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Título

Disentangling the geologic, human and climate drivers influencing sediment deposition in volcanic lakes on the Azores Archipelago

AutorBenavente-Marín, Mario CSIC ORCID ; Hernández, Armand CSIC ORCID ; Sáez, Alberto; Raposeiro, Pedro M.; Gonçalves, Vítor; Pla-Rabes, Sergi CSIC ORCID; Bao, Roberto; Andrade, Mariana; Richter, Nora; Ritter, Catarina; Prego, R. CSIC ORCID ; Ruiz-Fernández, Ana Carolina; Sanchez-Cabeza, Joan-Albert; Trigo, Ricardo M.; Viaplana-Muzas, Marc; Giralt, Santiago CSIC ORCID
Fecha de publicación2022
CitaciónIAL-IPA 2022 Joint Meeting (2022)
ResumenThe Azores Archipelago Western (AAWG) and Central (AACG) groups present a high diversity of tectono-volcanic settings, and, therefore, a wide range of lake-watershed system morphometries. This archipelago has suffered from anthropic impacts, mainly abrupt land-use changes, since medieval times (between 700 and 850 CE), and increasingly after the Portuguese arrival in the 15th century. In this complex geologic and human context, we used a multiproxy approach in sediment records from Lakes Caldeirão (Corvo Island), Funda (Flores Island), and Caveiro (Pico Island) to demonstrate a complex interlinking among several environmental drivers over the last millennia. Paleoenvironmental changes have been defined by a multivariate analysis of sedimentary facies, biogeochemical and mineralogical data. This analysis highlights that the most prominent sedimentary process in the AAWG lakes (Caldeirao and Funda) is hydrological grain size sorting, driven by runoff. Additionally, smooth catchment slopes of the low-gradient lake, Caldeirão, modulated this process by favouring rock grain size diminution through weathering, whereas the steep topographic-bathymetric profile of the high-gradient lake, Funda, do through water-level fluctuations. The frequent volcanic activity of the AACG and the small size of Caveiro lake catchment favoured the deposit of pyroclastic tephra through direct fallout in the lake, over the catchment-sourced inputs, reworked by climate and tectonic activity. The biogeochemical and mineral composition of the sedimentary records present extreme change rates at 1288+28-22-1388+41-32 CE, corresponding with the age of the most intense landscape transformation. Therefore, to obtain robust climate reconstructions from these Azorean lacustrine records, we present a detailed statistical approach to isolate the climate signal from volcano-tectonic, morphometric, and anthropic drivers
DescripciónIAL-IPA joint meeting "Lakes as Memories of the Landscape", Patagonia, Argentina, 27 November-01 December 2022
URIhttp://hdl.handle.net/10261/307416
Aparece en las colecciones: (IIM) Comunicaciones congresos




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