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L. Marquer
Research Group for Terrestrial Palaeoclimates, Max Planck Institute for Chemistry, Hahn-Meitner-Weg 1, 55128 Mainz, Germany

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Journal article
Published: 31 July 2020 in Journal of Archaeological Science: Reports
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While the use of fire has long been recognised as a crucial innovation in the cultural evolution of humankind, much research has focused on the (debated) chronology of its earliest use and control, and less on the ways in which fire was used in the deep past. At its latest by the Upper Palaeolithic, hunter-gatherers routinely used fire to heat a wide range of materials, adjusting parameters like temperature, exposure time and fuel type to the specific requirements of the treated materials, for instance in food preparation or tool production. Comparing analyses of the chemical and physical properties of modern materials, heated under a range of controlled conditions in a laboratory, to archaeological ones might allow the reconstruction of the “heating history” of excavated materials and hence to infer the function of particular fires in the past - provided changes affecting the properties of the heated archaeological material during burial time are taken into consideration. To investigate the feasibility of such an approach, heated materials sampled from ~40,000 to 25,000 year old fireplaces (hearths) and their sedimentary matrices from the Upper Palaeolithic Abri Pataud rock shelter in South-Western France are used here to study (1) the fuel type(s) used by the site’s occupants, (2) the temperatures reached in fireplaces and (3) the potential changes in human activities related to fireplaces over time, with the influence of post-depositional processes taken into explicit consideration throughout. For this purpose, we used a range of methods to analyse macroscopically visible as well as “invisible” (microscopic and molecular) heat-altered materials. The results suggest that charred organic materials (COM) encountered in the samples predominantly result from the fuel used in fireplaces, including the earliest reported use of dung as fuel. Earlier suggestions about the use of bone as fuel at the Abri Pataud are not supported by this study. The heating temperature of COM increased gradually from 350 °C in the Aurignacian to 450 °C in Gravettian levels. Py-GC–MS studies identified a range of organic compounds, biomolecules derived from plant as well as animal sources, still preserved in the sediments after exposure to heat and burial in the rock shelter more than 20,000 years ago. Mammalian mtDNA was identified in sediment samples retrieved from the fireplaces, including ancient mtDNA fragments that originated from one or more modern human-like mitochondrial genome(s). This makes the Abri Pataud the first archaeological site for which ancient modern human mtDNA has been retrieved from sediment samples. The absence of specific organic compounds (furans) in the Aurignacian levels and their presence in the Gravettian ones, the changes in temperatures reached through the Aurignacian-Gravettian sequence as well as changes in the character of the fireplaces (presence/absence of lining river pebbles) suggest that the functions of hearths changed through time. These results highlight the potential of multi-proxy analyses of macro- and microscopic traces of ancient fireplaces, and especially of a shift in focus towards molecular traces of such activities. Systematic sampling of fireplaces and their sedimentary matrix should become a standard part of the excavation protocol of such features, to improve our understanding of the activities of humans in the deep past.

ACS Style

F. Braadbaart; F.H. Reidsma; W. Roebroeks; L. Chiotti; V. Slon; M. Meyer; Isabelle Théry-Parisot; A. van Hoesel; K.G.J. Nierop; J. Kaal; B. van Os; Laurent Marquer. Heating histories and taphonomy of ancient fireplaces: A multi-proxy case study from the Upper Palaeolithic sequence of Abri Pataud (Les Eyzies-de-Tayac, France). Journal of Archaeological Science: Reports 2020, 33, 102468 .

AMA Style

F. Braadbaart, F.H. Reidsma, W. Roebroeks, L. Chiotti, V. Slon, M. Meyer, Isabelle Théry-Parisot, A. van Hoesel, K.G.J. Nierop, J. Kaal, B. van Os, Laurent Marquer. Heating histories and taphonomy of ancient fireplaces: A multi-proxy case study from the Upper Palaeolithic sequence of Abri Pataud (Les Eyzies-de-Tayac, France). Journal of Archaeological Science: Reports. 2020; 33 ():102468.

Chicago/Turabian Style

F. Braadbaart; F.H. Reidsma; W. Roebroeks; L. Chiotti; V. Slon; M. Meyer; Isabelle Théry-Parisot; A. van Hoesel; K.G.J. Nierop; J. Kaal; B. van Os; Laurent Marquer. 2020. "Heating histories and taphonomy of ancient fireplaces: A multi-proxy case study from the Upper Palaeolithic sequence of Abri Pataud (Les Eyzies-de-Tayac, France)." Journal of Archaeological Science: Reports 33, no. : 102468.

Discussion
Published: 22 July 2020 in Quaternary Science Reviews
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Laurent Marquer; Florence Mazier; Shinya Sugita; Didier Galop; Thomas Houet; Elodie Faure; Marie-José Gaillard; Sébastien Haunold; Nicolas de Munnik; Anaëlle Simonneau; François De Vleeschouwer; Gaël Le Roux. Reply to Theuerkauf and Couwenberg (2020) comment on: “Pollen-based reconstruction of Holocene land-cover in mountain regions: Evaluation of the Landscape Reconstruction Algorithm in the Vicdessos valley, northern Pyrenees, France”. Quaternary Science Reviews 2020, 244, 106462 .

AMA Style

Laurent Marquer, Florence Mazier, Shinya Sugita, Didier Galop, Thomas Houet, Elodie Faure, Marie-José Gaillard, Sébastien Haunold, Nicolas de Munnik, Anaëlle Simonneau, François De Vleeschouwer, Gaël Le Roux. Reply to Theuerkauf and Couwenberg (2020) comment on: “Pollen-based reconstruction of Holocene land-cover in mountain regions: Evaluation of the Landscape Reconstruction Algorithm in the Vicdessos valley, northern Pyrenees, France”. Quaternary Science Reviews. 2020; 244 ():106462.

Chicago/Turabian Style

Laurent Marquer; Florence Mazier; Shinya Sugita; Didier Galop; Thomas Houet; Elodie Faure; Marie-José Gaillard; Sébastien Haunold; Nicolas de Munnik; Anaëlle Simonneau; François De Vleeschouwer; Gaël Le Roux. 2020. "Reply to Theuerkauf and Couwenberg (2020) comment on: “Pollen-based reconstruction of Holocene land-cover in mountain regions: Evaluation of the Landscape Reconstruction Algorithm in the Vicdessos valley, northern Pyrenees, France”." Quaternary Science Reviews 244, no. : 106462.

Chapter
Published: 08 July 2020 in Perspectives on the Archaeology of Pipes, Tobacco and other Smoke Plants in the Ancient Americas
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The recovery of archaeological wood charcoals from combustion features provides insights into the exploitation and use of wood fuel resources and past landscapes. The quality of our interpretation based on wood charcoals, however, depends on reliable information about the charcoal assemblages resulting from taphonomy. Charcoal is very fragile in comparison to other combustion residues such as burnt bones. In archaeological contexts, charcoal can easily be fragmented into small pieces (<0.25 mm) due to their fragile property. The investigation of small fragments and particles is particularly important for the interpretation of combustion residues when large pieces of charcoal are rare or apparently absent in archaeological sites, which is mainly true for many European Palaeolithic sites. Here, archaeologists get incomplete information when only the largest pieces and fragments are considered. In this chapter, we present a method for extracting and quantifying charcoal pieces, fragments, and particles. This approach can be considered as a strategy to minimize the impact of sample incompleteness and biases related to combustion residues in archaeological contexts. We further provide (1) a definition of what the charcoal signal means in an archaeological context; (2) an overview of taphonomy that causes charcoal fragmentation; (3) a review of charcoal sampling, extraction, observation and quantification protocols; (4) a manual (pictures and descriptions) for the observation of charcoal, from large pieces to the smallest particles; and (5) a discussion about why the charcoal signal is useful for archaeologists. By taking into account the consequences of taphonomy, the microscopic charcoal analysis in archaeological contexts provides a reliable assessment of firewood and fuel management practices and the related resilience of societies through time. The microscopic charcoal analysis can further offer additional information about the intensity of taphonomical processes and dating.

ACS Style

Laurent Marquer; Thierry Otto. Microscopic Charcoal Signal in Archaeological Contexts. Perspectives on the Archaeology of Pipes, Tobacco and other Smoke Plants in the Ancient Americas 2020, 225 -254.

AMA Style

Laurent Marquer, Thierry Otto. Microscopic Charcoal Signal in Archaeological Contexts. Perspectives on the Archaeology of Pipes, Tobacco and other Smoke Plants in the Ancient Americas. 2020; ():225-254.

Chicago/Turabian Style

Laurent Marquer; Thierry Otto. 2020. "Microscopic Charcoal Signal in Archaeological Contexts." Perspectives on the Archaeology of Pipes, Tobacco and other Smoke Plants in the Ancient Americas , no. : 225-254.

Erratum
Published: 22 May 2020 in Revue de Micropaléontologie
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Anne-Laure Daniau; Stéphanie Desprat; Julie C. Aleman; Laurent Bremond; Basil Davis; William Fletcher; Jennifer R. Marlon; Laurent Marquer; Vincent Montade; César Morales-Molino; Filipa Naughton; Damien Rius; Dunia H. Urrego. Corrigendum to “Terrestrial plant microfossils in palaeoenvironmental studies, pollen, microcharcoal and phytolith. Towards a comprehensive understanding of vegetation, fire and climate changes over the past one million years” [Revue de Micropaléontologie 63 (2019) 1–35]. Revue de Micropaléontologie 2020, 67, 100412 .

AMA Style

Anne-Laure Daniau, Stéphanie Desprat, Julie C. Aleman, Laurent Bremond, Basil Davis, William Fletcher, Jennifer R. Marlon, Laurent Marquer, Vincent Montade, César Morales-Molino, Filipa Naughton, Damien Rius, Dunia H. Urrego. Corrigendum to “Terrestrial plant microfossils in palaeoenvironmental studies, pollen, microcharcoal and phytolith. Towards a comprehensive understanding of vegetation, fire and climate changes over the past one million years” [Revue de Micropaléontologie 63 (2019) 1–35]. Revue de Micropaléontologie. 2020; 67 ():100412.

Chicago/Turabian Style

Anne-Laure Daniau; Stéphanie Desprat; Julie C. Aleman; Laurent Bremond; Basil Davis; William Fletcher; Jennifer R. Marlon; Laurent Marquer; Vincent Montade; César Morales-Molino; Filipa Naughton; Damien Rius; Dunia H. Urrego. 2020. "Corrigendum to “Terrestrial plant microfossils in palaeoenvironmental studies, pollen, microcharcoal and phytolith. Towards a comprehensive understanding of vegetation, fire and climate changes over the past one million years” [Revue de Micropaléontologie 63 (2019) 1–35]." Revue de Micropaléontologie 67, no. : 100412.

Preprint content
Published: 23 March 2020
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Quantifying the long-term trend of climate versus land use influence on vulnerable ecosystems is of great importance to identify the threats of landscape modifications on biodiversity and ecosystem services, and therefore on societies. The evaluation of the resilience of ecosystems is particularly important considering the ongoing climate change.

As ecosystems in arid Central Asia are mainly influenced by climate and physical geography and most species are growing near their physiological limit, the predicted increased aridity for this region likely increases the threat on the ecosystems in this region.

Pollen are the main proxy to explore changes in vegetation at different spatial (local to subcontinental) and temporal (decades to millennia) scales. To quantify human- and climate-induced changes in vegetation, past land-cover (pollen-based estimates), land use (human deforestation scenarios and human population size) and climate (variables derived from climate models) data can be combined, as it has been done in Europe (e.g. Marquer et al., 2017).

This study aims at quantifying the effect of past climate changes on vegetation in Central Asia over the past millennia at century time scale. For this purpose, we use 49 pollen data from sedimentary records (lakes and mires) which were transformed into vegetation composition and diversity indices. Pollen data as point estimates and spatial grids of past vegetation are combined with available annually resolved gridded summer temperature and precipitation estimates inferred from tree-ring chronologies in this region. The reconstructed climate and vegetation trends are compared to different transient Earth System model simulations with the help of the biome-model BIOME4 (c.f. Dallmeyer et al., 2017). Statistical analyses have been performed to compare all data.

We found clear spatial pattern in the plant distribution with i) a large abundance of coniferous trees in northernmost areas and to a lesser extend in the mountains (e.g. Tian Shan), ii) steppes in the lowlands and at high plateaus, and iii) semi-deserts and steppes in the lowlands. The vegetation composition and diversity have significantly changed over the past millennia. Those changes are mainly related to modifications in composition and diversity of plant species in steppes and semi-deserts, of coniferous trees in the mountains, and changes in land use. Our results reveal that precipitation is the major driver of vegetation composition and diversity in Central Asia whereas temperature mainly explains the spatial variation, in particular during major climate events, e.g. the Little Ice Age and the Warm Medieval Period. Further studies are now in progress to quantify the relative (to climate) influence of land use (e.g. anthropogenic land-cover change; ALCC) in the region.

This study demonstrates the climate dependency of vegetation composition and diversity in Central Asia, especially during the major climate events over the last two millennia. This opens the discussion about the resilience of vulnerable ecosystems facing severe impacts of ongoing and predicted climate changes in arid Central Asia.      

Dallmeyer et al. (2017) Climate of the Past 13, 107-134. / Marquer et al. (2017) Quaternary Science Reviews 171, 20-37.

ACS Style

Laurent Marquer; Andrea Seim; Anne Dallmeyer; Data Contributors. Response of vegetation to past climate changes in Central Asia. 2020, 1 .

AMA Style

Laurent Marquer, Andrea Seim, Anne Dallmeyer, Data Contributors. Response of vegetation to past climate changes in Central Asia. . 2020; ():1.

Chicago/Turabian Style

Laurent Marquer; Andrea Seim; Anne Dallmeyer; Data Contributors. 2020. "Response of vegetation to past climate changes in Central Asia." , no. : 1.

Original paper
Published: 08 February 2020 in Archaeological and Anthropological Sciences
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The Mousterian site of Grotta Reali (Rocchetta a Volturno, Molise, southern Italy), dated from between 50,940 and 40,370 cal BP, provides detailed information on the depositional dynamic and human occupation in southern Italy, and contributes to the international debate on technical behaviour at the end of the Mousterian. The site was discovered in 2001 and it was located in a small cave/shelter now partially quarried, on the backside of a tufa waterfall, at the edge of a large alluvial terrace, in correspondence of the major spring of the Volturno River. Pollen and faunal assemblages record the persistence of wooded environments with large open areas as indicated by the presence of horse, aurochs and spotted hyena. Humans settled occasionally for hunting, processing game and performing related activities. Anthropic occupation was followed by carnivores, particularly in the upper part of the stratigraphy where the evidences of their activities prevail decisively rather than those left by humans. The chronological attribution of Grotta Reali to the MIS 3 allows placing the settlement in the last phase of Neanderthals presence in Europe. The technology of knapping stone does not deviate from the range of methods used during the Mousterian. However, the large presence of a laminar volumetric method may attest a new necessity related to activities differentiation. This paper offers for the first time a comprehensive and detailed illustration of this site with a unique set of environmental data and human occupation layers.

ACS Style

Carlo Peretto; Marta Arzarello; Mauro Coltorti; Marco Bertolini; Qiao-Yu Cui; Ornella De Curtis; Vincent Lebreton; Giuseppe Lembo; Laurent Marquer; Pierluigi Pieruccini; Silvia Ravani; Ettore Rufo; Benedetto Sala; Sahra Talamo; Ursula Thun Hohenstein. Grotta Reali, the first multilayered mousterian evidences in the Upper Volturno Basin (Rocchetta a Volturno, Molise, Italy). Archaeological and Anthropological Sciences 2020, 12, 1 -30.

AMA Style

Carlo Peretto, Marta Arzarello, Mauro Coltorti, Marco Bertolini, Qiao-Yu Cui, Ornella De Curtis, Vincent Lebreton, Giuseppe Lembo, Laurent Marquer, Pierluigi Pieruccini, Silvia Ravani, Ettore Rufo, Benedetto Sala, Sahra Talamo, Ursula Thun Hohenstein. Grotta Reali, the first multilayered mousterian evidences in the Upper Volturno Basin (Rocchetta a Volturno, Molise, Italy). Archaeological and Anthropological Sciences. 2020; 12 (3):1-30.

Chicago/Turabian Style

Carlo Peretto; Marta Arzarello; Mauro Coltorti; Marco Bertolini; Qiao-Yu Cui; Ornella De Curtis; Vincent Lebreton; Giuseppe Lembo; Laurent Marquer; Pierluigi Pieruccini; Silvia Ravani; Ettore Rufo; Benedetto Sala; Sahra Talamo; Ursula Thun Hohenstein. 2020. "Grotta Reali, the first multilayered mousterian evidences in the Upper Volturno Basin (Rocchetta a Volturno, Molise, Italy)." Archaeological and Anthropological Sciences 12, no. 3: 1-30.

Journal article
Published: 17 December 2019 in Quaternary Science Reviews
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Long-term perspectives on climate- and human-induced shifts in plant communities and tree line in mountains are often inferred from fossil pollen records. However, various factors, such as complex patterns of orographic wind fields and abundant insect-pollinated plants in higher altitudes, make pollen-based reconstruction in mountain regions difficult. Over the last decade the Landscape Reconstruction Algorithm (LRA) - a model-based approach in reconstruction of vegetation – has been successfully applied in various parts of the globe. However, evaluation of its effectiveness in mountain ranges is still limited. The present study assesses the extent to which the LRA approach helps quantify the local changes in vegetation cover at Vicdessos valley in northern French Pyrenees as a case study. In the study area well-dated sediment cores are available from eight bogs and ponds, 6–113 m in radius, located above the current tree line. We first use a simple simulation experiment to evaluate the way how pollen records from “landscape islands” (mountain tops and plateaus) would represent local vegetation and to clarify important factors affecting the LRA-based reconstruction in a mountainous region. This study then uses pollen records from these sites and vegetation and land-cover data both within a 50-km radius around the Vicdessos valley and within a 2-km radius from each site for evaluation of the REVEALS- and LOVE-based reconstruction of the regional and local plant cover, respectively, in the LRA approach. The land-cover data are complied for coniferous trees, broadleaved trees and non-forested areas from the CORINE and historical maps in three time windows: 1960–1970, 1990–2000 and 2000–2013. Major findings are as follows. (1) Accuracy of the regional vegetation estimates affects the reliability of the LRA-based reconstruction of vegetation within a 2-km radius; use of the CORINE data as input to the LOVE model improves reliability of the results over the use of the REVEALS-based estimates of regional vegetation. This implies that a systematic selection of pollen data only from sites above the tree line is problematic for estimating regional vegetation, and thus the entire LRA process. (2) Selection of the dispersal models for pollen transport (i.e. the Langrangian Stochastic Model vs. Gaussian Plume Model) does not affect significantly the LRA-based estimates at both the regional and local scales in the study area. (3) The LRA approach improves the pollen-based reconstruction of local vegetation compared to pollen percentage alone in northern Pyrenees. Although further empirical and simulation studies are necessary, our results emphasize the importance of site selection for the LRA-based reconstruction of vegetation in mountain regions.

ACS Style

Laurent Marquer; Florence Mazier; Shinya Sugita; Didier Galop; Thomas Houet; Elodie Faure; Marie-José Gaillard; Sébastien Haunold; Nicolas de Munnik; Anaëlle Simonneau; François De Vleeschouwer; Gaël Le Roux. Pollen-based reconstruction of Holocene land-cover in mountain regions: Evaluation of the Landscape Reconstruction Algorithm in the Vicdessos valley, northern Pyrenees, France. Quaternary Science Reviews 2019, 228, 106049 .

AMA Style

Laurent Marquer, Florence Mazier, Shinya Sugita, Didier Galop, Thomas Houet, Elodie Faure, Marie-José Gaillard, Sébastien Haunold, Nicolas de Munnik, Anaëlle Simonneau, François De Vleeschouwer, Gaël Le Roux. Pollen-based reconstruction of Holocene land-cover in mountain regions: Evaluation of the Landscape Reconstruction Algorithm in the Vicdessos valley, northern Pyrenees, France. Quaternary Science Reviews. 2019; 228 ():106049.

Chicago/Turabian Style

Laurent Marquer; Florence Mazier; Shinya Sugita; Didier Galop; Thomas Houet; Elodie Faure; Marie-José Gaillard; Sébastien Haunold; Nicolas de Munnik; Anaëlle Simonneau; François De Vleeschouwer; Gaël Le Roux. 2019. "Pollen-based reconstruction of Holocene land-cover in mountain regions: Evaluation of the Landscape Reconstruction Algorithm in the Vicdessos valley, northern Pyrenees, France." Quaternary Science Reviews 228, no. : 106049.

Journal article
Published: 16 December 2019 in CATENA
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Reconstruction of paleo-precipitation can provide an insight into past climate and precipitation. De Ploey et al. (1995) presents a highly simplified erosion equation to consider precipitation and erosion susceptibility. This empirical model allows estimation of total precipitation and erosion susceptibility across a range of catchment characteristics (including catchment area, slope, elevation, vegetation cover) and when limited catchment or meteorological data is available. The presented study tests the De Ploey equation using dated lacustrine records of catchment soil deposition both spatially and temporally. The objective is to examine the De Ploey equation’s ability and efficiency in reconstructing past long-term precipitation using sedimentological parameters. The erosion susceptibility factor is described as a ‘black box’ value by De Ploey et al. (1995). This research unravels the erosion susceptibility variable, identifying it to change spatially and temporally according to precipitation, vegetation cover and composition (the extent of tree establishment across the catchment), total lacustrine deposition and geochemical signatures in the archive. Calculation of the erosion sustainability variable and it’s use within the De Ploey erosion equation illustrate a reconstruction of an indicative mean annual precipitation and erosion susceptibility change over the recent period (∼100 years).

ACS Style

Deonie Allen; Anaëlle Simonneau; Gaël Le Roux; Florence Mazier; Laurent Marquer; Didier Galop; Stephane Binet. Considering lacustrine erosion records and the De Ploey erosion model in an examination of mountain catchment erosion susceptibility and precipitation reconstruction. CATENA 2019, 187, 104278 .

AMA Style

Deonie Allen, Anaëlle Simonneau, Gaël Le Roux, Florence Mazier, Laurent Marquer, Didier Galop, Stephane Binet. Considering lacustrine erosion records and the De Ploey erosion model in an examination of mountain catchment erosion susceptibility and precipitation reconstruction. CATENA. 2019; 187 ():104278.

Chicago/Turabian Style

Deonie Allen; Anaëlle Simonneau; Gaël Le Roux; Florence Mazier; Laurent Marquer; Didier Galop; Stephane Binet. 2019. "Considering lacustrine erosion records and the De Ploey erosion model in an examination of mountain catchment erosion susceptibility and precipitation reconstruction." CATENA 187, no. : 104278.

Review article
Published: 21 March 2019 in Revue de Micropaléontologie
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The Earth has experienced large changes in global and regional climates over the past one million years. Understanding processes and feedbacks that control those past environmental changes is of great interest for better understanding the nature, direction and magnitude of current climate change, its effect on life, and on the physical, biological and chemical processes and ecosystem services important for human well-being. Microfossils from terrestrial plants – pollen, microcharcoal and phytoliths – preserved in terrestrial and marine sedimentary archives are particularly useful tools to document changes in vegetation, fire and land climate. They are well-preserved in a variety of depositional environments and provide quantitative reconstructions of past land cover and climate. Those microfossil data are widely available from public archives, and their spatial coverage includes almost all regions on Earth, including both high and low latitudes and altitudes. Here, we (i) review the laboratory procedures used to extract those microfossils from sediment for microscopic observations and the qualitative and quantitative information they provide, (ii) highlight the importance of regional and global databases for large-scale syntheses of environmental changes, and (iii) review the application of terrestrial plant microfossil records in palaeoclimatology and palaeoecology using key examples from specific regions and past periods.

ACS Style

Anne-Laure Daniau; Stephanie Desprat; Julie C. Aleman; Laurent Bremond; Basil Davis; William Fletcher; Jennifer Marlon; Laurent Marquer; Vincent Montade; César Morales-Molino; Filipa Naughton; Damien Rius; Dunia H. Urrego. Terrestrial plant microfossils in palaeoenvironmental studies, pollen, microcharcoal and phytolith. Towards a comprehensive understanding of vegetation, fire and climate changes over the past one million years. Revue de Micropaléontologie 2019, 63, 1 -35.

AMA Style

Anne-Laure Daniau, Stephanie Desprat, Julie C. Aleman, Laurent Bremond, Basil Davis, William Fletcher, Jennifer Marlon, Laurent Marquer, Vincent Montade, César Morales-Molino, Filipa Naughton, Damien Rius, Dunia H. Urrego. Terrestrial plant microfossils in palaeoenvironmental studies, pollen, microcharcoal and phytolith. Towards a comprehensive understanding of vegetation, fire and climate changes over the past one million years. Revue de Micropaléontologie. 2019; 63 ():1-35.

Chicago/Turabian Style

Anne-Laure Daniau; Stephanie Desprat; Julie C. Aleman; Laurent Bremond; Basil Davis; William Fletcher; Jennifer Marlon; Laurent Marquer; Vincent Montade; César Morales-Molino; Filipa Naughton; Damien Rius; Dunia H. Urrego. 2019. "Terrestrial plant microfossils in palaeoenvironmental studies, pollen, microcharcoal and phytolith. Towards a comprehensive understanding of vegetation, fire and climate changes over the past one million years." Revue de Micropaléontologie 63, no. : 1-35.

Journal article
Published: 01 June 2018 in Quaternaire
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Une formation limoneuse épaisse de plus de 6 m a été mise au jour en 2005 lors d’une opération de diagnostic archéologique, au lieu-dit la Jouannière, commune de Bonneval (Eure-et-Loir, France), sur le rebord occidental de la haute vallée du Loir. Les études sédimentologiques, micromorphologiques, géochronologiques (Re-OSL) et des microcharbons ont permis de répartir les dix couches de dépôts limoneux d’origine lœssique en deux séquences. Dans la séquence inférieure (US 10 à 5), les lœss ont été déposés entre les Stades Isotopiques Marins (SIM) 12 et 6. La découverte de bifaces et de nucléus in situ dans les couches supérieures de cette séquence (Unités Stratigraphiques US 6a et 5) indique la présence des hommes du Paléolithique moyen dès le début du SIM 8. La séquence lœssique supérieure (US 4 à 1) a subi plusieurs séries de pédogenèses et de cryoturbations. Elle comprend notamment un sol gris forestier et, par comparaison avec les stratigraphies du Nord de la France, peut être rapportée au complexe Eemien-Weichselien. Deux amas de débitage de silex ont été fouillés en limite des US 4 et 3. Les chaînes opératoires utilisées, rapportées au Paléolithique moyen, ont également été observées dans les couches de lœss supérieures qui contenaient des nucléus Levallois et des bifaces moustériens. Même si les différentes unités stratigraphiques sont moins épaisses que dans le stratotype de Saint-Pierre-lès-Elbeuf en Haute-Normandie, la stratigraphie de la Jouannière à Bonneval est à l’heure actuelle la seconde dans la moitié nord de la France à avoir enregistré et conservé des dépôts successifs de lœss et de paléosols depuis 450 000 ans.

ACS Style

Jackie Despriée; Grégory Bayle; Sylvie Coutard; Xuefeng Sun; Norbert Mercier; Gilles Courcimault; Laurent Marquer; Pierre Voinchet; Jean‑Jacques Bahain; Jean‑Luc Locht. La formation lœssique du Pléistocène moyen et supérieur de la Jouannière à Bonneval, Eure‑et‑loir (France) : sédimentologie, géochronologie, paléoenvironnement et préhistoire. Quaternaire 2018, 1 .

AMA Style

Jackie Despriée, Grégory Bayle, Sylvie Coutard, Xuefeng Sun, Norbert Mercier, Gilles Courcimault, Laurent Marquer, Pierre Voinchet, Jean‑Jacques Bahain, Jean‑Luc Locht. La formation lœssique du Pléistocène moyen et supérieur de la Jouannière à Bonneval, Eure‑et‑loir (France) : sédimentologie, géochronologie, paléoenvironnement et préhistoire. Quaternaire. 2018; (vol. 29/2):1.

Chicago/Turabian Style

Jackie Despriée; Grégory Bayle; Sylvie Coutard; Xuefeng Sun; Norbert Mercier; Gilles Courcimault; Laurent Marquer; Pierre Voinchet; Jean‑Jacques Bahain; Jean‑Luc Locht. 2018. "La formation lœssique du Pléistocène moyen et supérieur de la Jouannière à Bonneval, Eure‑et‑loir (France) : sédimentologie, géochronologie, paléoenvironnement et préhistoire." Quaternaire , no. vol. 29/2: 1.

Original paper
Published: 10 March 2018 in Archaeological and Anthropological Sciences
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The occupation of the Iberian Peninsula during the Upper Palaeolithic is mainly known from archaeological sites located in the Cantabrian and Mediterranean regions. Numerous sites have been excavated in these two regions when few sites are found in the interior of the peninsula. Several authors explain this scarcity of sites, in the inner region during the Upper Palaeolithic, by a decrease of human population resulting from a low capacity of human groups to adapt to the cold conditions of the Marine Isotopic Stage 2 (MIS 2), i.e. the effect of cold climate on human populations might have been stronger in the interior of the peninsula than in coastal areas. Recent studies underline the evidence of prehistoric occupation during this period in that region. It has been suggested that these occupations are isolated events limited to the warmest phases of the end of the MIS 2. The present study focuses on zooarchaeological and taphonomic aspects of the Magdalenian site of La Peña de Estebanvela (Segovia, Spain). Our results show that this site was recurrently occupied during the Magdalenian period, including warm and cold phases, which provide a new evidence of sustainable presence of human populations in the interior of the Iberian Peninsula at the end of the Upper Palaeolithic. We further propose hypotheses on the subsistence strategies (e.g. availability of hunting resources) developed at La Peña de Estebanvela and in a larger context including other Magdalenian sites of the inner region of the Peninsula.

ACS Style

J. Yravedra; M. Andrés-Chaín; C. Cacho; J. A. Martos; Laurent Marquer; B. Avezuela; J. Jordá-Pardo; Ignacio Martín Lerma; C. Sésé; J. Valdivia. Recurrent Magdalenian occupation in the interior of the Iberian Peninsula: new insights from the archaeological site of La Peña de Estebanvela (Segovia, Spain). Archaeological and Anthropological Sciences 2018, 11, 1477 -1489.

AMA Style

J. Yravedra, M. Andrés-Chaín, C. Cacho, J. A. Martos, Laurent Marquer, B. Avezuela, J. Jordá-Pardo, Ignacio Martín Lerma, C. Sésé, J. Valdivia. Recurrent Magdalenian occupation in the interior of the Iberian Peninsula: new insights from the archaeological site of La Peña de Estebanvela (Segovia, Spain). Archaeological and Anthropological Sciences. 2018; 11 (4):1477-1489.

Chicago/Turabian Style

J. Yravedra; M. Andrés-Chaín; C. Cacho; J. A. Martos; Laurent Marquer; B. Avezuela; J. Jordá-Pardo; Ignacio Martín Lerma; C. Sésé; J. Valdivia. 2018. "Recurrent Magdalenian occupation in the interior of the Iberian Peninsula: new insights from the archaeological site of La Peña de Estebanvela (Segovia, Spain)." Archaeological and Anthropological Sciences 11, no. 4: 1477-1489.

Original research article
Published: 08 March 2018 in Frontiers in Plant Science
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Characterization of land cover change in the past is fundamental to understand the evolution and present state of the Earth system, the amount of carbon and nutrient stocks in terrestrial ecosystems, and the role played by land-atmosphere interactions in influencing climate. The estimation of land cover changes using palynology is a mature field, as thousands of sites in Europe have been investigated over the last century. Nonetheless, a quantitative land cover reconstruction at a continental scale has been largely missing. Here, we present a series of maps detailing the evolution of European forest cover during last 12,000 years. Our reconstructions are based on the Modern Analog Technique (MAT): a calibration dataset is built by coupling modern pollen samples with the corresponding satellite-based forest-cover data. Fossil reconstructions are then performed by assigning to every fossil sample the average forest cover of its closest modern analogs. The occurrence of fossil pollen assemblages with no counterparts in modern vegetation represents a known limit of analog-based methods. To lessen the influence of no-analog situations, pollen taxa were converted into plant functional types prior to running the MAT algorithm. We then interpolate site-specific reconstructions for each timeslice using a four-dimensional gridding procedure to create continuous gridded maps at a continental scale. The performance of the MAT is compared against methodologically independent forest-cover reconstructions produced using the REVEALS method. MAT and REVEALS estimates are most of the time in good agreement at a trend level, yet MAT regularly underestimates the occurrence of densely forested situations, requiring the application of a bias correction procedure. The calibrated MAT-based maps draw a coherent picture of the establishment of forests in Europe in the Early Holocene with the greatest forest-cover fractions reconstructed between ∼8,500 and 6,000 calibrated years BP. This forest maximum is followed by a general decline in all parts of the continent, likely as a result of anthropogenic deforestation. The continuous spatial and temporal nature of our reconstruction, its continental coverage, and gridded format make it suitable for climate, hydrological, and biogeochemical modeling, among other uses.

ACS Style

Marco Zanon; Basil A. S. Davis; Laurent Marquer; Simon Brewer; Jed O. Kaplan. European Forest Cover During the Past 12,000 Years: A Palynological Reconstruction Based on Modern Analogs and Remote Sensing. Frontiers in Plant Science 2018, 9, 253 .

AMA Style

Marco Zanon, Basil A. S. Davis, Laurent Marquer, Simon Brewer, Jed O. Kaplan. European Forest Cover During the Past 12,000 Years: A Palynological Reconstruction Based on Modern Analogs and Remote Sensing. Frontiers in Plant Science. 2018; 9 ():253.

Chicago/Turabian Style

Marco Zanon; Basil A. S. Davis; Laurent Marquer; Simon Brewer; Jed O. Kaplan. 2018. "European Forest Cover During the Past 12,000 Years: A Palynological Reconstruction Based on Modern Analogs and Remote Sensing." Frontiers in Plant Science 9, no. : 253.

Journal article
Published: 17 February 2018 in Journal of Vegetation Science
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We investigated the changing role of climate, forest fires and human population size in the broad-scale compositional changes in Holocene vegetation dynamics before and after the onset of farming in Sweden (at 6,000 cal yr BP) and in Finland (at 4,000 cal yr BP). Southern and central Sweden, SW and SE Finland. Holocene regional plant abundances were reconstructed using the REVEALS model on selected fossil pollen records from lakes. The relative importance of climate, fires and human population size on changes in vegetation composition was assessed using variation partitioning. Past climate variable was derived from the LOVECLIM climate model. Fire variable was reconstructed from sedimentary charcoal records. Estimated trend in human population size was based on the temporal distribution of archaeological radiocarbon dates. Climate explains the highest proportion of variation in vegetation composition during the whole study period in Sweden (10,000–4,000 cal yr BP) and in Finland (10,000–1,000 cal yr BP), and during the pre-agricultural period. In general, fires explain a relatively low proportion of variation. Human population size has significant effect on vegetation dynamics after the onset of farming and explains the highest variation in vegetation in S Sweden and SW Finland. Mesolithic hunter-gatherer populations did not significantly affect vegetation composition in Fennoscandia, and climate was the main driver of changes at that time. Agricultural communities, however, had greater effect on vegetation dynamics, and the role of human population size became a more important factor during the late Holocene. Our results demonstrate that climate can be considered the main driver of long-term vegetation dynamics in Fennoscandia. However, in some regions the influence of human population size on Holocene vegetation changes exceeded that of climate and has a longevity dating to the early Neolithic.

ACS Style

Niina Kuosmanen; Laurent Marquer; Miikka Tallavaara; Chiara Molinari; Yurui Zhang; Teija Alenius; Kevan Edinborough; Petro Pesonen; Triin Reitalu; Hans Renssen; Anna-Kari Trondman; Heikki Seppa. The role of climate, forest fires and human population size in Holocene vegetation dynamics in Fennoscandia. Journal of Vegetation Science 2018, 29, 382 -392.

AMA Style

Niina Kuosmanen, Laurent Marquer, Miikka Tallavaara, Chiara Molinari, Yurui Zhang, Teija Alenius, Kevan Edinborough, Petro Pesonen, Triin Reitalu, Hans Renssen, Anna-Kari Trondman, Heikki Seppa. The role of climate, forest fires and human population size in Holocene vegetation dynamics in Fennoscandia. Journal of Vegetation Science. 2018; 29 (3):382-392.

Chicago/Turabian Style

Niina Kuosmanen; Laurent Marquer; Miikka Tallavaara; Chiara Molinari; Yurui Zhang; Teija Alenius; Kevan Edinborough; Petro Pesonen; Triin Reitalu; Hans Renssen; Anna-Kari Trondman; Heikki Seppa. 2018. "The role of climate, forest fires and human population size in Holocene vegetation dynamics in Fennoscandia." Journal of Vegetation Science 29, no. 3: 382-392.

Journal article
Published: 15 February 2018 in Quaternary Research
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We report on a loess-paleosol sequence (LPS) near Remizovka, located in the northern Tian Shan piedmont of southeastern Kazakhstan. This site represents a key record for Late Pleistocene climatic fluctuations at the intersection of major northern hemisphere climate subsystems. This paper develops a synthesized dataset of previous conflicting studies at Remizovka by characterizing their (paleo)topographic context, which had remained previously overlooked. Digital elevation models, satellite images, and archival photography characterize recent topographic developments. Two well-developed pedocomplexes, which we investigate in detail and date by luminescence mark the paleotopography during Marine Oxygen Isotope Stage (MIS) 5. Peak dust accumulation rates here occurred during the middle MIS 5 and MIS 4/early MIS 3. These are partially comparable with records from neighboring regions, but not in phase with global ice volume records. This discrepancy may be related to a distinct regional environmental response to larger-scale climatic drivers and local topographic influences on dust deposition patterns. Our findings confirm the potential of the LPS Remizovka to provide high-resolution paleoclimate data for the Late Pleistocene. The three-dimensional stratigraphic reconstruction reinforces the caution required to correctly interpret loess formation processes prior to their interpretation as paleoclimate archives, and provides guidelines for a more suitable approach.

ACS Style

Tobias Sprafke; Kathryn E. Fitzsimmons; Christoph Grützner; Austin Elliott; Laurent Marquer; Saida Nigmatova. Reevaluation of Late Pleistocene loess profiles at Remizovka (Kazakhstan) indicates the significance of topography in evaluating terrestrial paleoclimate records. Quaternary Research 2018, 89, 674 -690.

AMA Style

Tobias Sprafke, Kathryn E. Fitzsimmons, Christoph Grützner, Austin Elliott, Laurent Marquer, Saida Nigmatova. Reevaluation of Late Pleistocene loess profiles at Remizovka (Kazakhstan) indicates the significance of topography in evaluating terrestrial paleoclimate records. Quaternary Research. 2018; 89 (3):674-690.

Chicago/Turabian Style

Tobias Sprafke; Kathryn E. Fitzsimmons; Christoph Grützner; Austin Elliott; Laurent Marquer; Saida Nigmatova. 2018. "Reevaluation of Late Pleistocene loess profiles at Remizovka (Kazakhstan) indicates the significance of topography in evaluating terrestrial paleoclimate records." Quaternary Research 89, no. 3: 674-690.

Journal article
Published: 15 January 2018 in Scientific Reports
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8000 years ago, prior to Neolithic agriculture, Europe was mostly a wooded continent. Since then, its forest cover has been progressively fragmented, so that today it covers less than half of Europe’s land area, in many cases having been cleared to make way for fields and pasture-land. Establishing the origin of Europe’s current, more open land-cover mosaic requires a long-term perspective, for which pollen analysis offers a key tool. In this study we utilise and compare three numerical approaches to transforming pollen data into past forest cover, drawing on >1000 14C-dated site records. All reconstructions highlight the different histories of the mixed temperate and the northern boreal forests, with the former declining progressively since ~6000 years ago, linked to forest clearance for agriculture in later prehistory (especially in northwest Europe) and early historic times (e.g. in north central Europe). In contrast, extensive human impact on the needle-leaf forests of northern Europe only becomes detectable in the last two millennia and has left a larger area of forest in place. Forest loss has been a dominant feature of Europe’s landscape ecology in the second half of the current interglacial, with consequences for carbon cycling, ecosystem functioning and biodiversity.

ACS Style

N. Roberts; R. M. Fyfe; J. Woodbridge; M.-J. Gaillard; B. A. S. Davis; J. O. Kaplan; Laurent Marquer; Florence Mazier; A. B. Nielsen; S. Sugita; A.-K. Trondman; M. Leydet. Europe’s lost forests: a pollen-based synthesis for the last 11,000 years. Scientific Reports 2018, 8, 1 -8.

AMA Style

N. Roberts, R. M. Fyfe, J. Woodbridge, M.-J. Gaillard, B. A. S. Davis, J. O. Kaplan, Laurent Marquer, Florence Mazier, A. B. Nielsen, S. Sugita, A.-K. Trondman, M. Leydet. Europe’s lost forests: a pollen-based synthesis for the last 11,000 years. Scientific Reports. 2018; 8 (1):1-8.

Chicago/Turabian Style

N. Roberts; R. M. Fyfe; J. Woodbridge; M.-J. Gaillard; B. A. S. Davis; J. O. Kaplan; Laurent Marquer; Florence Mazier; A. B. Nielsen; S. Sugita; A.-K. Trondman; M. Leydet. 2018. "Europe’s lost forests: a pollen-based synthesis for the last 11,000 years." Scientific Reports 8, no. 1: 1-8.

Journal article
Published: 19 December 2017 in Land
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Anthropogenic land cover change (ALCC) is the most important transformation of the Earth system that occurred in the preindustrial Holocene, with implications for carbon, water and sediment cycles, biodiversity and the provision of ecosystem services and regional and global climate. For example, anthropogenic deforestation in preindustrial Eurasia may have led to feedbacks to the climate system: both biogeophysical, regionally amplifying winter cold and summer warm temperatures, and biogeochemical, stabilizing atmospheric CO2 concentrations and thus influencing global climate. Quantification of these effects is difficult, however, because scenarios of anthropogenic land cover change over the Holocene vary widely, with increasing disagreement back in time. Because land cover change had such widespread ramifications for the Earth system, it is essential to assess current ALCC scenarios in light of observations and provide guidance on which models are most realistic. Here, we perform a systematic evaluation of two widely-used ALCC scenarios (KK10 and HYDE3.1) in northern and part of central Europe using an independent, pollen-based reconstruction of Holocene land cover (REVEALS). Considering that ALCC in Europe primarily resulted in deforestation, we compare modeled land use with the cover of non-forest vegetation inferred from the pollen data. Though neither land cover change scenario matches the pollen-based reconstructions precisely, KK10 correlates well with REVEALS at the country scale, while HYDE systematically underestimates land use with increasing magnitude with time in the past. Discrepancies between modeled and reconstructed land use are caused by a number of factors, including assumptions of per-capita land use and socio-cultural factors that cannot be predicted on the basis of the characteristics of the physical environment, including dietary preferences, long-distance trade, the location of urban areas and social organization.

ACS Style

Jed O. Kaplan; Kristen M. Krumhardt; Marie-José Gaillard; Shinya Sugita; Anna-Kari Trondman; Ralph Fyfe; Laurent Marquer; Florence Mazier; Anne Birgitte Nielsen. Constraining the Deforestation History of Europe: Evaluation of Historical Land Use Scenarios with Pollen-Based Land Cover Reconstructions. Land 2017, 6, 91 .

AMA Style

Jed O. Kaplan, Kristen M. Krumhardt, Marie-José Gaillard, Shinya Sugita, Anna-Kari Trondman, Ralph Fyfe, Laurent Marquer, Florence Mazier, Anne Birgitte Nielsen. Constraining the Deforestation History of Europe: Evaluation of Historical Land Use Scenarios with Pollen-Based Land Cover Reconstructions. Land. 2017; 6 (4):91.

Chicago/Turabian Style

Jed O. Kaplan; Kristen M. Krumhardt; Marie-José Gaillard; Shinya Sugita; Anna-Kari Trondman; Ralph Fyfe; Laurent Marquer; Florence Mazier; Anne Birgitte Nielsen. 2017. "Constraining the Deforestation History of Europe: Evaluation of Historical Land Use Scenarios with Pollen-Based Land Cover Reconstructions." Land 6, no. 4: 91.

Journal article
Published: 01 September 2017 in Quaternary Science Reviews
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Publisher: Elsevier articletitle: Quantifying the effects of land use and climate on Holocene vegetation in Europe journaltitle: Quaternary Science Reviews articlelink: http://dx.doi.org/10.1016/j.quascirev.2017.07.001 content_type: article copyright: © 2017 Elsevier Ltd. All rights reserved

ACS Style

Laurent Marquer; Marie-José Gaillard; Shinya Sugita; Anneli Poska; Anna-Kari Trondman; Florence Mazier; Anne Birgitte Nielsen; Ralph M. Fyfe; Anna Maria Jönsson; Benjamin Smith; Jed O. Kaplan; Teija Alenius; H. John B. Birks; Anne E. Bjune; Jörg Christiansen; John Dodson; Kevin J. Edwards; Thomas Giesecke; Ulrike Herzschuh; Mihkel Kangur; Tiiu Koff; Małgorzata Latałowa; Jutta Lechterbeck; Jörgen Olofsson; Heikki Seppä. Quantifying the effects of land use and climate on Holocene vegetation in Europe. Quaternary Science Reviews 2017, 171, 20 -37.

AMA Style

Laurent Marquer, Marie-José Gaillard, Shinya Sugita, Anneli Poska, Anna-Kari Trondman, Florence Mazier, Anne Birgitte Nielsen, Ralph M. Fyfe, Anna Maria Jönsson, Benjamin Smith, Jed O. Kaplan, Teija Alenius, H. John B. Birks, Anne E. Bjune, Jörg Christiansen, John Dodson, Kevin J. Edwards, Thomas Giesecke, Ulrike Herzschuh, Mihkel Kangur, Tiiu Koff, Małgorzata Latałowa, Jutta Lechterbeck, Jörgen Olofsson, Heikki Seppä. Quantifying the effects of land use and climate on Holocene vegetation in Europe. Quaternary Science Reviews. 2017; 171 ():20-37.

Chicago/Turabian Style

Laurent Marquer; Marie-José Gaillard; Shinya Sugita; Anneli Poska; Anna-Kari Trondman; Florence Mazier; Anne Birgitte Nielsen; Ralph M. Fyfe; Anna Maria Jönsson; Benjamin Smith; Jed O. Kaplan; Teija Alenius; H. John B. Birks; Anne E. Bjune; Jörg Christiansen; John Dodson; Kevin J. Edwards; Thomas Giesecke; Ulrike Herzschuh; Mihkel Kangur; Tiiu Koff; Małgorzata Latałowa; Jutta Lechterbeck; Jörgen Olofsson; Heikki Seppä. 2017. "Quantifying the effects of land use and climate on Holocene vegetation in Europe." Quaternary Science Reviews 171, no. : 20-37.

Journal article
Published: 01 August 2017 in Current Anthropology
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We can trace the beginnings of our knowledge of early Upper Paleolithic (Aurignacian) use of fire to the pioneering 1910–1911 excavations at Abri Blanchard undertaken by Louis Didon and Marcel Castanet. At Blanchard, the excavators recognized and described fire structures that correspond in many ways to features excavated more recently in Western and Central Europe. Here, we address the issue of heat and light management in the early Upper Paleolithic, demonstrating a pattern that builds on these early excavations but that is refined through our recent field operations. Topics to be discussed include (1) recently excavated fire structures that suggest complex fire management and use, (2) the seemingly massive use of bone as fuel in most early Aurignacian sites, and (3) the anchoring of skin structures for purposes of heat retention with fireplaces behind animal-skin walls. Furthermore, new data on activities around fireplaces make it possible to infer social and organizational aspects of fire structures within Aurignacian living spaces. The vast majority of early Aurignacian occupations, most of them now dated to between 33,000 and 32,000 BP (uncalibrated), occurred on a previously unoccupied bedrock platform into which the occupants dug their fire features.

ACS Style

Randall White; Romain Mensan; Amy E. Clark; Elise Tartar; Laurent Marquer; Raphaëlle Bourrillon; Paul Goldberg; Laurent Chiotti; Catherine Cretin; William Rendu; Anne Pike-Tay; Sarah Ranlett. Technologies for the Control of Heat and Light in the Vézère Valley Aurignacian. Current Anthropology 2017, 58, S288 -S302.

AMA Style

Randall White, Romain Mensan, Amy E. Clark, Elise Tartar, Laurent Marquer, Raphaëlle Bourrillon, Paul Goldberg, Laurent Chiotti, Catherine Cretin, William Rendu, Anne Pike-Tay, Sarah Ranlett. Technologies for the Control of Heat and Light in the Vézère Valley Aurignacian. Current Anthropology. 2017; 58 (S16):S288-S302.

Chicago/Turabian Style

Randall White; Romain Mensan; Amy E. Clark; Elise Tartar; Laurent Marquer; Raphaëlle Bourrillon; Paul Goldberg; Laurent Chiotti; Catherine Cretin; William Rendu; Anne Pike-Tay; Sarah Ranlett. 2017. "Technologies for the Control of Heat and Light in the Vézère Valley Aurignacian." Current Anthropology 58, no. S16: S288-S302.

Journal article
Published: 01 December 2016 in Forest Ecology and Management
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Mihaela-Mariana Tudoran; Laurent Marquer; Anna Maria Jönsson. Historical experience (1850–1950 and 1961–2014) of insect species responsible for forest damage in Sweden: Influence of climate and land management changes. Forest Ecology and Management 2016, 381, 347 -359.

AMA Style

Mihaela-Mariana Tudoran, Laurent Marquer, Anna Maria Jönsson. Historical experience (1850–1950 and 1961–2014) of insect species responsible for forest damage in Sweden: Influence of climate and land management changes. Forest Ecology and Management. 2016; 381 ():347-359.

Chicago/Turabian Style

Mihaela-Mariana Tudoran; Laurent Marquer; Anna Maria Jönsson. 2016. "Historical experience (1850–1950 and 1961–2014) of insect species responsible for forest damage in Sweden: Influence of climate and land management changes." Forest Ecology and Management 381, no. : 347-359.

Journal article
Published: 01 September 2015 in L'Anthropologie
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Laurent Marquer; Vincent Lebreton; Thierry Otto; Erwan Messager. Étude des macro-, méso- et micro-charbons du site épigravettien de Mezhyrich (Ukraine) : données taphonomiques et anthracologiques. L'Anthropologie 2015, 119, 487 -504.

AMA Style

Laurent Marquer, Vincent Lebreton, Thierry Otto, Erwan Messager. Étude des macro-, méso- et micro-charbons du site épigravettien de Mezhyrich (Ukraine) : données taphonomiques et anthracologiques. L'Anthropologie. 2015; 119 (4):487-504.

Chicago/Turabian Style

Laurent Marquer; Vincent Lebreton; Thierry Otto; Erwan Messager. 2015. "Étude des macro-, méso- et micro-charbons du site épigravettien de Mezhyrich (Ukraine) : données taphonomiques et anthracologiques." L'Anthropologie 119, no. 4: 487-504.