The vanishing and the establishment of a new ecosystem on an oceanic island - Anthropogenic impacts with no return ticket.

Autor:	Ritter C; CIBIO, Centro de Investigação em Biodiversidade e Recursos Genéticos, InBIO Laboratório Associado, Pólo dos Açores, Rua da Mãe de Deus, 9500-321 Ponta Delgada, Portugal. Electronic address: catarinaritter@hotmail.com., Gonçalves V; CIBIO, Centro de Investigação em Biodiversidade e Recursos Genéticos, InBIO Laboratório Associado, Pólo dos Açores, Rua da Mãe de Deus, 9500-321 Ponta Delgada, Portugal; Faculdade de Ciências e Tecnologia, Universidade dos Açores, Rua da Mãe de Deus, 9500-321 Ponta Delgada, Portugal., Pla-Rabes S; CREAF, Campus de Bellaterra (UAB), Edifici C, 08193 Cerdayola del Valles, Spain; Department of Geography, Environmental Management and Energy Studies, University of Johannesburg, Corner Ditton and University Avenue, Auckland Park, Johannesburg, South Africa., de Boer EJ; UB-Geomodels Research Institute. Department de Dinàmica de la Terra i de l'Oceà, Facultat de Ciències de la Terra, Universitat de Barcelona, Martí i Franquès s/n, 08028 Barcelona, Spain., Bao R; Universidade da Coruña, GRICA Group, Centro de Investigacións Científicas Avanzadas (CICA), Rúa as Carballeiras, 15071, A Coruña, Spain., Sáez A; UB-Geomodels Research Institute. Department de Dinàmica de la Terra i de l'Oceà, Facultat de Ciències de la Terra, Universitat de Barcelona, Martí i Franquès s/n, 08028 Barcelona, Spain., Hernández A; Universidade da Coruña, GRICA Group, Centro de Investigacións Científicas Avanzadas (CICA), Rúa as Carballeiras, 15071, A Coruña, Spain., Sixto M; Centro Oceanográfico de Vigo, Instituto Español de Oceanografía (IEO-CISC), Subida a Radio Faro 50-52, 36390 Vigo, Spain; Campus do Mar, Facultad de Ciencias del Mar, Universidad de Vigo, 36311 Vigo, Spain., Richter N; NIOZ Royal Netherlands Institute for Sea Research, P.O. Box 59, 1790 AB Den Burg, the Netherlands; Department of Earth, Environmental and Planetary Sciences, Brown University, Providence, RI 02912, USA., Benavente M; Geosciences Barcelona (Geo3BCN-CSIC), Lluís Solé i Sabarís s/n, 08028 Barcelona, Spain., Prego R; Department of Oceanography, Marine Research Institute (CSIC), Eduardo Cabello, 6. 36208 Vigo, Spain., Giralt S; Geosciences Barcelona (Geo3BCN-CSIC), Lluís Solé i Sabarís s/n, 08028 Barcelona, Spain., Raposeiro PM; CIBIO, Centro de Investigação em Biodiversidade e Recursos Genéticos, InBIO Laboratório Associado, Pólo dos Açores, Rua da Mãe de Deus, 9500-321 Ponta Delgada, Portugal; Faculdade de Ciências e Tecnologia, Universidade dos Açores, Rua da Mãe de Deus, 9500-321 Ponta Delgada, Portugal.
Jazyk:	angličtina
Zdroj:	The Science of the total environment [Sci Total Environ] 2022 Jul 15; Vol. 830, pp. 154828. Date of Electronic Publication: 2022 Mar 26.
DOI:	10.1016/j.scitotenv.2022.154828
Abstrakt:	A multiproxy approach was applied to a sediment core retrieved from the deep crater Lake Funda, located in the middle of the North Atlantic Ocean on Flores Island, Azores archipelago (Portugal). The purpose of this study was to determine how this ecosystem responded to natural and anthropogenic forces over the last millennium. We distinguished three main phases in lake evolution using multiproxy reconstructions and documentary sources. (A) Climate and lake catchment processes, as well as internal ones, were the main drivers of ecosystem variability before 1335 CE, when human disturbances were absent in the Lake Funda catchment. (B) The second phase is marked by unprecedented changes in all studied proxies between 1335 and 1560 CE, including abrupt changes in the composition and diversity of diatom and chironomid assemblages. Synergistic effects from high climate variability and the onset of human disturbances in the catchment (e.g., introduction of livestock) during the Medieval Climate Anomaly-Little Ice Age transition, led to an increase in lake trophic state from mesotrophic to eutrophic conditions. (C) In the last phase (1560 CE to the present), the eutrophic conditions in Lake Funda were maintained through a positive feedback loop between lake productivity and in-lake phosphorous recycling. Variability within the lake ecosystem was mainly associated with climate variability and internal lake dynamics (e.g., phosphorus remobilization). Our results show that a paleoecological approach is crucial to understanding lake ecological states in the present-day in order to develop locally adapted management and restoration strategies. A long-term perspective enables us to understand the harmful consequences of ongoing climate change and human disturbances on lake ecosystems. Competing Interests: Declaration of competing interest The authors declare that they have no known competing financial interests or personal relationships that could have appeared to influence the work reported in this paper. (Copyright © 2022 The Authors. Published by Elsevier B.V. All rights reserved.)
Databáze:	MEDLINE
Externí odkaz:	Full Text from ScienceDirect