Lake Pavin History, geology, biogeochemistry, and sedimentology of a deep meromictic maar lake

356 not compare the relationship between number of fi sh released and number caught without estimating the theoretical sur- viva ...

357 misunderstanding with the people responsible for carrying out the work, individuals got tagged several consecutive years wit ...

358 The 2012 study by the ONEMA (Olivier 2012 ) shows: a numerical distribution dominated by three species: European perch (42 ...

359 Underwater photos taken by the Arvernes Diving Club (D Chassain) show a change in bottom conditions in the breeding grounds. ...

360 This tagging program will also allow us to assess the annual growth of released individuals. 21.5.3 Implementation of Incu ...

361 It is hoped that the trend monitoring does not just show a slow and infl exible degradation of the lake quality and tro- phi ...

P a r t V Sedimentology and Paleolimnology Emmanuel Chapron http://www.ebook3000.com ...

© Springer International Publishing Switzerland 2016 365 T. Sime-Ngando et al. (eds.), Lake Pavin, DOI 10.1007/978-3-319-39961-4 ...

366 suggest that maar lakes from the study area are concerned by subaquatic slope stabilities, especially in Lake Pavin were slo ...

367 22 m deep and consist in two coalescing small maars damned by the Montcineyre scoria cone and lava fl ow which developed sho ...

368 Lake Pavin sedimentary environments, in particular because it clearly illustrates the development of a subaquatic plateau be ...

369 60 m -30 m -30 m -20 m -40 m littoral facies Pavin crater formation multiple WE a b c d W E multiple Pavin crater formatio ...

370 more precisely the subaqueous geomorphology of this maar lake. 22.2.2 Short Sediment Cores Based on Lake Pavin multibeam bat ...

371 dure described in Behar et al. ( 2001 ) and Simonneau et al. ( 2014 ). 22.3 Signatures of Littoral Environments in Lakes Pav ...

372 10 −5 SI) and labeled E2, E3 and E4. Below, Unit B is, on the contrary, a dark brownish massif unit with lower MS values and ...

373 s CHA13 7B CHA13-4 CHA13-6 LITTORAL s BASIN BASIN 0 40 80 120 Magnetic susceptibility (10-5 SI) Spectral map d405 d695 0155 ...

374 organic matter essentially of algal origin developing a strati- fi ed sedimentary unit along the gentle slopes of Lake Pavin ...

375 22.5 Sedimentary Environments in the Deep Central Basins of Lakes Chauvet and Pavin 22.5.1 Lake Chauvet Basin The deep centr ...

376 turbidity current (Mulder and Cochonat 1996 ; Chapron et al. 2006 ; St-Onge et al. 2012 ). Sedimentary facies retrieved in c ...

377 profi les illustrated in Fig. 22.6 , it is also possible to identify that the turbidite associated with E1 essentially remol ...