RT info:eu-repo/semantics/article
T1 Paleo-watertable definition using cave ferromanganese stromatolites and associated cave-wall notches (Sierra de Arnero, Spain)
A1 Rossi, Carlos .
A1 Villalaín Santamaria, Juan José
A1 Lozano, Rafael P. .
A1 Hellstromd, John .
K1 Speleogenesis
K1 Karst
K1 Paleo-watertable
K1 Cave stromatolites
K1 Paleomagnetism
K1 U-series dating
K1 Physics
K1 Paleontology
K1 Física
K1 Paleontología
AB The steeply-dipping-dolostone-hosted caves of the Sierra de Arnero (N Spain) contain low-gradient relict canyons with up to ten mapped levels of ferromanganese stromatolites and associated wall notches over a vertical range of 85 m, the highest occurring ~ 460 m above base level. Despite a plausible speleogenetic contribution by pyrite oxidation, and the irregular cave-wall mesomorphologies suggestive of hypogenic speleogenesis, the Arnero relict caves are dominantly epigenic, as indicated by the conduit pattern and the abundant allogenic sediments. Allogenic input declined over time due to a piracy-related decrease in the drainage area of allogenic streams, explaining the large size of the relict Arnero caves relative to the limited present-day outcrop area of the karstified carbonates. Allogenic-sediment input also explains the observed change from watertable canyons to phreatic conduits in the paleo-downstream direction. Stromatolites and notches arguably formed in cave-stream passages at the watertable. The best-defined paleo-watertables show an overall slope of 1.7°, consistent with the present-day relief of the watertable, with higher-slope segments caused by barriers related to sulfide mineralization. The formation of watertable stromatolites favored wall notching by the combined effect of enhanced acidity by Mn–Fe oxidation and shielding of cave floors against erosion. Abrasive bedload further contributed to notch formation by promoting lateral mechanical erosion and protecting passage floors. The irregular wallrock erosional forms of Arnero caves are related partly to paragenesis and partly to the porous nature of the host dolostones, which favored irregular dissolution near passage walls, generating friable halos. Subsequent mechanical erosion contributed to generate spongework patterns. The dolostone porosity also contributes to explain the paradox that virtually all Arnero caves are developed in dolostone despite being less soluble than adjacent limestone. U-series dating of carbonate speleothems and paleomagnetic data from ferromanganese stromatolites and clastic sediments indicate that the paleo-watertables recorded ~ 320 m above the present-day watertable formed during the Matuyama Chron but prior to ~ 1.5 Ma, implying long-term base-level-lowering rates from ~ 125 to ~ 213 m/Ma. To our knowledge, this is the first attempt of paleomagnetic dating of cave ferromanganese stromatolites. These deposits are excellent geomagnetic recorders and offer a direct way to delineate and date paleo-watertables, especially in caves developed in dolostone.
PB Elsevier
SN 0169-555X
YR 2016
FD 2016-05
LK http://hdl.handle.net/10259/4589
UL http://hdl.handle.net/10259/4589
LA eng
NO Financial support was provided by grants ICT-Soplao-53.5.00.12.00(IGME - Provincial Government of Cantabria - Turismo del Nansa) andCGL2012-38481 (Ministerio de Economía y Competitividad - EuropeanRegional Development Fund)
DS Repositorio Institucional de la Universidad de Burgos
RD 21-nov-2024