Late Holocene vegetation and fire dynamics on the summits of the Guayana Highlands: The Uei-tepui palynological record

The summits of the tepuis (sandstone table mountains of the Neotropical Guayana region-Guayana Highlands, GH) have been considered valuable for palaeoecological studies due to their pristine nature, which emphasizes the role of natural (i.e. non-human) factors on ecological change. Anthropogenic fires, very frequent in the surrounding Gran Sabana (GS) uplands, have very rarely been documented in the GH, and are therefore not considered an important ecological factor in the high-tepui biome. This paper reports the palynological and charcoal results of a Late Holocene sequence from the summit of Uei-tepui (2104 m elevation), where extensive signs of fire were recently observed. Since ~. 2000 cal yr BP, the landscape of the study site has been dominated by meadows with occasional shrubs and cloud forests, which underwent expansions and contractions driven by climate changes and fire. A major vegetation shift occurred in the mid-18th century, when a sustained increase in local fires favoured the expansion of the low and spreading Cyrilla racemiflora shrublands at the expense of meadows and forests. Uei-tepui fires most probably were the result of human activities and reached the summit under study from the GS uplands through the vegetated slopes that characterize this tepui. The mostly anthropogenic nature of these fires, especially the more recent ones, is supported by the initial occurrence of wetter conditions, and by its coincidence with significant social changes in the GS indigenous populations, mainly the European contact. The emergence of fire as a disturbing agent of the GH biome highlights the need for an effective management plan in the GS uplands, where the vast majority of present-day fires originate, and designed in collaboration with the indigenous communities. Proactive conservation measures are considered even more important under future warming projections in the area. © 2016 Elsevier B.V.This research was supported by projects BIOCON 2004 90/05, BIOCON 08-188/09 (BBVA Foundation, Spain), CGL2006-00974/BOS (Ministry of Education and Science, Spain) and CGL2009-07069/BOS (Ministry of Science and Innovation, Spain) to V. Rull, and a predoctoral grant to E. Safont from the University of Barcelona. Fieldwork permits were provided by the Ministry of Science and Technology of Venezuela (no. 0000013, 5 Jan. 2007) and the Ministry of Environment of the same country (no. IE-085, 9 Feb. 2007).Peer reviewe

Late-Holocene vegetation and fire dynamics on the summits of the Guayana Highlands: the Uei-tepui palynological record.

The summits of the tepuis (sandstone table mountains of the Neotropical Guayana region¿Guayana Highlands, GH) have been considered valuable for palaeoecological studies due to their pristine nature, which emphasizes the role of natural (i.e. non-human) factors on ecological change. Anthropogenic fires, very frequent in the surrounding Gran Sabana (GS) uplands, have very rarely been documented in the GH, and are therefore not considered an important ecological factor in the high-tepui biome. This paper reports the palynological and charcoal results of a Late Holocene sequence from the summit of Uei-tepui (2104 m elevation), where extensive signs of fire were recently observed. Since ~2000 cal yr BP, the landscape of the study site has been dominated by meadowswith occasional shrubs and cloud forests,which underwent expansions and contractions driven by climate changes and fire. A major vegetation shift occurred in the mid-18th century, when a sustained increase in local fires favoured the expansion of the low and spreading Cyrilla racemiflora shrublands at the expense of meadows and forests. Uei-tepui firesmost probably were the result of human activities and reached the summit under study from the GS uplands through the vegetated slopes that characterize this tepui. The mostly anthropogenic nature of these fires, especially themore recent ones, is supported by the initial occurrence of wetter conditions, and by its coincidence with significant social changes in the GS indigenous populations, mainly the European contact. The emergence of fire as a disturbing agent of theGH biome highlights the need for an effective management plan in the GS uplands, where the vast majority of present-day fires originate, and designed in collaboration with the indigenous communities. Proactive conservationmeasures are considered even more important under future warming projections in the area

Seasonal patterns of pollen sedimentation in Lake Montcortès (Central Pyrenees) and potential applications to high-resolution paleoecology: a 2-year pilot study

14 páginas, 2 tablas, 10 figuras.Lakes with varved sediments are especially well suited for paleoecological study, from annual to even seasonal resolution. The interpretative power of such high-resolution paleoenvironmental reconstructions relies on the availability of modern analogs with the same temporal resolution. We studied seasonal pollen sedimentation in varved Lake Montcorte`s, Central Pyrenees (Spain), as a modern analog for highresolution reconstruction of Late Holocene vegetation and landscape dynamics. Seasonal samples were obtained from sediment traps that were submerged near the maximum water depth for a 2-year period (fall 2013 to fall 2015). Seasonal pollen sedimentation was compared with meteorological variables from a nearby weather station. Bulk pollen sedimentation, dominated by Pinus (pine) and Quercus (oak), followed a clear seasonal pattern that peaked during the spring/summer, coinciding with maximum temperature and precipitation, minimum relative humidity and moderate winds from the SSE. Pollen sedimentation lags (PSL) were observed formost pollen types, as substantial amounts of pollen were found in the traps outside of their respective flowering seasons. Two pollen assemblages were clearly differentiated by their taxonomic composition, corresponding to spring/summer and fall/winter. This pattern is consistent with existing interpretation of the sediment varves, specifically, that varves are formed by two-layer couplets that represent the same seasonality as pollen. We concluded that pollen sedimentation in Lake Montcorte`s exhibits a strong seasonal signal in the quantity of pollen, the taxonomic composition of the pollen assembalges, and relationships between the pollen and meteorological variables. Thus, varved sediments provide a potentially powerful tool for paleoecological reconstruction at seasonal resolution. This method could be used not only to identify paleoenvironmental trends, but also to identify annual layers and therefore date sediments, even in the absence of evident sediment laminations. A satisfactory explanation of PSL will require further studies that examine internal lake dynamics and pollen production/dispersal patterns.This work was funded by the Ministry of Economy and Competitivity (project MONT-500; reference CGL2012-33665; PI: Teresa Vegas-Vilarru´bia).Peer reviewe

Seasonal patterns of pollen sedimentation in Lake Montcortès (Central Pyrenees) and potential applications to high-resolution paleoecology: a two-year pilot study.

Lakes with varved sediments are especially well suited for paleoecological study, from annual to even seasonal resolution. The interpretative power of such high-resolution paleoenvironmental reconstructions relies on the availability of modern analogs with the same temporal resolution. We studied seasonal pollen sedimentation in varved Lake Montcorte`s, Central Pyrenees (Spain), as a modern analog for highresolution reconstruction of Late Holocene vegetation and landscape dynamics. Seasonal samples were obtained from sediment traps that were submerged near the maximum water depth for a 2-year period (fall 2013 to fall 2015). Seasonal pollen sedimentation was compared with meteorological variables from a nearby weather station. Bulk pollen sedimentation, dominated by Pinus (pine) and Quercus (oak), followed a clear seasonal pattern that peaked during the spring/summer, coinciding with maximum temperature and precipitation, minimum relative humidity and moderate winds from the SSE. Pollen sedimentation lags (PSL) were observed for most pollen types, as substantial amounts of pollen were found in the traps outside of their respective flowering seasons. Two pollen assemblages were clearly differentiated by their taxonomic composition, corresponding to spring/summer and fall/winter. This pattern is consistent with existing interpretation of the sediment varves, specifically, that varves are formed by two-layer couplets that represent the same seasonality as pollen. We concluded that pollen sedimentation in Lake Montcorte`s exhibits a strong seasonal signal in the quantity of pollen, the taxonomic composition of the pollen assembalges, and relationships between the pollen and meteorological variables. Thus, varved sediments provide a potentially powerful tool for paleoecological reconstruction at seasonal resolution. This method could be used not only to identify paleoenvironmental trends, but also to identify annual layers and therefore date sediments, even in the absence of evident sediment laminations. A satisfactory explanation of PSL will require further studies that examine internal lake dynamics and pollen production/dispersal patterns

Paradigmenwechsel in der Arbeitsmarkt- und Sozialpolitik?

<div><p>Climate change is forcing many plant species to shift their range in search of adequate environmental conditions, being localized endemic species particularly at risk on mountain summits. The Pantepui biogeographic province, a set of flat-topped mountain summits (called <i>tepuis</i>) of northern South America, contains both high plant diversity and a high degree of endemism. Previous studies based on warming projections for the area suggested that half of the Pantepui endemic flora would disappear due to habitat loss by 2100. In this study, we selected one of the best-explored tepuis, Roraima-tepui, to establish the baseline of diversity and endemism for comparisons with historical data and future monitoring surveys, aimed at testing the hypothesis of upward migration of plants in response to global warming. We also analysed floristic and physiognomic features of the Eastern Tepui Chain (ETC, the mountain range where Roraima is located), and the phytogeographic patterns of both the ETC and Pantepui. The Roraima summit contains 227 species, including 44 new records, 13 exotic species (some of them with high invasive potential), and at least one species new to science. At the ETC level, Roraima is the tepui with highest species richness and degree of endemism, and shows a relatively high floristic similarity with Kukenán and Ilú. Herbaceous species dominate over shrubs on these tepuis, Tramen and Maringma, whereas on Yuruaní, Karaurín and Uei, they reach similar abundances. At the Pantepui level, endemic species have highly localized distribution patterns (17% local endemics). Conservation opportunities are evaluated in light of these results.</p></div

Modern Analogue Approach Applied to High-Resolution Varved Sediments-A Synthesis for Lake Montcortès (Central Pyrenees)

In Quaternary paleosciences, the rationale behind analogical inference presupposes that former processes can be explained by causes operating now, although their intensity and rates can vary through time. In this paper we synthesised the results of di erent modern analogue studies performed in a varved lake. We discuss their potential value to obtain best results from high resolution past records. Di erent biogeochemical contemporary processes revealed seasonality and year-to-year variability, e.g., calcite precipitation, lake oxygenation, production and deposition of pollen and phytoplankton growth. Fingerprints of the first two of these processes were clearly evidenced in the varve-sublayers and allow understanding related to past events. Pollen studies suggested the possibility of identifying and characterizing seasonal layers even in the absence of varves. Marker pigments in the water column were tightly associated with phytoplankton groups living today; most of them were identified in the sediment record as well. We observed that 50% of these marker pigments were destroyed between deposition and permanent burying. In another study, seasonality in the production/distribution of branched glycerol dialkyl glycerol tetraethers (brGDGTs) and derived temperature estimates were investigated in catchment soils and particles settling in the lake. The signatures of brGDGTs in depositional environments mainly were representative of stable conditions of soils in the catchment that last over decades; no brGDGTs seemed to be produced within the lake. The main contribution of this review is to show the advantages and limitations of a multiproxy modern-analogue approach in Lake Montcortès as a case study and proposing new working hypotheses for future research

Flora and vegetation of the Guayana highlands : past dynamics, global warming and conservation guidelines; Flora i vegetació de les Terres de Guayana : dinàmica del passat, escalfament global i directrius de conservació

This thesis is aimed at the study of the flora and vegetation of the Guayana Highlands (GH), a set of -50 table mountains (called tepuis) located in the Guayana Shield of northern South America. Special emphasis is put on the potential upward migration of vascular plants as a response to global warming and the suggestion of conservation strategies. The tepui summits contain exceptional diversity and endemism of vascular plants, with more than 2400 known species, of which 30% would be endemics. In this study, the results of the Altitudinal Range Displacement analysis suggest that 30-50% of the GH endemic species could disappear due to total habitat loss by 2100 according to the most optimistic (B1) and pessimistic (A2) warming scenarios, respectively. An Environmental Impact Value has been calculated for each threatened species for a subsequent classification of these species into priority categories (10 for B1 and 13 for A2), which should be used in a chronological sequence to guide conservation and research actions. Subsequently, flora and vegetation approaches have been applied for the verification of the migratory phenomenon in the GH. Since this verification is based on the comparison of inventories conducted at different times, the first necessary step is to establish a baseline. The Roraima-tepui summit (2810 m elevation) has been selected for that purpose, as it is the best well-known tepui from the botanical point of view. The floristic survey of this tepuian summit has yielded 227 species, including 44 novelties since the publication of the Flora of the Venezuelan Guayana, one species new for science (Epidendrum sp. nov.), and 13 exotics, among which Poa annua and Polypogon elongatus (Poaceae) show the highest invasive potential. Five main plant communities have been identified: three herbaceous, one shrubland, and one forest formation, with their corresponding diagnostic species. An environmental characterization of these communities has been also performed. Finally, palaeoecological records may provide valuable information of the species' responses to past environmental changes, which is not available from short-term ecological observations. In this thesis, a palynological analysis of a sedimentary sequence from Uei-tepui (2150 m elevation) has been conducted to record the vegetation changes occurred in the last 2000 years in this tepui and to investigate the potential drivers involved. At -810 cal yr BP (AD 1140), a peak of fire incidence, coeval with a decrease in regional precipitation, reduced the woody elements of meadows (mainly Biophytum) and the Bonnetia cloud forests. Forest recovery to its previous abundance occurred slowly and elapsed several centuries to be completed after fire disturbance. In the mid-18th century, forests and meadows were replaced by Cyrilla racemiflora shrublands, coinciding with intense fires, synchronous with the arrival of Europeans to the Gran Sabana (GS) uplands. These results suggest that fire has been the main factor in the shaping of Uei¬tepui vegetation during the last two millennia. The documented local fire events were most likely caused by human activities and reached the summit from the GS, probably favoured by climatic conditions. The last local fire leading to forest clearing and the establishment of present-day vegetation most likely took place in the AD 1920s. The preservation of the GH flora in front of global warming should be addressed, at least partially, through ex situ conservation techniques, due to the nature of the threat (habitat loss).Proyectos BIOCON 08-188/09 y BIOCON 2004-90/05 (Fundación BBVA); CGL200907069-BOS (Ministerio de Ciencia e Innovación) CGL-200600974-BOS (Ministerio de Educación y CienciaPeer Reviewe

Flora and vegetation of the Guayana highlands : past dynamics, global warming and conservation guidelines = Flora i vegetació de les Terres de Guayana : dinàmica del passat, escalfament global i directrius de conservació

Aquesta tesi té com a objectiu l'estudi de la flora i la vegetació de les Terres Altes de Guayana (TAG), un conjunt de -50 muntanyes tabulars (anomenades tepuis) situades al nord d'Amèrica del Sud, amb especial èmfasi en la potencial migració altitudinal de les plantes vasculars com a resposta a l'escalfament global. Els cims dels tepuis contenen una diversitat i endemisme de plantes vasculars excepcional. Aquest estudi suggereix que el 30-50% de les espècies endèmiques de les TAG podrien desaparèixer per pèrdua total d'hàbitat cap a l'any 2100 segons els escenaris d'escalfament B1 (més optimista) i A2 (més pessimista), respectivament. S'ha calculat un Valor d'Impacte Ambiental per a cada espècie amenaçada per a la posterior classificació d'aquestes espècies en categories de prioritat (10 pel B1 i 13 per l'A2), les quals haurien de ser utilitzades en una seqüència cronològica per orientar les accions de conservació i recerca. Posteriorment, s'ha establert una línia base de diversitat florística, endemisme i vegetació al cim del Roraima-tepui per a la verificació del fenomen migratori a les TAG. L'inventari florístic d'aquest cim tepuià conté 227 espècies, incloent 44 nous registres, una espècie nova per a la ciència i 13 espècies exòtiques. S'han identificat cinc tipus de comunitats vegetals principals, amb les seves corresponents espècies diagnòstiques. També s'ha dut a terme una caracterització ambiental d'aquestes comunitats. Finalment, l'estudi paleoecològic de la seqüència sedimentària del Uei-tepui ha permès documentar la resposta de les espècies als canvis ambientals dels últims 2000 anys. Els resultats suggereixen que el foc ha estat el principal factor que ha modelat la vegetació del Uei durant aquest període. Els esdeveniments de focs locals molt probablement van ser causats per activitats humanes i van assolir el cim des de la Gran Sabana afavorits per les condicions climàtiques. La preservació de la flora de les TAG enfront de l'escalfament global s'hauria d'adreçar, com a mínim parcialment, mitjançant tècniques de conservació ex situ, a causa de la naturalesa de l'amenaça (pèrdua d'hàbitat). No obstant, la documentació en aquest estudi d'altres impactes humans (trepig de la vegetació, espècies exòtiques, canvis en les propietats del sòl, etc.) i l'aparició del foc com a potencial agent pertorbador del bioma tepuià posen de manifest que la conservació in situ mitjançant àrees protegides pot ser també molt important.This thesis is aimed at the study of the flora and vegetation of the Guayana Highlands (GH), a set of -50 table mountains (called tepuis) located in the Guayana Shield of northern South America. Special emphasis is put on the potential upward migration of vascular plants as a response to global warming and the suggestion of conservation strategies. The tepui summits contain exceptional diversity and endemism of vascular plants, with more than 2400 known species, of which 30% would be endemics. In this study, the results of the Altitudinal Range Displacement analysis suggest that 30-50% of the GH endemic species could disappear due to total habitat loss by 2100 according to the most optimistic (B1) and pessimistic (A2) warming scenarios, respectively. An Environmental Impact Value has been calculated for each threatened species for a subsequent classification of these species into priority categories (10 for B1 and 13 for A2), which should be used in a chronological sequence to guide conservation and research actions. Subsequently, flora and vegetation approaches have been applied for the verification of the migratory phenomenon in the GH. Since this verification is based on the comparison of inventories conducted at different times, the first necessary step is to establish a baseline. The Roraima-tepui summit (2810 m elevation) has been selected for that purpose, as it is the best well-known tepui from the botanical point of view. The floristic survey of this tepuian summit has yielded 227 species, including 44 novelties since the publication of the Flora of the Venezuelan Guayana, one species new for science (Epidendrum sp. nov.), and 13 exotics, among which Poa annua and Polypogon elongatus (Poaceae) show the highest invasive potential. Five main plant communities have been identified: three herbaceous, one shrubland, and one forest formation, with their corresponding diagnostic species. An environmental characterization of these communities has been also performed. Finally, palaeoecological records may provide valuable information of the species' responses to past environmental changes, which is not available from short-term ecological observations. In this thesis, a palynological analysis of a sedimentary sequence from Uei-tepui (2150 m elevation) has been conducted to record the vegetation changes occurred in the last 2000 years in this tepui and to investigate the potential drivers involved. At -810 cal yr BP (AD 1140), a peak of fire incidence, coeval with a decrease in regional precipitation, reduced the woody elements of meadows (mainly Biophytum) and the Bonnetia cloud forests. Forest recovery to its previous abundance occurred slowly and elapsed several centuries to be completed after fire disturbance. In the mid-18th century, forests and meadows were replaced by Cyrilla racemiflora shrublands, coinciding with intense fires, synchronous with the arrival of Europeans to the Gran Sabana (GS) uplands. These results suggest that fire has been the main factor in the shaping of Uei¬tepui vegetation during the last two millennia. The documented local fire events were most likely caused by human activities and reached the summit from the GS, probably favoured by climatic conditions. The last local fire leading to forest clearing and the establishment of present-day vegetation most likely took place in the AD 1920s. The preservation of the GH flora in front of global warming should be addressed, at least partially, through ex situ conservation techniques, due to the nature of the threat (habitat loss). However, the documentation in this study of other human impacts (trampling on vegetation, exotic species, changes in soil properties, etc.) and the emergence of fire as a potential disturbing agent of the GH biome highlight that in situ conservation through protected areas may also be very important. A management plan with the involvement of local indigenous communities should be implemented in the GH region (i.e., lowlands, uplands and highlands), in order to reduce the risks posed by global warming, human impacts, and the potential synergy among them

L’escalfament global i l’extinció de les plantes: un exemple tropical

14p.; Grafs.; Fots. col.[EN]Global warminG and plant extinction: a tropical example. – Pantepui is a phytogeographical province made up of a group of approximately 50 tabular mountain summits or tepuis in southeast Venezuela. This region lies between 1500 and 3014 m a.s.l and covers an approximate area of 6000 km2. Its pristine state of conservation is remarkable. The summits of the tepuis contain an excep- tional level of vascular plant diversity, including 2446 known species, of which 771 are endemic to Pantepui. It is expected that the ongoing effects of global warming will produce upward displace- ments of summit taxa, which could result in the extinction of certain species due to habitat loss. This study is an assessment of the potential extinction risk during the 21st century due to global warming. In order to determine those species that will potentially become extinct during each time frame (2011-2030, 2046-2065 and 2080-2099), we used Altitudinal Range Displacement (ARD) analysis and different scenarios to forecast expected temperatures, as predicted by the Intergov- ernmental Panel on Climate Change (IPCC). The ARD results revealed that at least 169, and up to 321, endemic species would lose their habitat by the end of this century based on the more con- servative and pessimistic scenarios, respectively. In light of these results, a number of in situ and ex situ conservation alternatives are discussed. In situ conservation by means of protected areas does not appear be a viable option because of the upward habitat displacement that would occur. Conversely, ex situ conservation techniques (seed or pollen banks, in vitro culture, collections un- der cultivation, etc.) have great potential to preserve the species discussed herein.Aquest tre- ball ha estat finançat pel Programa de Conser- vació de la Biodiversitat de la Fundació BBVA, i s’emmarca dins del projecte “Conservació de la biodiversitat enfront de l’escalfament global a les Terres Altes de Guayana (nord d’Amèrica del Sud). Fase II: migracions recents i futures (PANTEPUI-II)”, amb seu a l’Institut Botànic de Barcelona (CSIC) (ref. BIOCON08-031).Peer reviewe