We discuss the mechanisms leading to nutrient limitation in tropical marine
systems, with particular emphasis on nitrogen cycling in Caribbean ecosyst
ems. We then explore how accelerated nutrient cycling from human activities
is affecting these systems.
Both nitrogen and phosphorus exert substantial influence on biological prod
uctivity and structure of tropical marine ecosystems. Offshore planktonic c
ommunities are largely nitrogen limited while nearshore ecosystems are larg
ely phosphorus limited. For phosphorus, the ability of sediment to adsorb a
nd store phosphorus is probably greater for tropical carbonate sediments th
an for most nearshore sediments in temperate coastal systems. However, the
ability of tropical carbonate sediments to take up phosphorus can become sa
turated as phosphorus loading from human sources increases. The nature of t
he sediment, the mixing rate between nutrient-laden runoff waters and nutri
ent-poor oceanic waters and the degree of interaction of these water masses
with the sediment will probably control the dynamics of this transition.
Nearshore tropical marine ecosystems function differently from their temper
ate counterparts where coupled nitrification/denitrification serves as an i
mportant mechanism for nitrogen depuration. In contrast, nearshore tropical
ecosystems are more susceptible to nitrogen loading as depurative capacity
of the microbial communities is limited by the fragility of the nitrificat
ion link. At the same time, accumulation of organic matter in nearshore car
bonate sediments appears to impair their capacity for phosphorus immobiliza
tion. In the absence of depurative mechanisms for either phosphorus or nitr
ogen, limitation for both these nutrients is alleviated and continued nutri
ent loading fuels the proliferation of nuisance algae.