Phytoplankton production in the North Atlantic peaks in the spring and mostly comes to a halt in the winter. In the North Pacific, plankton production occurs throughout the winter months. This difference in productivity between the North Atlantic and Pacfic is due to: Group of answer choices

sunlight availability

salinity of the mixed layer

different species of plankton

thermocline

Atp is is our little "pocket" of energy. of course, if you have too little, then it means you have too little energy, and you'll pass out. the way to not have enough, is to have no energy sources (glucose, fats, proteins). you can't have too many atp molecules. cycles like the krebs cycle produce it, but if you have too much of any substrate (or too little for that matter), the cycle stops and atp is no longer made (it stops until substrate levels are such that the process can go on). in any case, this is unlikely since atp is constantly hydrolyzed and remade, even while you're asleep. you won't have too much. if you have zero, you are dead or dying.

Passive transport of the bag, quavo once said "you get the bag and fumble it, i get the bag, flip it, and tumble it". but the answer could either be quavo, offset, or, takeoff.