Little is known about the influence of nanoconfinement on calcium carbonate mineralization. Here, colloidal probe atomic force microscopy is used to confine the calcite-solution interface with a silica microsphere and to measure Derjaguin-Landau-Verwey-Overbeek (DLVO) and non-DLVO forces as a function of the calcium concentration, also after charge reversal of both surfaces occurs. Through the statistical analysis of the oscillatory component of a strong hydration force, the subnanometer interfacial structure of the confined atomically flat calcite is resolved in aqueous solution. By applying a mechanical work, both water and hydrated counterions are squeezed out from the nanoconfined solution, leaving the calcite surface more negatively charged than the analogous unconfined surfaces. Layer size and applied work allow a distinction between the hydration states of the counterions in the Stern layer; we propose counterions to be inner-and outer-sphere calcium ions, with a population of inner-sphere calcium ions larger than on unconfined calcite surfaces. It is also shown that the composition of the nanoconfined solution can be tuned by varying calcium concentration. This is a fundamental study of DLVO and hydration forces, and of their connection, on atomically flat calcite. More broadly, our work scrutinizes the greatly unexplored relation between surface science and confined mineralization, with implications for diverse areas of inquiry, such as nanoconfined biomineralization, CO 2 sequestration in porous aquifers, and pressure solution and crystallization in confined hydrosystems.calcite | hydration forces | DLVO theory | nanoconfinement | atomic force microscopy U nderstanding the effect of nanoconfinement on the solution composition near the calcite surface is crucial in revealing the mechanisms of biomineralization in confinement, because the confined thin film of aqueous electrolyte, which provides the path for ions and water to the buried mineral interface, can behave totally different from the unconfined (free) solution.Whereas the effect of confinement on the properties of the calcite-solution interface is largely unexplored, the Stern layer of unconfined calcite surfaces has been intensively investigated via simulations and experiments. Interestingly, Ca 2+ and CO 3 2− (and HCO 3 − ) ions are not adsorbed directly to calcite but to surfaceadsorbed water molecules as outer-sphere species (OS) due to calcite's strong affinity to water (1). X-ray reflectivity studies (2, 3) and molecular dynamics (MD) simulations (4) have proved that the calcite-solution interface is well defined by two layers of water molecules. Hence, instead of the conventional model, where the Stern layer is adjacent to the charged surface, calcite's Stern layer, the compact layer of counterions, is believed to be located on top of two water layers: OS calcium (OS-Ca 2+ ) ions mainly populate the interface at ∼4.9 Å from the unconfined calcite surface, whereas the population of inner-sphere calcium (IS-Ca 2+ ) ions is located at ∼3.3 Å...