First of all: Landing in an ocean has its benefits. The biggest one is clearly, that water is 'soft' in contrast to solid land (by being less dense and quite fluid in contrast to rigid crystals of rock), giving way quite easily on a hard impact and thus allowing a higher landing speeds without ripping the ship apart. However, decellerating to a 'reasonable' speed of maybe 30 to 40 feet per second like the Apollo is still very much advised. The latest land-landing Soyuz TMA only makes a touchdown at less than 5 feet per second. Being allowed a splashdown velocity of factor 6 to 8 larger than for a ground impact will seriously help in emergency landings (and is already doing so for airplanes).
Also, sealing the ship airtight to sustain space means, you made it watertight the same moment. Just keeping the overall density below 1 ton/m³ (density of water) by having enough hollow space in walkways and labs and the whole thing will float.
As a bonus, the ocean could cool the heated hull of the ship after reentry, especially if the atmosphere is very dense or the reentry very fast and thus aerobreaking heats up the ship quite much in the lower atmosphere.
However, landing is easy, as a ship just has to make sure of 3 things: not burn up in the atmosphere, not get crushed on impact and don't break your cargo on landing. Placing the landing in the ocean serves 2 of those targets, as shown above.
So, we landed. Landing obviously comes at a cost: you go deep into the gravity well of the planet, so you have to overcome it again to get away again. To do so, you need to go to escape velocity, which is:
$v_e=\sqrt{\frac{2GM}{r}}$
In this $G = 6.67×10^{−11} \frac{m^2}{kg \times s^2}$, M the planetary mass, r the position the ship rests at, so normal nill, which is usually the water level. Now, accelerating from rest to that speed is usually fatal (in case of earth: 11.2 km/s!), but one can use a trick: accalerate over time and go up on the way, and as you go up, reduce also the needed escape velocity. Just make sure to accelerate enough over time. This is what rockets do. Now, we parked our ship in the ocean — where do we get fuel from to reaccelerate up and away?!
Luckily, the basic answer is pathetically easy: from the ocean itself! The most simple rocket fuel is $2H_2+O_2=2H_2O$, which is a highly exothermic reaction. To get to the needed Oxygen and Hydrogen, one can simply crack the water, for example with a battery or by applying the current from solar panels or the ship's reactor. With a bit work on the hydrogen, it can be refined to even better storeable fuels, such as Hydrazine ($N_2H_4$).
However, we still should get to at least a shallow spot to launch our spaceship: our engines may not be submerged to burn our fuel and the acceleration of the initial blastoff is much more effective if the exhaust gases get propelled downwards and it is pretty hard to keep the exhausts facing downwards and out of the water while floating.
To launch from shallow water, having launch-legs would be a good feature, errecting the ship to launch position and retracting in flight. To launch floating, retractable legs with pontons/floaters at the end that do the same and get the engines over the sea surface would be needed.