragmented in a cellular pattern in its central and northern parts, with each cell separated by 100 m-deep troughs and with the centres of the cells being on average 50 m above the edges
The other half of Tombaugh Regio (i.e. the eastern part) is 2-4 km above Sputnik Planum and is populated by many pits (sublimation?), with depths of 1 km and diameters of up to 25 km. 1.5-6 km wide troughs contain glacial flows towards Sputnik Planum
Crater sizes range from 0.5 to 250 km
Globally, the surface dates back to epoch of gas giant migration (4 bln years ago), except for Tartarus Dorsa, mountain ranges and Sputnik Planum
Sputnik Planum has no crater > 2 km, suggesting it's <10 million years old. However, its basin (perhaps an impact crater) is likely very ancient and modified
Two quasi-circular mounds (Wright and Piccard Monts) to the south of Sputnik Planum are likely cryovolcanoes. They are 4-6 km high and 150-225 km wide
Charon's northern terrains are networks of polygonal troughs 3-6 km deep; the southern terrains are smoother plains, possibly hinting to tectonic resurfacing, with fields of small hills and less crater which hint at cryovolcanic resurfacing
Overall, Charon is very different from Pluto, not showing signs of volatile transport (except possibly for Mordor Macula). Maybe the volatiles were lost to space due to the lower gravity?
Pluto's activity can be explained by atmosphere-surface interaction, volatile mobility, radiogenic heat. However, youngness of mountain chains and possible cryovolcanoes is mysterious
Composition
Main ices are: N2, CO (very volatile) and CH4 (less volatile), which act like Earth snow even at Pluto's frigid 35-50 K. Other ices include water (which, being very rigid at such low temperatures, is the bedrock on which the other ices flow, sublimate and condense, and also makes up most of the mountains), C2H6 and NH3, plus obviously non-volatile tholins.
Sputnik Planum features all three of the main ices, but no water ice. The three ices are all soluble in each other to an extent, so they are likely mixed at a molecular level
CH4 is found in Sputnik Planum, crater rims and pathces in northern mid-latitudes
N2 is found in Sputnik Planum, crater floors and none in the high northern latitudes (which have been in constant sunlight since the '80s, so any N2 there is likely to have sublimated long ago
Sputnik Planum is continuously refreshed by glacial flows, possibly powered by convective overturning
Four major global albedo units are evident: low equatorial regions (Cthulhu Regio, Krun Macula), northern summer polar region (Lowell Regio), sliver of southern winter hemisphere, and high-albedo Tombaugh Regio. Darkest equatorial regions have albedos similar to some outer solar system moons rich in carbonaceous or organic materials (Hyperion, Phoebe, Umbriel)
Albedo interacts with composition: high-albedo regions absorb more sunlight, driving sublimation
Charon is made predominantly of water ice, partially in crystalline phase
Minor Moons
All four are highly elongated objects
Their very high albedos (56-83%, approx. 6-8x brighter than a typical KBO) mean they are unlikely to be captured KBO objects. Also, their albedos suggest they are rich in water ice
Their highly asymmetrical shapes (see double-lobed Kerberos) suggest a growth process by agglomeration of small objects into single, loosely bound, macroporous bodies, which in turn is consistent with formation within the remnant disk of the Pluto-Charon-forming collision
The abundance of water ice suggests the two parents of Pluto and Charon were at least partially differentiated on the inside, with icy surfaces
Crater counts (11 on Nix, 3 on Hydra) lead to densities equal or great than the ones of Pluto's oldest surfaces (i.e. they are >4 bln years old)
Regolith sharing between moons is less extensive than thought
Surfaces are mostly greish (neutral in color), except for a reddish crater on Nix, implying different composition either in the impacting body or in the moon's subsurface layers, excavated by the impact
Sorry for the long post -- hope it helps!