Even though Patagonia is ideally located to study climate of the southern mid-latitudes,
many questions on the late Quaternary climate evolution remain unresolved. The timing of …

This paper reviews published geochronological data on glacier fluctuations and
environmental changes in central Patagonia (44° S-49° S) from the Last Glacial Maximum …

Grain size is one of the most fundamental properties of sediments. It is frequently used in
paleoclimate, paleoceanographic, and paleoenvironmental research as a proxy for river …

Glaciated environments have been highlighted as important sources of bioavailable
nutrients, with inputs of glacial meltwater potentially influencing productivity in downstream …

Abstract Changes may be occurring in the carbonate chemistry of fjords due to natural and
anthropogenic disturbance of major freshwater sources. We present a high‐frequency time …

Despite the importance of silicon (Si) as benefecial nutrient for many plants, including
economically-important cereals, the reactivity of various Si pools in soils (silicate minerals …

The formation of chemical and biological heterogeneity in lakes can be favored by physical
and morphometric constrains. This study describes the results of four whole-lake field …

This study investigates the immediate and mid-term effects of the biogeochemical variables
input into the Reloncaví fjord (41° 40′ S; 72° 23′ O) as a result of the eruption of Calbuco …

Fjords are increasingly recognized as hotspots for organic carbon (OC) burial. The OC
buried in fjords is of both marine and terrestrial origin, with a predominance of terrestrial OC …

The ability to trace and quantify sediment provenance in northwestern Patagonia is
increasingly needed to properly understand modern sediment erosion and transport …