The Amazon shelf–offshore continuum is a dynamic biogeochemical hotspot of the tropical Atlantic, where river discharge, ocean circulation, and strong tides interact to shape nutrient and phytoplankton distributions. The Amazon plume and regional circulation have been widely studied and are known to strongly influence nutrient availability and biological productivity in this region. However, shelf-break tides remain an overlooked pathway linking physical energy to offshore fertilization, and their contribution to seasonal and intraseasonal biogeochemical variability remains unclear. Here, we quantify how tidal dynamics, including internal tides, modulate nitrate supply and chlorophyll distributions from the Amazon shelf to offshore waters. We use a high-resolution coupled physical–biogeochemical model (1/36°), evaluated against climatological, satellite, and in situ observations. The model reproduces the main observed patterns of surface nitrate and chlorophyll, as well as key vertical features such as the nitracline and the deep chlorophyll maximum. We show that tides strongly enhance upward nitrate transport, increasing surface nitrate by more than 50% over the northern shelf, along the shelf break, and within the main internal-tide pathway. This tidally supplied nitrate fuels offshore phytoplankton growth, increasing chlorophyll by about 15–50%, while reducing surface chlorophyll near the Amazon mouth by 30– 40%.Seasonally, surface chlorophyll and nitrate are higher over the Amazon shelf during April–June but lower offshore, revealing a marked cross-shelf contrast. When the tidal contribution is isolated, a similar but weaker spatial structure 30 emerges, with a cone-shaped chlorophyll anomaly extending from the shelf break toward the offshore internal-tide propagation region. Remarkably, tides account for about 63% of the total seasonal variability in surface nitrate, meaning that tidal forcing alone explains more than half of the seasonal nutrient signal. At intraseasonal timescales, tides generate a clear spring–neap rhythm of about 15 days in both nitrate and chlorophyll. This spring–neap tidal pulse propagates from the shelf break toward offshore waters and is especially pronounced near the deep chlorophyll maximum, where oscillations of the upper nitracline periodically modulate nitrate availability and drive a corresponding chlorophyll response., where chlorophyll variability is nearly doubled when tides are included. The concurrent increase in nitrate variability indicates that this spring–neap phytoplankton response is sustained by tidally driven nutrient supply. These findings identify internal tides as a key biogeochemical driver of the Amazon shelf–offshore continuum, linking tidal energy to nutrient injection, offshore fertilization, seasonal redistribution, and rhythmic ecosystem variability in the western tropical Atlantic.