“…In some cases, invasions by less well-preserved taxa can be inferred by tracking the patterns of change in other taxa. For example, the introduction of fish in formerly fishless lakes can be tracked based on the abundance, size and morphology of the invertebrate predator Chaoborus and its prey Bosmina (Labaj et al, 2013). Determining the degree to which biological invasions drive ecosystem change, or are a response to changes driven by other factors such as catchment disturbance, eutrophication or pollution, is an important question for biological invasion science, and one that palaeoecology, with its capacity to extend temporal perspectives, is in a strong position to answer (Kamenova et al, 2017; Willis and Birks, 2006).…”
Section: Anthropogenic Drivers Of Catchment and Lake Changesmentioning
Lake sediments constitute natural archives of past environmental changes. Historically, research has focused mainly on generating regional climate records, but records of human impacts caused by land use and exploitation of freshwater resources are now attracting scientific and management interests. Long-term environmental records are useful to establish ecosystem reference conditions, enabling comparisons with current environments and potentially allowing future trajectories to be more tightly constrained. Here we review the timing and onset of human disturbance in and around inland water ecosystems as revealed through sedimentary archives from around the world. Palaeolimnology provides access to a wealth of information reflecting early human activities and their corresponding aquatic ecological shifts. First human impacts on aquatic systems and their watersheds are highly variable in time and space. Landscape disturbance often constitutes the first anthropogenic signal in palaeolimnological records. While the effects of humans at the landscape level are relatively easily demonstrated, the earliest signals of humaninduced changes in the structure and functioning of aquatic ecosystems need very careful investigation using multiple proxies. Additional studies will improve our understanding of linkages between human settlements, their exploitation of land and water resources, and the downstream effects on continental waters.
“…In some cases, invasions by less well-preserved taxa can be inferred by tracking the patterns of change in other taxa. For example, the introduction of fish in formerly fishless lakes can be tracked based on the abundance, size and morphology of the invertebrate predator Chaoborus and its prey Bosmina (Labaj et al, 2013). Determining the degree to which biological invasions drive ecosystem change, or are a response to changes driven by other factors such as catchment disturbance, eutrophication or pollution, is an important question for biological invasion science, and one that palaeoecology, with its capacity to extend temporal perspectives, is in a strong position to answer (Kamenova et al, 2017; Willis and Birks, 2006).…”
Section: Anthropogenic Drivers Of Catchment and Lake Changesmentioning
Lake sediments constitute natural archives of past environmental changes. Historically, research has focused mainly on generating regional climate records, but records of human impacts caused by land use and exploitation of freshwater resources are now attracting scientific and management interests. Long-term environmental records are useful to establish ecosystem reference conditions, enabling comparisons with current environments and potentially allowing future trajectories to be more tightly constrained. Here we review the timing and onset of human disturbance in and around inland water ecosystems as revealed through sedimentary archives from around the world. Palaeolimnology provides access to a wealth of information reflecting early human activities and their corresponding aquatic ecological shifts. First human impacts on aquatic systems and their watersheds are highly variable in time and space. Landscape disturbance often constitutes the first anthropogenic signal in palaeolimnological records. While the effects of humans at the landscape level are relatively easily demonstrated, the earliest signals of humaninduced changes in the structure and functioning of aquatic ecosystems need very careful investigation using multiple proxies. Additional studies will improve our understanding of linkages between human settlements, their exploitation of land and water resources, and the downstream effects on continental waters.
“…In Pocket Lake, Chaoborus mandibles were recovered in low abundances (less than 10 per interval) throughout the sediment core, including both the pre-, peak and post-mining periods, and no notable changes in biomass or productivity of these macroinvertebrate predators on Daphnia can be inferred in response to metal(loid) contamination. Furthermore, the large-bodied species Chaoborus americanus and Chaoborus trivattatus were recovered throughout, suggesting Pocket Lake has probably always been fishless, as C. americanus is a well-known indicator of fishless (or very low planktivorous fish) conditions, and C. trivattatus, which often coexists with C. americanus, generally dominates in lakes with minimal fish community [70]. The recovery of remains of these taxa at low, but consistent, abundances throughout the sediment core suggests that Pocket Lake has not undergone changes in fish community, and has most probably been fishless over the recent past, including the period of intense contamination from mining operations.…”
Section: R I C O T O P U S P S E C T R O C L a D I U S T A N Y T A mentioning
Giant Mine, located in the city of Yellowknife (Northwest Territories, Canada), is a dramatic example of subarctic legacy contamination from mining activities, with remediation costs projected to exceed $1 billion. Operational between 1948 and 2004, gold extraction at Giant Mine released large quantities of arsenic and metals from the roasting of arsenopyrite ore. We examined the long-term ecological effects of roaster emissions on Pocket Lake, a small lake at the edge of the Giant Mine lease boundary, using a spectrum of palaeoenvironmental approaches. A dated sedimentary profile tracked striking increases (approx. 1700%) in arsenic concentrations coeval with the initiation of Giant Mine operations. Large increases in mercury, antimony and lead also occurred. Synchronous changes in biological indicator assemblages from multiple aquatic trophic levels, in both benthic and pelagic habitats, indicate dramatic ecological responses to extreme metal(loid) contamination. At the peak of contamination, all Cladocera, a keystone group of primary consumers, as well as all planktonic diatoms, were functionally lost from the sediment record. No biological recovery has been inferred, despite the fact that the bulk of metal(loid) emissions occurred more than 50 years ago, and the cessation of all ore-roasting activities in Yellowknife in 1999.
“…Fossil invertebrate remains reveal information about food-web structures, predatorprey dynamics, and they are useful for investigating the influence of invertebrate competition and predation on zooplankton size structure (Alexander and Hotchkiss, 2010). Invertebrate remains have been used to document the presence or absence of fish, often for specific fish families (e.g., Cyprinidae), to identify changes in fish planktivory, and to examine keystone fish predation (Palm et al, 2011;Tolonen et al, 2012;Twining and Post, 2013;Labaj et al, 2013). The use of these fossils to address aquatic trophic-web questions often relies on contemporary limnological information about zooplankton community structure in lakes with and without fish.…”
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