Abstract
Abstract. Present-day lake water phosphorus (P) enrichment and accelerated P cycling are changes superimposed on a dynamic Holocene history of landscape development following glaciation, changes in climate, and long-term low-intensity human activity. Knowledge of the history of long-term P dynamics is essential for understanding present-day landscape P export and for managing both terrestrial and aquatic environments. This study is the first attempt to constrain the timing and magnitude of terrestrial changes in Holocene P dynamics across the Northern Hemisphere using lake sediment records. Here we reconstruct trajectories in terrestrial Holocene P dynamics for the Northern Hemisphere. We apply a simple process model to published lake sediment geochemical P records from 24 sites, producing records of landscape P yield and reconstructing lake water total phosphorus (TP) concentrations. Individual site trajectories of landscape P yield and lake water TP vary systematically, with differences attributable to local landscape development history. Three distinct traits are apparent. Mountain sites with minimal direct human impact show falling P supply and conform to conceptual models of natural soil development (Trait 1). Lowland sites where substantial (pre-)historic agriculture was present show progressively increasing P supply (Trait 2). Lowland sites may also show a rapid acceleration in P supply over the last few centuries, where high-intensity land use, including settlements and farming, is present (Trait 3). Where data availability permitted comparison, our reconstructed TP records agree well with monitored lake water TP data, and our sediment-inferred P yields are comparable to reported catchment export coefficients. Comparison with diatom-inferred TP reveals good agreement for recent records. Our reconstructions form the first systematic assessment of average terrestrial P export for the Northern Hemisphere over the Holocene and provide the empirical data needed for constraining long-term landscape P cycling models and values for terrestrial P export that could be used for ocean P cycling models. The long-term perspective provided by our sediment-inferred TP can be used to identify pre-disturbance baselines for lake water quality, information essential to target-driven lake management. We find the first detectable anthropogenic impacts on P cycling ca. 6000 BP, with more substantial impacts as early as 3000 BP. Consequently, to characterize pre-disturbance lake P conditions at Trait 2 and Trait 3 sites, it is necessary to consider time periods before the arrival of early farmers. Our use of trait classifications has a predictive power for sites without sediment records, allowing prediction of TP baselines and P trajectories based on regional landscape development history.
Highlights
Present-day lake water phosphorus (P) enrichment and accelerated P cycling are changes superimposed on a dynamic Holocene history of landscape development following glaciation, changes in climate, and long-term low-intensity human activity (Boyle et al, 2015; Filippelli and Souch, 1999)
Recent moves to mitigate the effects of anthropogenic nutrient enrichment on lakes, through the identification of lake water total phosphorus (TP) reference conditions and targets, require a thorough quantitative knowledge of this dynamic past, because lake P availability depends on the terrestrial P cycle
Using published sediment P records from 24 lakes distributed across the Northern Hemisphere, we apply the SI-TP model (Moyle and Boyle, 2021), a simple process model, to generate Holocene records of long-term average lake water TP concentration and landscape P yield
Summary
Present-day lake water phosphorus (P) enrichment and accelerated P cycling are changes superimposed on a dynamic Holocene history of landscape development following glaciation, changes in climate, and long-term low-intensity human activity (Boyle et al, 2015; Filippelli and Souch, 1999). M. Moyle et al.: Holocene P dynamics for the Northern Hemisphere palaeolimnology is to provide accurate histories of catchment P yield and lake water TP. Reconstructed P yield records have application beyond limnology They can provide the empirical data needed for constraining long-term landscape P cycling models. Values for terrestrial P export are applied to ocean biogeochemical models and are currently supplied by riverine data which lack the long-term (millennial) temporal perspective of lake sediment P yield records (Sharples et al, 2017)
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