Characterization and Management of Natural Resources

2020

Underground Flash Flood Events

Watlet A, Camp MV, Francis O, Poulain A, Rochez G, Hallet V, Quinif Y, Kaufmann O. 2020. Gravity Monitoring of Underground Flash Flood Events to Study Their Impact on Groundwater Recharge and the Distribution of Karst Voids. Water Resources Research 56:e2019WR026673. DOI: 10.1029/2019WR026673.

Flash flood events are expected to become increasingly common with the global increases in weather extremes. They are a significant natural hazard that affects karst landscapes, which host large resources of drinking water worldwide. This study analyses 20 incave flash flood events affecting the Rochefort karst system (Belgium). Continuous gravity measurements at one single station were used and water level sensors installed in caves. Underground flood events typically produce a peak in the gravity signal, due to an increase in the associated mass change. After the flood, the gravity values drop but remain slightly increased compared to before the flood event. Via forward gravity modeling, the authors demonstrate that this remaining anomaly can be reasonably explained by the infiltration of local rainfall within the karst system rather than by allogenic recharge of the aquifer.

Hormonal stimulation in pikeperch

Żarski D, Ben Ammar I, Bernáth G, Baekelandt S, Bokor Z, Palińska-Żarska K, Fontaine P, Horváth Á, Kestemont P, Mandiki SNM. 2020. Repeated hormonal induction of spermiation affects the stress but not the immune response in pikeperch (Sander lucioperca). Fish & Shellfish Immunology 101:143–151. DOI: 10.1016/j.fsi.2020.03.057.

Controlled reproduction remains a challenge in aquaculture, especially for newly domesticated fish species, such as pikeperch (Sander lucioperca). Sperm quality and quantity is crucial for the success of a selective-breeding program. It is common practice to stimulate fish with hormones, either with human chorionic gonadotropin (hCG) or salmon gonadoliberine analogue (sGnRHa). This study shows that hormonal stimulation increased quality and quantity of sperm. No effects on immune response were detected, but HCG affected stress response in pikeperch males. Sperm quality was further negatively correlated with immune markers, pronouncing the need to carefully revise broodstock management and selection practices in aquaculture.

Biotic resource use by fisheries

Luong AD, Dewulf J, De Laender F. 2020. Quantifying the primary biotic resource use by fisheries: A global assessment. Science of The Total Environment 719:137352. DOI: 10.1016/j.scitotenv.2020.137352.

Capture fisheries contribute to fish production via fishmeal and fish oil which are important for livestock production as well as aquaculture systems. Estimates of primary production required (PPR) are used to assess the ecological impacts of fishing. Currently, the calculation of Specific PPR (SPPR) relies on simplified and invalid assumptions. In this study, SPPRs of more than 1700 species were directly calculated based on food web flow matrices using an advanced SPPR calculation framework for five countries. The trophic level of a species was the most important ecological factor determining its SPPR. The results indicate that the conventional approach underestimates PPRs by up to a factor of 5. This new approach gives a more conservative assessment of marine biotic resource use.

Fe-rich bentonites from Westerwald

Fontaine F, Christidis GE, Yans J, Hollanders S, Hoffman A, Fagel N. 2020. Characterization and origin of two Fe-rich bentonites from Westerwald (Germany). Applied Clay Science 187:105444. DOI: 10.1016/j.clay.2020.105444.

The Westerwald region is one of the major ceramic clay mining areas of Germany. The mined clays were deposited on the weathered Rhenish massif during Eocene and Oligocene and were protected from erosion by a large alkaline basalt cover. Two Fe-rich bentonite layers exposed in quarries of the Eastern part of the Westerwald were investigated with X-ray diffraction, thermogravimetric analysis, infrared spectroscopy, optical microscopy, scanning electron microscopy, chemical analyses and cation exchange capacity (CEC). In both bentonite layers, the main mineral is a high-charge Fe-rich beidellite containing exchangeable Ca and Mg. Even if they both derive from mafic volcanic rocks, the difference in accessory minerals and trace element content leads to the conclusion that they have a different precursor.

Supergene ore of Cu–Co in the Kongo

Fontaine L, De Putter T, Bernard A, Decrée S, Cailteux J, Wouters J, Yans J. 2020. Complex mineralogical-geochemical sequences and weathering events in the supergene ore of the Cu–Co Luiswishi deposit (Katanga, D.R. Congo). Journal of African Earth Sciences 161:103674. DOI: 10.1016/j.jafrearsci.2019.103674.

The Luiswishi copper and cobalt (Cu–Co) ore deposit (Haut-Katanga, D.R. Congo) belongs to the Katanga Copperbelt (KCB), a world-class Cu–Co district. The primary orebodies in the KCB consist of sulphide ore hosted in Neoproterozoic fine-grained siliciclastic and carbonate sedimentary rocks. The secondary weathered ores are still poorly documented, though most of them are strongly enriched in both copper and cobalt with regard to the primary sulphide ores. Combined mineralogical and geochemical investigations on both host rocks and ore minerals allow identifying and characterizing three distinct zones in the studied profile, from base to top: the protore, which contains sulphides and massive dolomite; the cementation zone where oxides and sulphides coexist, and the saprolite, comprised of oxidized ores only.
The demand for these geological resources (such as copper and cobalt, but also manganese, see above) will be growing in the coming years / decades, in particular to supply high-tech products and renewable energies.

2019

Belgian Black Marbles

Boulvain F, Poulain G, Tourneur F, Yans J. 2019. Potential Discrimination of Belgian Black Marbles Using Petrography, Magnetic Susceptibility and Geochemistry. Archaeometry. DOI: 10.1111/arcm.12530.

The world famous black marbles of Belgium are used since the Roman Antiquity. These rocks are not marbles in a petrographic meaning; instead they correspond to several varieties of fine‐grained, well‐cemented Paleozoic limestones, without dots, veins or fossils. But these marbles are difficult to distinguish from each other. This paper synthesizes the geological data already bibliographically available and provides new accurate geological data to compare and discriminate them. Five marbles were investigated in this study. The results confirm that discrimination is not straightforward and needs a combination of very different techniques, ranging from petrography to geochemical analysis. However, all these techniques are destructive.

Solé F, Noiret C, Desmares D, Adnet S, Taverne L, De Putter T, Mees F, Yans J, Steeman T, Louwye S, Folie A, Stevens NJ, Gunnell GF, Baudet D, Yaya NK, Smith T. 2019. Reassessment of historical sections from the Paleogene marine margin of the Congo Basin reveals an almost complete absence of Danian deposits. Geoscience Frontiers 10:1039–1063. DOI: 10.1016/j.gsf.2018.06.002.

Elementary analyses of willemite mineralisation

Choulet F, Richard J, Boiron M-C, Dekoninck A, Yans J. 2019. Distribution of trace elements in willemite from the Belgium non-sulphide deposits. European Journal of Mineralogy 31:983–997. DOI: 10.1127/ejm/2019/0031-2871.

Samples of willemite (Zn2SiO4) mineralisation from the historical non-sulphide Zn–Pb deposits of La Calamine (eastern Belgium) have been recovered from collections of the Geological Survey of Belgium. Textural and chemical analyses were used to evaluate the critical element distribution (Ge, In, Ga) and deportment. Willemite is a mineral of secondary origin and occurs as a variety of types that are continuously formed between the protore stage (sulphides) and the late supergene stage (carbonates and hydrated phases). Different types of willemite may be distinguished on the basis of their shape and zoning characteristics, also marked by a significant change of major-element compositions in the late generation of willemite. Among the trace elements, anomalous high contents of P, Cd, As, Pb, Ag and Sb were noted. While Ga and In contents are very low (less than 4 ppm) or even below detection limits, significant Ge contents up to 250 ppm were measured. Such contents are consistent with values reported from willemite mineralization throughout the world.

Dating of Manganese oxides

Dekoninck A, Monié P, Blockmans S, Hatert F, Rochez G, Yans J. 2019. Genesis and 40Ar/39Ar dating of K-Mn oxides from the Stavelot Massif (Ardenne, Belgium): Insights into Oligocene to Pliocene weathering periods in Western Europe. Ore Geology Reviews 115:103191. DOI: 10.1016/j.oregeorev.2019.103191.

The occurrence of Ordovician Fe-Mn-rich sediments in the Stavelot inlier (NE Ardennes, Rhenish Massif, Belgium) has drawn the attention of geoscientists for more than one century, as they contain natural “coticule” whetstones and numerous weathered Manganese (Mn) deposits. The Mn-bearing sediments have undergone greenschist facies metamorphism in relation to the Caledonian and Variscan orogenesis. More recent weathering processes transformed the early mineral assemblages into secondary Mn oxides. This study investigates the weathering processes of these Mn-rich rocks by new mineralogical, petrographical and geochemical data and a new 40Ar/39Ar geochronology of K-Mn oxides.

Climate change in the Palaeocene

Wouters S, Spassov S, Martinez M, Steurbaut E, Storme J-Y, Yans J, Devleeschouwer X. 2019. Depositional changes during the Danian–Selandian transition in Loubieng (France), Zumaia (Spain) and Sidi Nasseur (Tunisia): insights from and limits of rock magnetism. Geological Magazine:1–19. DOI: 10.1017/S0016756819000281.

Depositional changes that occurred during the Danian–Selandian transition are studied in France, Spain and Tunisia. These changes are linked to climatic events such as hyperthermals, i.e. short-term warming events. Here, rock-magnetic techniques are used that are very sensitive and allow the identification, characterization and quantification of magnetic minerals in rocks by measuring magnetic parameters. These help to understand a wide range of geological processes involving these minerals. For example, humidity levels or detrital or biogenic origin of minerals can be determined.

Old, feathered dinosaurs

Cincotta A, Pestchevitskaya EB, Sinitsa SM, Markevich VS, Debaille V, Reshetova SA, Mashchuk IM, Frolov AO, Gerdes A, Yans J, Godefroit P. 2019. The rise of feathered dinosaurs: Kulindadromeus zabaikalicus, the oldest dinosaur with ‘feather-like’ structures. PeerJ 7:e6239. DOI: 10.7717/peerj.6239.

A first dating of the Kulinda locality (south-eastern Siberia) is presented, the locality of the primitive ornithischian dinosaur Kulindadromeus zabaikalicus. The method combines U-Pb analyses (LA-ICP-MS) on detrital zircons and monazites from sedimentary rocks of volcanoclastic origin with palynological observations. Evidence of a Bathonian age—between 168.3 ± 1.3 Ma and 166.1 ± 1.2 Ma—for Kulindadromeus is provided. This is older than the previous Late Jurassic to Early Cretaceous ages tentatively based on local stratigraphic correlations. Thus, Kulindadromeus is the oldest known dinosaur with “feather-like” structures discovered so far.

OM-MADE - an open-source program

Tinet A-J, Collon P, Philippe C, Dewaide L, Hallet V. 2019. OM-MADE: An open-source program to simulate one-dimensional solute transport in multiple exchanging conduits and storage zones. Computers & Geosciences 127:23–35. DOI: 10.1016/j.cageo.2019.03.001.

OM-MADE (One-dimensional Model for Multiple Advection, Dispersion, and storage in Exchanging zones) is an open-source python code to simulate one-dimensional solute transport in conduits. It enables the simulation of multiple exchanging flow and storage zones in steady-state flow conditions. It further helps with the interpretation of multi-peaked breakthrough curves that can be observed in karstic system tracer tests.

Geological analysis of fossil-bearing Dakhla

Benammi M, Adnet S, Marivaux L, Yans J, Noiret C, Tabuce R, Surault J, Kati IE, Enault S, Baidder L, Saddiqi O, Benammi M. 2019. Geology, biostratigraphy and carbon isotope chemostratigraphy of the Palaeogene fossil-bearing Dakhla sections, southwestern Moroccan Sahara. Geological Magazine 156:117–132. DOI: 10.1017/S0016756817000851.

Nature and age of the sedimentological deposits exposed in the Dakhla region (Sahara, Morocco) were described and refined based on lithological, palaeomagnetic, carbon isotope chemostratigraphy and biochronological data to date its Palaeogene faunas. Analyses show that the rodent assemblage (a high diversity of micromammals) found in the region represents the first Oligocene record of rodents from north-western Saharan Africa.

River channelization increases competition among young fish

Latli A, Michel LN, Lepoint G, Kestemont P. 2019. River habitat homogenisation enhances trophic competition and promotes individual specialisation among young of the year fish. Freshwater Biology 64:520–531. DOI: 10.1111/fwb.13239.

Large rivers are heavily modified for navigation, which may reduce food availability for young fish and their chance to reach the adult age. In the Meuse River, decrease of fish abundance is thought to be linked to a drastic reduction of phytoplankton biomass. The trophic niches of four fish species at various stages of development were studied to compare intra‐ and interspecific competition between reaches that differ in their degree of channelization. In the heavily channelized reach, resource diversity was lower. Trophic competition between larval stages was thus increased, leading also to the consumption of vegetation, which is a suboptimal energy source.

2018

Underground galleries

Quinif Y, Hallet V. 2018. The Karstic System of Han-sur-Lesse. In: Demoulin A ed. Landscapes and Landforms of Belgium and Luxembourg. World Geomorphological Landscapes. Cham: Springer International Publishing, 139–158. DOI: 10.1007/978-3-319-58239-9_9.

The karstic system of Han-sur-Lesse is the archetype of underground meander cutoff. Located in the “Calestienne”, a narrow bench extending along the northern margin of the Lower Devonian Ardenne, it comprises all caves and underground flow paths related to the epigenetic Lesse River across the Givetian limestone anticline of Boine.

Post-Paleozoic evolution of the northern Ardenne Massif

Barbarand J, Bour I, Pagel M, Quesnel F, Delcambre B, Dupuis C, Yans J. 2018. Post-Paleozoic evolution of the northern Ardenne Massif constrained by apatite fission-track thermochronology and geological data. BSGF - Earth Sciences Bulletin 189:16. DOI: 10.1051/bsgf/2018015.

This work characterizes the vertical evolution of the northern Ardenne and the Brabant massifs considering new fission-track data, using robust geological constraints. Fission track dating is a radiometric dating technique based on analyses of the damage trails, or tracks, left by fission fragments in certain uranium-bearing minerals and glasses. The damage appears as linear features referred to as fission tracks. This technique is useful at unravelling the thermal evolution of rocks and minerals.

Understanding fossil fauna

Solé F, Noiret C, Desmares D, Adnet S, Taverne L, De Putter T, Mees F, Yans J, Steeman T, Louwye S, Folie A, Stevens NJ, Gunnell GF, Baudet D, Yaya NK, Smith T. 2018. Reassessment of historical sections from the Paleogene marine margin of the Congo Basin reveals an almost complete absence of Danian deposits. Geoscience Frontiers. https://doi.org/10.1016/j.gsf.2018.06.002.

The early Paleogene is critical for understanding global biodiversity patterns in modern ecosystems. During this interval, Southern Hemisphere continents were largely characterized by isolation and faunal endemism following the breakup of Gondwana. Africa has been proposed as an important source area for the origin of several marine vertebrate groups but its Paleogene record is poorly sampled, especially from sub-Saharan Africa. To document the early Paleogene marine ecosystems of Central Africa, we revised the stratigraphic context of sedimentary deposits from three fossil-rich vertebrate localities: the Landana section in the Cabinda exclave (Angola), and the Manzadi and Bololo localities in western Democratic Republic of Congo.

Unusual H- and O-isotope compositions in the Tamra deposit, Tunisia

Dekoninck, A, Moussi, B, Vennemann, T, Jamoussi, F, Mattielli, N, Decrée, S, Chaftar, H-R, Hatira, N, & Yans, J 2018, ‘Mixed hydrothermal and meteoric fluids evidenced by unusual H- and O-isotope compositions of kaolinite-halloysite in the Fe(-Mn) Tamra deposit (Nefza district, NW Tunisia)’, Applied Clay Science, vol. 163, pp. 33–45, https://doi.org/10.1016/j.clay.2018.07.007

The iron mine of Tamra (Nefza District, NW Tunisia) is a 50 m thick Upper Mio-Pliocene sedimentary series impregnated by Fe-Mn oxides associated with white clay lenses with high halloysite and kaolinite content. The unusually high δ18O values of the kaolinite-halloysite and goethite-hematite deposit show that these latter minerals did not originate solely from an equilibrium state with pure meteoric waters. The most appropriate explanation for their relatively heavy isotopic values is a hydrothermal fluid-rock interaction of the meteoric fluid with the underlying carbonate rocks (marls and skarns).

Groundwater recharge processes

Poulain, A, Watlet, A, Kaufmann, O, Camp, MV, Jourde, H, Mazzilli, N, Rochez, G, Deleu, R, Quinif, Y, & Hallet, V 2018, ‘Assessment of groundwater recharge processes through karst vadose zone by cave percolation monitoring’, Hydrological Processes, vol. 32, no. 13, pp. 2069–2083, doi: 10.1002/hyp.13138

Recharge processes of karst aquifers are difficult to assess given their strong heterogeneity and the poorly known effect of vadose zone on infiltration. However, recharge assessment is crucial for the evaluation of groundwater resources. This experimental study identifies and quantifies recharge modes in the Rochefort Cave (Belgium). The quantification allowed investigating the question of recharge efficiency and aquifer vulnerability. Both methods used, i.e. discharge monitoring and artificial dye tracing highlighted a two‐flow component behaviour with a continuous diffuse recharge and an ephemeral quickflow recharge.

Where do the “Lorraine limestones” from the Saint-Paul Cathedral of Liège come from?

Lecuit, MX, Fronteau, G, Boulvain, F, Boulvain, F, Dechamps, F, Eyssautier-Chuine, S, Piavaux, M, Yans, J (2018) Geochemical characterization of “Lorraine limestones” from the Saint-Paul Cathedral of Liège (Belgium): assumptions for the true provenance of the building stones, Environmental Earth Sciences 77: 361. https://doi.org/10.1007/s12665-018-7554-8

Some architectural specific elements of the Saint-Paul Cathedral in Liège (Belgium) are made from ochre building stones, so-called “Lorraine limestones” (13th-15th century). However, within a radius of 200km, no such rocks can be found. This multi-analytical approach applied petrography, Rare Earth Elements geochemistry and studied archives and archeological material to characterize the stones used in the church and to compare them with ochre limestones outcropping in the north-east of the Paris Basin. The results make it highly probable that a very restricted geographical area near the ancient port of Donchery (Ardennes, France) including Dom-le-Mesnil and Hannogne ancient quarries of Bajocian limestones (Middle Jurassic) are the potential origin location for the stones used in the Saint-Paul Cathedral.

Underground lakes traced

Dewaide, L, Collon, P, Poulain, A, Rochez, G, & Hallet, V 2018, ‘Double-peaked breakthrough curves as a consequence of solute transport through underground lakes: a case study of the Furfooz karst system, Belgium’, Hydrogeology Journal, vol. 26, no.2, pp. 641–650, doi: 10.1007/s10040-017-1671-4

To study underground lakes, dye tracers are injected into the cave system and their transport measured. In karst systems, such measurements can result in double-peaked breakthrough curves (BTCs) – often reported but poorly understood. From physical laboratory experiments only, it has been proposed that these result from solute transport through underground lakes or pools. This report first describes field data (tracer tests in various hydrologic conditions) which point towards the double peak being linked to a nonlinear process that originates within the lakes. Observations took place on the Furfooz karst system in southern Belgium, where the River Lesse sinks partially into a swallow hole. The water follows a solitary conduit leading to an underground lake that is directly connected to a second underground lake.

Groundwater infiltration dynamics revealed with long-term ERT monitoring

Watlet, A, Kaufmann, O, Triantafyllou, A, Poulain, A, Chambers, JE, Meldrum, PI, Wilkinson, PB, Hallet, V, Quinif, Y, Van Ruymbeke, M, & Van Camp, M 2018, ‘Imaging groundwater infiltration dynamics in the karst vadose zone with long-term ERT monitoring’, Hydrology and Earth System Sciences, vol. 22, no.2, pp. 1563–1592, doi: 10.5194/hess-22-1563-2018

Karst regions are important sources of drinking water and their improved management is essential. This necessitates a better understanding of superficial water movements (Water infiltration and recharge processes), which are strongly heterogeneous in karst areas and measure with conventional hydrological methods. This study is the first long-term (3 y) and permanently installed electrical resistivity tomography (ERT) monitoring in a karst landscape (Rochefort Cave Laboratory, Belgium). Three types of hydrological dynamics, corresponding to areas with distinct lithological and structural features, could be identified.

Mineralogy and Genesis of an Ore in the Eastern High Atlas, Morocco

Verhaert, M, Bernard, A, Saddiqi, O, Dekoninck, A, Essalhi, M & Yans, J 2018, ‘Mineralogy and Genesis of the Polymetallic and Polyphased Low Grade Fe-Mn-Cu Ore of Jbel Rhals Deposit (Eastern High Atlas, Morocco)’, Minerals, vol. 8, no. 2, p. 39. DOI: 10.3390/min8020039

The Jbel Rhals deposit, also known as “Guelb en Nahas” (“Copper Hill”) is located in the Oriental High Atlas of Morocco and hosts a polymetallic Fe-Mn-Cu ore. It has been shortly exploited during the 19th–20th centuries but receives again attention. This work presents a petrological, mineralogical, and geochemical synthesis of the deposit with a focus on the supergene processes responsible for the current ore mineralogy. A metallogenic model explains the genesis of the ores. Special attention is given to “strategic” or “critical” raw materials in supergene mineral phases.

Sourabié A, Mandiki SNM, Geay F, Sene T, Toguyeni A, Kestemont P. 2018. Fish proteins not lipids are the major nutrients limiting the use of vegetable ingredients in catfish nutrition. Aquaculture Nutrition 24:1393–1405. DOI: 10.1111/anu.12676.

Demoulin, A, Barbier, F, Dekoninck, A, Verhaert, M, Ruffet, G, Dupuis, C & Yans, J 2018, Erosion Surfaces in the Ardenne–Oesling and Their Associated Kaolinic Weathering Mantle. in A Demoulin (ed.), Landscapes and Landforms of Belgium and Luxembourg. World Geomorphological Landscapes, Springer Verlag, Cham, pp. 63-84. DOI: 10.1007/978-3-319-58239-9_5

2017

Barral, A, Gomez, B, Zorrilla, JM, Serrano, JM, Yans, J, Daviero-Gomez, V, Ewin, TAM & Lécuyer, C 2017, 'Analysing the representativeness of local-scale palaeodiversity measurements: a case from the Lower Cretaceous plant assemblage of Hautrage (Mons Basin, Belgium)' Lethaia, vol 50, no. 2, pp. 244-257. DOI: 10.1111/let.12194

Capette, L & Hallet, V 2017, Captage SWDE de Blaton (Bernissart) - Aperçu hydrogéologique. Cellule de diagnostic "pesticide - captage" CRAW - SPGE. UNamur Département de géologie. Commissioned Report.

Capette, L & Hallet, V 2017, Site Lhoist de Marche-les-Dames - Estimation par modélisation des débits d'exhaure pour une cote altimétrique de +3 m du fond de fosse : situation actuelle et extension projetée. Commissioned Report.

Capette, L & Hallet, V 2017, SWDE - Prises d'eau de Gesves (Hoûte E1 et Houyoux G1) - Aperçu hydrogéologique. Cellule de diagnostic "pesticide - captage" CRAW - SPGE. UNamur Département de géologie. Commissioned Report.

Latli, A, Sturaro, N, Desjardin, N, Michel, LN, Otjacques, W, Lepoint, G & Kestemont, P 2017, 'Isotopic half-life and enrichment factor in two species of European freshwater fish larvae: an experimental approach' Rapid Communications in Mass Spectrometry, vol 31, no. 8, pp. 685-692. DOI: 10.1002/rcm.7838

Latli, A, Descy, J-P, Mondy, CP, Floury, M, Viroux, L, Otjacques, W, Marescaux, J, Depiereux, E, Ovidio, M, Usseglio-Polatera, P & Kestemont, P 2017, 'Long-term trends in trait structure of riverine communities facing predation risk increase and trophic resource decline' Ecological Applications, vol 27, no. 8, pp. 2458-2474.  DOI: 10.1002/eap.1621

Marivaux L, Adnet S, Benammi M, Tabuce R, Yans J, Benammi M. 2017. Earliest Oligocene hystricognathous rodents from the Atlantic margin of northwestern Saharan Africa (Dakhla, Morocco): systematic, paleobiogeographical, and paleoenvironmental implications. Journal of Vertebrate Paleontology 37:dem. DOI: 10.1080/02724634.2017.1357567.

Mellery J, Brel J, Dort J, Geay F, Kestemont P, Francis DS, Larondelle Y, Rollin X. 2017. A n-3 PUFA depletion applied to rainbow trout fry (Oncorhynchus mykiss) does not modulate its subsequent lipid bioconversion capacity. British Journal of Nutrition 117:187–199. DOI: 10.1017/S0007114516004487.

Poulain, A, Rochez, G, Van Roy, J-P, Dewaide, L, Hallet, V & De Sadelaer, G 2017, 'A compact field fluorometer and its application to dye tracing in karst environments' Hydrogeology Journal, vol 25, no. 5, pp. 1517–1524. DOI: 10.1007/s10040-017-1577-1

Schnyder J, Pons D, Yans J, Tramoy R, Abdulanova S. 2017. Integrated stratigraphy of a continental Pliensbachian–Toarcian Boundary (Lower Jurassic) section at Taskomirsay, Leontiev Graben, southwest Kazakhstan. Geological Society, London, Special Publications 427:337–356. DOI: 10.1144/SP427.15.

Verhaert, M, Bernard, A, Dekoninck, A, Lafforgue, L, Saddiqi, O & Yans, J 2017, 'Mineralogical and geochemical characterization of supergene Cu–Pb–Zn–V ores in the Oriental High Atlas, Morocco' Mineralium Deposita, vol 52, no. 7, pp. 1049-1064. DOI: 10.1007/s00126-017-0753-5, 10.1007/s00126-017-0753-5

Yans J, 2017. Gestion durable des ressources minérales en Wallonie (Belgique) : singularités et pistes de réflexion. In: L’industrie minière et le développement durable : une perspective internationale francophone. ed. Rouleau A, Gasquet D, CERM, Université du Québec à Chicoutimi et Institut de la Francophonie pour le développement durable, Collection Points de repère, 26, 99-114. link

2016

Barthélemy, J, Carletti, T, Collier, L, Hallet, V, Moriamé, M & Sartenaer, A 2016, 'Interaction prediction between groundwater and quarry extension using discrete choice models and artificial neural networks' Environmental Earth Sciences, vol 75, no. 23, 1467. DOI: 10.1007/s12665-016-6268-z

Dekoninck, A, Bernard, A, Barbarand, J, Saint-Bezar, B, Missenard, Y, Lepretre, R, Saddiqi, O & Yans, J 2016, 'Detailed mineralogy and petrology of manganese oxyhydroxide deposits of the Imini district (Morocco)' Mineralium Deposita, vol 51, no. 1, pp. 13-23. DOI: 10.1007/s00126-015-0590-3

Dekoninck, A, Leprêtre, R, Saddiqi, O, Barbarand, J & Yans, J 2016, The high-grade Imini manganese district-karst-hosted deposits of Mn oxides and oxyhydroxides. In: Bouabdellah M., Slack J. (eds) Mineral Deposits of North Africa. Mineral Resource Reviews. Springer, Cham, pp. 575-594. DOI: 10.1007/978-3-319-31733-5_22

Dewaide, L, Bonniver, I, Rochez, G & Hallet, V 2016, 'Solute transport in heterogeneous karst systems: Dimensioning and estimation of the transport parameters via multi-sampling tracer-tests modelling using the OTIS (One-dimensional Transport with Inflow and Storage) program' Journal of Hydrology, vol 534, pp. 567-578. DOI: 10.1016/j.jhydrol.2016.01.049

Geay F, Mellery J, Tinti E, Douxfils J, Larondelle Y, Mandiki SNM, Kestemont P. 2016. Innate immune system modulation and disease resistance in Eurasian perch fed contrasted LC-PUFA dietary contents. Fish & Shellfish Immunology 53:70. DOI: 10.1016/j.fsi.2016.03.078.

Geay F, Tinti E, Mellery J, Michaux C, Larondelle Y, Perpète E, Kestemont P. 2016. Cloning and functional characterization of Δ6 fatty acid desaturase (FADS2) in Eurasian perch (Perca fluviatilis). Comparative Biochemistry and Physiology Part B: Biochemistry and Molecular Biology 191:112–125. DOI: 10.1016/j.cbpb.2015.10.004.

Noiret, C, Steurbaut, E, Tabuce, R, Marandat, B, Schnyder, J, Storme, JY & Yans, J 2016, 'New bio-chemostratigraphic dating of a unique early eocene sequence from southern europe results in precise mammalian biochronological tie-points' Newsletters on Stratigraphy, vol 49, no. 3, pp. 469-480. DOI: 10.1127/nos/2016/0336

Otjacques, W, De Laender, F & Kestemont, P 2016, 'Discerning the causes of a decline in a common European fish, the roach (Rutilus rutilus L.): A modelling approach' Ecological Modelling , vol 322, pp. 92-100. DOI: 10.1016/j.ecolmodel.2015.12.002

Radinger, J, Hölker, F, Horký, P, Slavík, O, Dendoncker, N & Wolter, C 2016, 'Synergistic and antagonistic interactions of future land use and climate change on river fish assemblages' Global Change Biology, vol 22, no. 4, pp. 1505-1522. DOI: 10.1111/gcb.13183

Roland, S, Rorive, A, Capette, L & Hallet, V Carte hydrogéologique de Wallonie, Planchettes Rebecq - Ittre n° 39/1-2. link

Ruthy, I, Dassargues , A, Capette, L & Hallet, V Carte hydrogéologique de Wallonie, Planchettes Natoye – Ciney n° 54/1-2. link

Tramoy, R, Schnyder, J, Nguyen Tu, TT, Yans, J, Jacob, J, Sebilo, M, Derenne, S, Philippe, M, Huguet, A, Pons, D & Baudin, F 2016, 'The Pliensbachian-Toarcian paleoclimate transition: New insights from organic geochemistry and C, H, N isotopes in a continental section from Central Asia' Palaeogeography, Palaeoclimatology, Palaeoecology, vol 461, pp. 310-327. DOI: 10.1016/j.palaeo.2016.08.020

Verhaert, M-A, Bernard, A, Dekoninck, A & Yans, J 2016, 'Characterization and genesis of Cu-Pb-Zn-V-Fe-Mn supergene ore deposits in the area of Bou Arfa (Oriental High Atlas, Morocco)' Geologica Belgica, vol 19, no. 3/4, pp. 302-304.

Yans, J & Dekoninck, A 2016, Ressources du sous-sol wallon : historique, état des lieux et perspectives. in Mines et Carrières. vol. Hors Série 18, 236, Revue de la Société de l'Industrie Minérale, Paris, pp. 5-12. pdf

Fossil Feathers

Lindgren J, Sjövall P, Carney RM, Cincotta A, Uvdal P, Hutcheson SW, Gustafsson O, Lefèvre U, Escuillié F, Heimdal J, Engdahl A, Gren JA, Kear BP, Wakamatsu K, Yans J, Godefroit P. 2015. Molecular composition and ultrastructure of Jurassic paravian feathers. Scientific Reports 5:13520. DOI: 10.1038/srep13520.

Feathers are extremely complex epidermal structures. Their evolutionary trajectory across dinosaurs and basal birds is well documented. Melanosome-like microbodies preserved in association with fossil plumage have been used to reconstruct original colour, behaviour and physiology. However, these putative ancient melanosomes might alternatively represent microorganismal residues, a conflicting interpretation compounded by a lack of unambiguous chemical data. The authors used sensitive molecular imaging to provide novel insights into the early evolution of feathers at the sub-cellular level, and unequivocally determine that melanosomes can be preserved in fossil feathers.