Not in a million years!
Subaqueous eruptions lead to a range of obvious macro-and micro-scale features that are not generally observed on Mars:-
1) Pillow Basalts - blobs and tubes of lava, rather than sheets as in subaerial eruptions
2) Hyaloclastics - vast amounts of shattered volcanic glass
3) Very fine crystal size
4) Tuya geometry of volcanoes (steep-sided mounds with much flatter tops representing the submarine and subaerial components)
With the exception of some work by Mary Chapman showing Tuya-like features within the enclosed rifts of Vallis Marineris, none of these diagnostic signs are found on Mars or seen in Mars meteorites.