Abstract

AbstractRecent cyanobacterial blooms in otherwise unproductive lakes may be warning signs of impending eutrophication in lakes important for recreation and drinking water, but little is known of their historical precedence or mechanisms of regulation. Here, we examined long‐term sedimentary records of both general and taxon‐specific trophic proxies from seven lakes of varying productivity in the northeastern United States to investigate their relationship to historical in‐lake, watershed, and climatic drivers of trophic status. Analysis of fossil pigments (carotenoids and chlorophylls) revealed variable patterns of past primary production across lakes over two centuries despite broadly similar changes in regional climate and land use. Sediment abundance of the cyanobacterium Gloeotrichia, a large, toxic, nitrogen‐fixing taxon common in recent blooms in this region, revealed that this was not a new taxon in the phytoplankton communities but rather had been present for centuries. Histories of Gloeotrichia abundance differed strikingly across lakes and were not consistently associated with most other sediment proxies of trophic status. Changes in ice cover most often coincided with changes in fossil pigments, and changes in watershed land use were often related to changes in Gloeotrichia abundance, although no single climatic or land‐use factor was associated with proxy changes across all seven lakes. The degree to which changes in lake sediment records co‐occurred with changes in the timing of ice‐out or agricultural land use was negatively correlated with the ratio of watershed area to lake area. Thus, both climate and land management appeared to play key roles in regulation of primary production in these lakes, although the manner in which these factors influenced lakes was mediated by catchment morphometry. Improved understanding of the past interactions between climate change, land use, landscape setting, and water quality underscores the complexity of mechanisms regulating lake and cyanobacterial production and highlights the necessity of considering these interactions—rather than searching for a singular mechanism—when evaluating the causes of ongoing changes in low‐nutrient lakes.

Highlights

  • Eutrophication and phytoplankton blooms are commonly identified as primary concerns in aquatic systems (Carpenter et al 1998)

  • We investigated whether variation among lakes in the answers to these questions was related to watershed and lake morphometry

  • Relationship to watershed and bathymetric characteristics.—we examined whether the degree of similarity in zone breaks across proxies was related to watershed and bathymetric

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Summary

Introduction

Eutrophication and phytoplankton blooms are commonly identified as primary concerns in aquatic systems (Carpenter et al 1998). It is well documented that both nutrient loading from watersheds and warmer conditions favor phytoplankton growth and, in eutrophic lakes, the development of extensive cyanobacterial blooms (Brookes and Carey 2011). These blooms negatively impact recreation, property values, drinking water, and the health of people, domesticated animals, and wildlife (Walker et al 2008, Dodds et al 2009, Carmichael and Boyer 2016, Mueller et al 2016). Even lakes in close proximity may exhibit asynchronous patterns of change in the abundance of phytoplankton species due to sitespecific differences in chemistry or morphometry that control the abundance of cyanobacteria (Patoine and Leavitt 2006) or the ways climate impacts lakes (Moorhouse et al 2018)

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