Biogeochemical Responses to Holocene Catchment-Lake
Journal of Geophysical Research: Biogeosciences RESEARCH ARTICLE Biogeochemical Responses to Holocene Catchment-Lake 10.1029/2017JG004136 Dynamics in the Tasmanian World Key Points: Heritage Area, Australia • Aquatic dynamics at Dove Lake are modulated by climate- and fire-driven Michela Mariani1 , Kristen K. Beck1 , Michael-Shawn Fletcher1 , Peter Gell2, terrestrial vegetation changes 3 3 3 • A period of high rainforest cover Krystyna M. Saunders , Patricia Gadd , and Robert Chisari prior ca. 6 ka is linked to changing 1 2 dystrophic conditions, lower light School of Geography, University of Melbourne, Parkville, Victoria, Australia, Faculty of Science and Technology, penetration depths, and anoxic Federation University, Mt Helen, Victoria, Australia, 3Australian Nuclear Science and Technology Organization, Lucas conditions in the lake bottom waters Heights, New South Wales, Australia • Increasing sclerophyll cover after ca. 6 ka is associated with lower nutrient input, lower dystrophy, more oxic Abstract Environmental changes such as climate, land use, and fire activity affect terrestrial and aquatic conditions, and higher light availability for aquatic organisms ecosystems at multiple scales of space and time. Due to the nature of the interactions between terrestrial and aquatic dynamics, an integrated study using multiple proxies is critical for a better understanding of fi Supporting Information: climate- and re-driven impacts on environmental change. Here we present a synthesis of biological and • Figure S1 geochemical data (pollen, spores, diatoms, micro X-ray fluorescence scanning, CN content, and stable isotopes) from Dove Lake, Tasmania, allowing us to disentangle long-term terrestrial-aquatic dynamics Correspondence to: through the last 12 kyear. We found that aquatic dynamics at Dove Lake are tightly linked to vegetation shifts M.
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