RT Journal Article
T1 The influence of subaquatic springs in lacustrine sedimentation: Origin and paleoenvironmental significance of homogenites in karstic Lake Banyoles (NE Spain)
A1 Morellón Marteles, Mario
A1 Anselmett, Flavio S.
A1 Valero-Garcés, Blas
A1 Giralt, Santiago
A1 Ariztegui, Daniel
A1 Sáez, Alberto
A1 Mata, M. Pilar
A1 Barreiro-Lostres, Fernando
A1 Mayte Rico, Mayte
A1 Moreno Bofarull, Ana
AB Banyoles (42°08′N, 2°45′E) is the largest and deepest lake of karstic–tectonic origin in the Iberian Peninsula. The lake comprises two basins and six sub-circularly shaped sub-basins fed by subaquatic springs. Periods of intense groundwater inflow in the deepest sub-basins lead to the fluidization and re-suspension of previously deposited sediments and subsequent settling forming homogenite deposits on the southern basin intermediate platforms. The multiproxy analysis of sediment cores combined with high resolution seismic stratigraphy (3.5 kHz pinger and multi-frequency Chirp surveys) allows a precise reconstruction of depositional environments and related hydrological variability and groundwater inflow during the last ca. 7.6 cal kyr BP. According to the age model based on 137Cs, 210Pb and AMS 14C dating, homogenite deposition occurred between 7.2 and 5.5 cal kyr BP, stopped during the middle Holocene (5.5–2.8 cal kyr BP) and greatly increased during the last two millennia with a total of 17 homogenite layers individually up to 75 cm-thick. The onset of this unique sedimentation mode at ca. 3 cal kyr BP coincides with an increase in lake level, evidenced by the onlapping of fine-grained, distal sediments over coarser massive, carbonate-rich, littoral deposits. A detailed, multidisciplinary study of the homogenites (sedimentology, physical properties, high-resolution elemental geochemistry, mineral composition, grain-size, organic matter content and SEM) combined with seismic stratigraphy demonstrates that the fluidization events triggering the formation of the homogenites were caused by higher and more intense local groundwater inflow, related to increased rainfall during the Late Holocene and likely intensified by land use changes during the last millennium.
PB Elsevier
SN 0037-0738
YR 2014
FD 2014-08
LK https://hdl.handle.net/20.500.14352/34311
UL https://hdl.handle.net/20.500.14352/34311
LA eng
NO Ministerio de Economía y Competitividad (MINECO)
NO Universidad de Barcelona
NO Consejo Superior de Investigaciones Científicas (CSIC)
DS Docta Complutense
RD 23 abr 2025