The stratification of bird species along elevational gradients is widely reported, with montane bird communities typically characterized by distinctive species occurring in relatively small and isolated populations; as such, these species are the subject of considerable interest to ecologists and conservationists. The stratification of species along elevation is largely attributed to compressed climatic zonation. Recent evidence that bird species are shifting up in elevation has fueled speculation that these species are tracking their climactic niches in response to climate change. However, there is also evidence plant communities are shifting in elevation, presenting a potential additional mechanism explaining changes observed in the bird community. Uncertainty as to the degree to which climate directly influences bird abundance versus the degree to which climate indirectly influences bird abundance via habitat composition and structure represents a key impediment to understanding the ecology of these species in montane environments. To address this question I measured species abundance, habitat characteristics, and temperature at 150 survey points located along 15 elevational transects in the Presidential Mountains of New Hampshire in the summers of 2014 and 2015. I used N-mixture models to correct for imperfect detection of species and structural equation models, incorporating abundance, habitat, temperature, and precipitation derived from a downscaled regional dataset to assign variation to the direct and indirect effects of climate upon birds. Analysis of 21 species revealed species-specific patterns on how climate exerts direct effects and indirect effects mediated by forest composition and structure on bird abundance. This work represents an important contribution to the ecological understanding of the pathways by which climate influences bird abundance. Finding that 62% of species experience both direct and indirect effects of climate, with 62% experiencing stronger direct than indirect effects, these results underscore the vulnerability of these species to climate change. With 81% of species found to experience indirect effects of climate via forests, these findings indicate great conservation value of maintaining forest habitat amidst climate change. Overall, this information will facilitate the refinement of predictive models of the abundance of montane bird species and represents an approach that will advance future investigations of climate effects in the Northern Appalachians and other systems.

The tropical montane forest of Ecuador is one of the ‘hot spots’ of species diversity. Despite this great species diversity, there are forests in our study area, namely in the Zamora-Chinchipe province in southern Ecuador, which are being depleted at an alarming rate. For example, large areas are being permanently deforested for use as ‘pastureland ’. This development is typically characterized by intensive slash and burn activities for vegetation clearance. After clear cut and slash burning, pasture species are planted of which Setaria sphacelata and Melinis minutiflora, are the most common. However, forest clearing by slash burn for pasture production occurs in the region simultaneously with subsequent invasion of bracken fern (Pteridium arachnoideum) and re-colonization of secondary succession vegetation on abandoned pasture land. In this study, we will examine the effects that the above phenomena have on ecosystems, namely the effects associated with the conversion of natural forestland to pasture land, and the succession that occurs as a result. We will also examine how land use change affects the nutrient status of the soil. This study focuses specifically on the area called the ‘San Francisco Valley’, (3°58’ 30”S latitude, 79°4’ 25”W longitude), which lies between Loja and the Zamora-Chinchipe provinces in Ecuador. Field work for this study was carried out at 1,798 and 2,226 m a.s.l in the following sites: 1) the San Francisco Natural Forest (this area refers to the eastern part of Podocarpus National Park); 2) active pastures Type I (this area refers to the pastureland in front of the San Francisco Scientific Station ECSF, and are pastures that have existed for 50 years or more); 3) active pastures Type II (this area refers to the pastureland in Sabanilla sites, and are pastures that have existed for approximately 17 years); and 4) abandoned pastureland (affected by succession over a period of at least twenty years). Each land-use type consists of five plots of approximately 20 x 20m2. Five points in each plot were then chosen and later sampled (two sub-samples) according to the defined horizons and depth units, namely the organic layer and mineral top soil horizons. Organic layer (only on forest and succession sampling plots) were designated as LOf1, Of2/Oh1 and mineral top soil was sampled to a depth of a 0-10, 10-20, 20-30 cm. To quantify the effects of the impact that land use change has on the chemical characteristics of soil in the selected areas, we analyzed the following bio-elements: the pH value, soil organic carbon (SOC), the total nitrogen (TN), the effective cation exchange capacity (ECEC), as well as stocks of total and available macronutrients. In addition, we examined the biological characteristics such as carbon and nitrogen microbial biomass (MBC, MBN), basal respiration (BR), and nitrogen mineralization (Nmin) in organic layers and top mineral soils (0-30 cm) of the following: the San Francisco Natural Forest, ECSF pastureland, Sabanilla pastureland, and abandoned pastures affected by succession. The main results of this study can be summarised as follows: The soil pH value increased after forest-to-pasture conversion and tended to decrease with soil depth. Moreover, pastureland in the study that was fifty years or more, showed evidence of a decrease in pH values. This decrease in pH value of the soil can be attributed to the reduction in exchangeable cations . However, they still remained higher than the pH values for the forest sites in the study. After the abandonment of pastureland, we observed a re-acidification in the soil of succession sites. This resulted in a decrease of base saturation . On the other hand, the total exchangeable base cation stocks were significantly higher for pasture soils compared with forest and succession soils. This was because of the addition of basic cations by ‘slash and burn activity ’. In this study, we observed that the greater values of soil organic carbon stocks occurred in forest sites. This can be explained by their high SOC value in the organic layer (73.9 Mg ha-1). However, the mineral layer (0 to 30 cm depth) of forest had a lower value than pasture and succession sites. This higher SOC stock of the mineral layer of our pasture sites are partly a result of carbon input from the former standing biomass. Likewise, in the mineral layers, we found that MBC content increases in a similar way to the SOC content. For example, when we compared the MBC content of forests with the pasture sites, we observed that pastures had approximately three times as much MBC. The results of nitrogen stored in the Microbial Biomass (MBN) showed the same tendency as the MBC values. Moreover, for organic layers, the total nitrogen stocks of forest were higher compared to succession sites. On the other hand, for mineral soil (0 to 30 cm depth), nitrogen stocks increased after forest to pasture conversion. This increase is partly due to the burning of aboveground biomass and the subsequent death of roots. Furthermore, the values of nitrogen stocks decreased again in succession sites (4.2 Mg N. ha-1), with similar values those of forests (4.4 Mg N. ha-1 ). Our results show that the slash-and-burn practice leads to a significant increase of P stock. We found that stocks of total phosphorus were significantly higher in the mineral topsoil (0–30 cm) of 50 year-old pastures (ECSF) than in the 17 year-old pastures (Sabanilla). It is important to note that the P stocks in the mineral soil of the abandoned pasture (20 year-old pasture sites) tend to return to forest values (399.9. Kg.ha-1). Nevertheless, the results show very low values of available P on both pastures and succession sites compared with forest sites. In the organic layers, our results show significant differences in the values of basal respiration between forest and succession sites. This indicates that the level of CO2 was greater in the selected forestland due to an increase of organic material. This essentially means that there was an increase of micro-organisms in the soil and subsequently an improved nutrient cycle . For the mineral soil, however, the results only showed a significant difference of 0-10 cm depth in the ECSF pastures and forests. In our study, we did not find any significant differences in the net nitrogen mineralization values in the four studied areas. Nevertheless, the results show that net nitrogen mineralization values decrease systematically according to the depth of the land uses. Summarizing, after the conversion of forest to pasture, there was an increase of the value of bio-elements in the mineral layers at both pasture sites. However, this increase was higher in 50 year old pastures (ECSF) than in the 17 year old pastures (Sabanilla). In addition, we noticed that after 20 years of the abandonment of pastures, most measured soil properties returned to the old-growth forest levels. / El bosque montano tropical de Ecuador es uno de los \"puntos calientes\" de diversidad de especies. Pero el bosque primario en el área de investigación (la provincia de Zamora Chinchipe al Sur de Ecuador) se está perdiendo a un ritmo alarmante. Grandes áreas están siendo permanentemente deforestadas para su uso como tierras de pastoreo. Este proceso se caracteriza por el uso intensivo de fuego para desmonte de la vegetación. Después de la quema y roza, se plantan especies de pastos entre las que Setaria sphacelata y Melinis minutiflora son las más comunes. Sin embargo, la quema y tala del bosque para la conversión a zonas de pastos ocurre simultáneamente con la subsecuente invasión del helecho común (Pteridium arachnoideum), produciéndose. La difusión de esta maleza y la decreciente productividad de los pastos (especialmente Setaria spacelata y Melinis minutiflora) conducen a que las tierras se utilizan en pastoreo hasta que la tierra se agota de nutrientes y luego se abandonan. En este estudio, se examinan los efectos que los fenómenos anteriormente mencionados tienen sobre los ecosistemas; a saber, los efectos asociados a la conversión de bosques naturales en tierras de pastoreo y la posterior sucesión de los pastizales; además de cómo el cambio de uso del suelo afecta el estado nutricional de los suelos del sur del Ecuador. El estudio se sitúa en la zona del valle de San Francisco (3°58’ 30”S latitud, 79°4’ 25”W longitud), entre Loja y Zamora Chinchipe, provincias que se encuentran en el sur de Ecuador. El trabajo de campo se llevó a cabo a una altura entre 1,798 y 2,226 m s.n.m.; en: 1) las áreas de bosque natural San Francisco (esta área se refiere a la parte oriental del Parque Nacional Podocarpus); 2) pasto activos Tipo I (esta área se refiere a los pastos en frente de la Estación Científica San Francisco ECSF, y son pastizales que tienen más de 50 años de edad); 3) pastos activos Tipo II (esta área se refiere a los pastos en los sitios de Sabanilla, y son pastizales que existen desde hace aproximadamente 17 años); y 4) pastos abandonados bajo vegetación de sucesión (más de 20 años de edad). Cada tipo de uso de la tierra consistió en cinco parcelas de aproximadamente 20 x 20 m2; se eligieron cinco puntos en cada parcela y se tomaron muestras (dos sub-muestras) de acuerdo con los horizontes orgánico y mineral. Las capas Orgánicas (solo presentes en el bosque y en los sitios de sucesión) se identificaron como LOf1, Of2/Oh1 y las capas minerales se muestrearon hasta los 0-30 cm de profundidad del suelo. Para cuantificar los efectos del impacto del cambio del uso de la tierra en las características químicas del suelo, se analizó los siguientes bio-elementos: pH, carbono orgánico del suelo (COS), nitrógeno total (Nt), la capacidad de intercambio catiónico efectiva (CICE), así como las reservas del contenido total y disponibilidad de los macro nutrientes. Además, las características biológicas, tales como el carbón (MBC) y nitrógeno (MBN) de la biomasa microbiana, la respiración basal (Rb) y la mineralización de nitrógeno (Nmin) en las capas orgánicas y en la capa mineral del suelo (hasta -30 cm) de los bosques naturales, pastos y pastizales abandonados bajo vegetación de sucesión. Los principales resultados del estudio se describen a continuación: El valor de pH del suelo indica una elevada acidez, después de la conversión de bosque a pastos y tiene una tendencia general a disminuir con la profundidad del suelo, cuando los pastos se hacen más viejos (más de 50 años de edad); los valores de pH del suelo disminuye como consecuencia de la lixiviación de cationes intercambiables, pero siguen siendo superiores a los valores de pH de los sitios del bosque. Tras el abandono de los pastos se observó una re-acidificación en el suelo de los sitios de sucesión, lo que resulta en una disminución de la saturación de bases. Los resultados además indican que las capas orgánicas, especialmente en los suelos de los bosques, almacenan una cantidad importante de potasio, calcio y magnesio. Sin embargo, las reservas totales de cationes básicos intercambiables fueron significativamente mayores en los suelos de los pastizales que en los bosques y que los suelos de sucesión, debido a la adición de cationes básicos producidos por la tala y quema usada en la conversión de bosques a pastizales. En este estudio, se encontró que los mayores valores de reservas de COS se producen en zonas forestales, que se corresponde con un alto valor en la capa orgánica (73,9 Mg C ha-1). Sin embargo, la capa mineral (hasta - 30 cm de profundidad) de los suelos del bosque tiene un valor menor en comparación con los valores de los pastos y sucesión. Este alto contenido de COS en los pastos, se debe en parte al ingreso de carbono desde la biomasa. Asimismo, en las capas minerales, se encontró que el contenido de carbono en biomasa microbiana (CBM) aumenta de una manera similar al contenido de carbono orgánico del suelo (COS). Por ejemplo, cuando comparamos el contenido de CBM de los bosques con los sitios de pastoreo, se observó que los pastos tenían aproximadamente tres veces más MBC. El resultado de nitrógeno almacenado en la biomasa microbiana (NBM) mostró la misma tendencia que los valores de CBM. En las capas orgánicas, las reservas totales de nitrógeno de los bosques fueron mayores en comparación con los sitios de sucesión. Por otro lado, en el suelo mineral (hasta -30 cm de profundidad) las reservas de nitrógeno aumentan después de la conversión de bosques a pastizales. Este incremento es parte debido a la quema de la biomasa superior y de la subsecuente muerte de las raíces. Además, los valores de las reservas de nitrógeno disminuyen de nuevo en los sitios de sucesión (4.2 Mg N. ha-1), a valores similares a las del bosque (4.4 Mg N. ha-1 ). Nuestros resultados muestran que las prácticas de quema y tala incrementan significativamente las reservas de fosforo, encontramos que las reservas de fosforo total fueron significativamente altas en las capas minerales (- 30 cm) de los pastos de 50 años (ECSF), seguido de los pastos de 17 años de edad (Sabanilla). Es importante notar que las reservas de fosforo en las capas minerales de los suelos de pastos abandonados (20 años de edad) tienden a retornar a los valores del bosque (399.9. Kg.ha-1). Sin embargo, los resultados muestran valores muy bajos de fosforo disponible en ambos sitios de pastos y sucesión comparado con el bosque. En las capas orgánicas, los resultados revelan diferencias significativas en los valores de la respiración basal (potencial) entre el bosque y la sucesión. Esto indica que el nivel de CO2 fue mayor en el los sitios de bosque debido a un aumento de la materia orgánica. Esto implica un aumento de los microorganismos en el suelo y, posteriormente, una mejora en el ciclo de nutrientes. En el suelo mineral, los resultados sólo muestran una diferencia significativa en la profundidad de 0-10 cm entre los pastos ECSF con los bosques. En nuestro estudio, no se encontró diferencias significativas en los valores de mineralización neta de nitrógeno entre las cuatro áreas estudiadas. Sin embargo, los resultados muestran que los valores netos de mineralización del nitrógeno disminuyen sistemáticamente con la profundidad en todos los usos de los suelos estudiados. En resumen, después de la conversión de bosques en pastizales, se produjo un incremento del valor de los bio-elementos en las capas minerales de ambos sitios de pastoreo. Sin embargo, este aumento fue mayor en los pastos de 50 años de edad (ECSF) que en los pastos de 17 años de edad (Sabanilla). Además, los resultados muestras que después de 20 años del abandono de los pastos, la mayoría de los parámetros medidos retornan a valores similares a los de los sitios de bosque. / Im globalen Kontext stellt der tropische Bergregenwald in Süd-Ecuador ein „Hotspot“ der Biodiversität dar. Im Untersuchungsgebiet ist die enorme Artenvielfalt durch die massive Zerstörung der natürlichen Waldökosysteme gefährdet. Der Wald wird durch intensive Brandrodung großflächig in Weideland umgewandelt. Im Laufe der Weidenutzung kommt es auf den Weideflächen zu einer zunehmenden Ausbreitung und Dominanz des tropischen Adlerfarns (Pteridium arachnoideum). Die Farnausbreitung und die abnehmende Produktivität der Weidegräser insbesondere von Setaria sphacelata und Melinis minutiflora, führt zum Verlassen der Weiden und zur Etablierung neuer Weideflächen durch fortgesetzte Brandrodung des Naturwaldes. Aufgelassene ehemalige Weideflächen unterliegen einer sekundären Sukzession. Innerhalb dieser Studie wurden die Effekte der Umwandlung des Naturwaldes in Weideland, der Weidenutzung sowie der Wirkungen der sekundären Sukzession nach dem Verlassen unproduktiver Weideflächen auf die Nährstoffsituation der Böden untersucht. Die Untersuchung erfolgte im Gebiet des „San Francisco Tales“, (3°58’ 30”S, 79°4’ 25”W), welches sich zwischen den beiden Provinzen Loja und Zamora-Chinchipe in Ecuador befindet. Feldarbeiten innerhalb dieser Studie wurden in einer Höhe zwischen 1798 und 2225 m NN in den folgenden Bereichen ausgeführt: 1) Naturwald in San Francisco; 2) aktive Weidefläche Typ I (seit circa 50 Jahren in Nutzung); 3) aktive Weidefläche Typ II (seit circa 17 Jahren in Nutzung); und 4) verlassenes Weideland (bestimmt durch sekundäre Sukzession seit mindestens 20 Jahren). Jeder Landnutzungstyp besteht aus fünf Plots mit einer Ausdehnung von circa 20 x 20 m. Fünf Punkte innerhalb eines jeden Plots wurden zur Beprobung ausgewählt. Die organische Auflage (Naturwald, verlassenes Weideland) wurde nach Auflagehorizonten (LOf1 und Of2/Oh) und der Mineralboden nach Tiefenstufen (0-10 cm, 10-20 und 20-30 cm) getrennt beprobt. Um die Effekte und den Einfluss des Landnutzungswandels auf chemische Bodenkennwerte zu quantifizieren, wurden die folgenden Indikatoren untersucht: pH, organischer Kohlenstoffgehalt des Bodens (SOC), Gesamtstickstoff (TN), effektive Kationenaustauschkapazität (CECeff) sowie Vorräte der gesamten und pflanzenverfügbaren Makronährelemente. Zusätzlich wurden bodenbiologische Indikatoren wie Kohlenstoff und Stickstoff der mikrobiellen Biomasse (MBC, MBN), Basalatmung (BR) und Stickstoffmineralisation (Nmin) in den organischen Auflagehorizonten und dem mineralischen Oberboden (0-30 cm) wie folgt untersucht: Naturwald in San Francisco, ECSF Weideflächen, Sabanilla Weideflächen und aufgelassene, von der Sukzession beeinflusste Weiden. Die hauptsächlichen Resultate der Untersuchung können wie folgt zusammengefasst werden: Der pH-Wert des Bodens erhöhte sich nach der Umwandlung von Wald zu Weide und zeigt mit zunehmender Tiefe einen abnehmenden Trend. Darüber hinaus nahmen die pH-Werte von der 17 Jahre alten zur 50 Jahre alten Weide ab. Diese Abnahme kann auf den Rückgang austauschbarer Kationen zurückgeführt werden. Dennoch verblieb der pH-Wert in den 50 Jahre alten Weiden oberhalb des pH-Wertes der im Wald beprobten Flächen. Nach dem Auflassen der Weiden wurde eine erneute Versauerung des Bodens im Stadium der Sukzession beobachtet. Dieser pH-Rückgang wird durch einen Abnahme der Basensättigung begleitet. Auf der anderen Seite waren die Vorräte an austauschbaren Basen der CECeff auf den Weideflächen signifikant über denen der Wald- und Sukzessionsflächen. Ursächlich dafür war die Freisetzung basischer Kationen während der Brandrodung des Naturwaldes. Innerhalb dieser Studie wurden die höchsten Vorräte an Bodenkohlenstoff im Naturwald ermittelt. Das kann durch hohe Vorräte an SOC in der organischen Auflage (73.9 Mg ha-1) erklärt werden. Allerdings waren die Vorräte im Mineralboden (0-30 cm) des Waldes geringer als auf den Weide- und Sukzessionsflächen. Diese höheren SOC-Vorräte im Mineralboden der Weideflächen sind teilweise das Resultat der höheren Kohlenstoffzufuhr durch Reste der oberirdischen Biomasse. Der Gehalt an mikrobiellem Biomassekohlenstoff nahm in ähnlicher Art und Weise wie der des bodenbürtigen organischen Kohlenstoffs zu. Beispielsweise wurde beim Vergleich von MBC und MBN-Gehalten des Waldes mit denen der Weide der dreifache Gehalt in der Weide gefunden. Außerdem waren die Stickstoffvorräte der organischen Auflagen im Wald höher als auf den Sukzessionsflächen. Andererseits nahmen die Stickstoffvorräte nach der Umwandlung von Wald zu Weide im Mineralboden (0-30 cm) zu. Diese Zunahme beruht zum Teil auf dem Abbrennen der oberirdischen Biomasse und dem anschließenden Absterben der Wurzeln. Des Weiteren verringerten sich die Stickstoffvorräte im Stadium der Sukzession (4.2 Mg N ha-1) und glichen sich wieder denen des Waldes (4.4 Mg N ha-1) an. Die Resultate zeigen, dass die Brandrodung zu einem signifikanten Anstieg der Phosphorvorräte führte. Vorräte des Gesamtphosphors waren in den mineralischen Oberböden (0-30 cm) der 50 Jahre alten Weide, gefolgt von der 17 Jahre alten Weide signifikant am höchsten. Zu betonen ist, dass die P-Vorräte im Mineralboden der aufgelassenen Weide dazu tendieren auf Werte des Waldes abzusinken (399.9 kg ha-1). Trotzdem zeigten die Ergebnisse sehr geringe Werte für pflanzenverfügbaren Phosphor in Weide und Sukzession im Vergleich zum Wald. In den organischen Auflagehorizonten wurden signifikante Unterschiede in der mikrobiellen Aktivität (Basalatmung) zwischen Wald und Weide gefunden. Das zeigt, dass das Niveau an C-Mineralisierung in der ausgewählten Waldfläche größer ist, was auf die erhöhte Verfügbarkeit der organischen Substanz zurückgeführt werden kann. Das bedeutet im Wesentlichen einen Anstieg der Mikroorganismen in den Böden und darauffolgend einen verbesserten Nährstoffkreislauf. Für den Mineralboden zeigten die Ergebnisse jedoch nur einen signifikanten Unterschied in einer Tiefe von 0-10 cm zwischen Wald und Weide. Signifikante Unterschiede in der Nettostickstoffmineralisation der vier untersuchten Gebiete konnten nicht gefunden werden. Nichtsdestotrotz zeigten die Ergebnisse, dass die Nettostickstoffmineralisation mit zunehmender Tiefe in den unterschiedlichen Landnutzungen abnimmt. Zusammenfassend kann festgestellt werden, dass nach der Brandrodung die Gehalte an Bioelementen im Mineralboden beider Weideflächen zunahmen. Dieser Anstieg war in den 50 Jahre alten Weideflächen (ECSF) sogar ausgeprägter als in den 17 Jahre alten Weideflächen (Sabanilla). Zusätzlich zeigte sich in den 20 Jahre alten Sukzessionsflächen, dass durch die Regeneration einer organischen Auflage ein positiver Effekt hinsichtlich erhöhter Vorräte an SOC und pflanzenverfügbarem Phosphor festgestellt werden konnte. Diese allmähliche Zunahme an Nährstoffen im Boden der Sukzession setzte sich fort, bis das Ausgangsniveau des Waldes wieder erreicht war.

No description available.

Climate change models predict an increase in frequency and amplitude of extreme weather events, including heat waves. To better predict how the composition and distribution of plant assemblages might respond to these changes in temperature, it is important to understand how species currently respond to these extremes. Photosynthetic thermal tolerance (T25)and photosynthetic recovery (RT25) were quantified in 27 species. We also studied the relationships between T25, RT25 and leaf mass per area (LMA). Leaf temperature was also monitored in the field. Leaves used in this study were collected from two distinct environments representing desert and montane plant assemblages. T25 and RT25 were measured using a chlorophyll fluorescence protocol incorporating sub-saturating light and short duration heat stress. Mean T25and LMA were significantly different between environments. Mean RT25 was not significantly different between environments. There was a positive relationship between T25 and LMA in both environments. The ability to recover from heat stress does not differ between two biomes that experience vastly different mean maximum temperatures during the summer months. LMA is a predictive leaf trait for thermal tolerance.

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As comunidades florestais periféricas às florestas que recobrem o sopé e as médias encostas da Serra do Mar apresentam uma convergência de fisionomias e aspectos xeromórficos, sustentada por floras que estão relacionadas quanto às suas origens. Como estas semelhanças podem indicar condições ecológicas similares, o trabalho investigou qualitativa e quantitativamente se as semelhanças fisionômicas, entre a Floresta do Topo dos Morros da Serra do Mar e a Floresta Seca de Restinga no Estado de São Paulo, são acompanhadas por semelhanças florísticas e estruturais. Esta investigação teve como objetivos: caracterizar e comparar, em termos fitossociológicos, as florestas secas de restinga e as florestas do topo das escarpas atlânticas; e analisar as relações entre possíveis padrões florísticos e estruturais do componente arbóreo destas florestas e condições edáficas e climáticas de seus ambientes. A amostragem foi realizada a partir de 10 parcelas de 10 m X 10 m em cada uma das seis áreas de estudo. Para o topo da Serra do Mar considerou-se a floresta nas seguintes Unidades de Conservação: Estação Biológica de Boracéia; Núcleo Curucutu do PESM e Parque Estadual Intervales. Para a floresta seca de restinga, as áreas de estudo foram: Núcleo Picinguaba do PESM, Estação Ecológica Juréia-Itatins e Parque Estadual Ilha do Cardoso. Através da descrição fitossociológica das comunidades e de técnicas de análise multivariada para classificação e ordenação, observou-se que as áreas de floresta do topo das encostas são pouco similares florística e estruturalmente em relação às florestas secas de restinga. As pequenas semelhanças entre as florestas estudadas dizem respeito às espécies de grande plasticidade ecológica e que, por isso, possuem ampla distribuição geográfica. As diferenças florísticas e estruturais foram determinadas pelas espécies oriundas das florestas que recobrem as encostas da Serra do Mar, sendo que nehuma das espécies consideradas importantes é endêmica de um dos tipos florestais, não sustentando, assim, a convergência ecológica. / Plant communities at the periphery of the Atlantic rainforest that recover the lower and middle slopes of Serra do Mar presents a convergence of physiognomy and xeromorphycs aspects, supported by floras that are related on its origins. As these convergence can indicate similar ecological conditions, this present work investigated if the similarities between Upper Slope Forest and the Restinga Forest in the State of São Paulo, Brazil, are followed by floristic and structural similarities. This inquiry had two objectives: characterize and compare the Upper Slope Forest and the Restinga Forest in its phytosociological aspects; analyze the relationships between edaphic and climatic conditions and floristic and structural patterns of the arboreal component of these forests. To characterize the Upper Slope Forest was considered forests in the following Conservation Units: Estação Biológica de Boracéia, Núcleo Curucutu do Parque Estadual da Serra do Mar and Parque Estadual Intervales; and to characterize the Restinga Forest the study areas were in the following Conservation Units: Núcleo Picinguaba do PESM, Estação Ecológica Juréia-Itatins and Parque Estadual Ilha do Cardoso. For structural vegetation analysis, were used 10 plots of 10 x 10 m in each area. The phytosociological description and multivaried analysis of classification and ordination showed that areas of Upper Slope Forest and Restinga Forest have low similarity. The resemblances are based on occurrence of broad ecological plasticity species and, therefore, of wide distribution. On the other hand, the floristic and structural heterogeneity is consequence of the predominance, in each forests type, of different species from the Atlantic rainforest that recover the lower and middle slopes of Serra do Mar, not supporting the ecological convergence hypothesis.

Montane ecosystems cover approximately 22 to 25% of land surface from sea level to more than 8,000 m a.s.l., harboring more than a third of the planet\'s biodiversity and includ half of global biodiversity hotspots. Among geographical gradients (latitudinal or altitudinal), the latitudinal species richness pattern is the most recognized and studied. Although not so intensively studied as latitudinal gradients, altitudinal gradients also provide great patterns of species richness distributions. Despite of the processes that driving the species richness patterns are still poorly understood, three main patterns have been reported along altitudinal gradients: 1) decreasing of species richness with increasing altitude, 2) increase in species richness with increased altitude, and 3) increasing species richness at intermediate altitudes (hump-shaped pattern), followed by a decreasing of species richness with increasing altitude. The hump-shaped pattern is considered the most common. A macroecological hypothesis that to explain species richness patterns along geographical gradients focusing in species range size is Rapoport\'s rule. This rule is a positive correlation between altitude and species range size distribution based on climate seasonality effects. Rapoport\'s rule prediz that species that can withstand broad climatic variability can become more widely distributed along geographical gradients. However, this hypothesis still has presented controversial results and this controversial results increased our interest in testing Rapoport\'s altitudinal rule in Atlantic Forest mountain ecosystems biome. However, patterns and process that drivres community assembly along altitudinal gradients have received little attention and remain controversial. Based on the anuran community strutucture variation (richness, composition and abundance) along altitudinal gradients, the present work aims to understand and disentangle the topographic and climatic effects on spatial patterns distribution and species altitudinal range size in the Atlantic Forest highlands, which will highlight how topographic and climate conditions acting in communities\' assembly along altitudinal gradients subside important rules to biodiversity conservation. / Os ecossistemas montanhosos cobrem aproximadamente 22 a 25% da superfície terrestre desde o nível do mar até mais de 8.000 m, abrigam mais de um terço da biodiversidade do planeta incluindo metade dos hotspots globais de biodiversidade. Entre os gradientes geográficos (latitudinais ou altitudinais), o padrão latitudinal de riqueza de espécies é o mais reconhecido e estudado. Embora não tão intensamente estudados como os gradientes latitudinais, os gradientes altitudinais também fornecem ótimos padrões de distribuição de riqueza de espécies. Apesar dos processos que impulsionam os padrões de riqueza de espécies ainda serem pouco compreendidos, três principais padrões tem sido relatados ao longo dos gradientes altitudinais: 1) decréscimo da riqueza de espécies com o aumento da altitude; 2) aumento da riqueza de espécies com o aumento da altitude and 3) aumento da riqueza de espécies em altitudes intermediárias (unimodal padrão), seguido por uma diminuição da riqueza de espécies com o aumento da altitude. O unimodal padrão é considerado o mais comum. Uma hipótese macroecológica que explica os padrões de riqueza de espécies ao longo de gradientes geográficos com foco no tamanho das faixas altitudinais das espécies é Rapoport regra. Esta prediz uma correlação positiva entre a altitude e a distribuição do tamanho das faixas altitudinais das espécies com base nos efeitos da sazonalidade climática. Rapoport regra prediz que as espécies que podem suportar um ampla variabilidade climática podem se tornar mais amplamente distribuídas ao longo dos gradientes geográficos. No entanto, essa hipótese ainda apresenta resultados controversos o que aumentaram nosso interesse em testar a Rapoport altitudinal regra em ecossistemas montanhosos na Mata Atlântica. Entretanto, os padrões e os processos que conduzem a montagem da comunidade ao longo dos gradientes altitudinais receberam pouca atenção e ainda permanecem controversos. Com base na variação da estrutura da comunidade de anuros (riqueza, composição e abundância) ao longo dos gradientes altitudinais, o presente estudo teve como objetivo compreender e desemaranhar os efeitos topográficos e climáticos nos padrões de distribuição espacial e tamanho das faixas altitudinais das espécies em ecossitemas montanhosos na Mata Atlântica, o qual realçará como as condições topográficas e climáticas atuam na montagem de comunidades ao longo de gradientes de altitude subsidiando importantes regras para a conservação da biodiversidade.

Submitted by Mariana Dornelles Vargas (marianadv) on 2015-05-18T12:06:00Z No. of bitstreams: 1 padroes_estruturais.pdf: 1608201 bytes, checksum: 202eac1edefaff08f88aa686d56f9c59 (MD5) / Made available in DSpace on 2015-05-18T12:06:00Z (GMT). No. of bitstreams: 1 padroes_estruturais.pdf: 1608201 bytes, checksum: 202eac1edefaff08f88aa686d56f9c59 (MD5) Previous issue date: 2011 / Nenhuma / Fatores topográficos afetam as comunidades vegetais em diferentes escalas espaciais agindo como filtros para a distribuição e abundância das espécies. Essa influência é proeminente em ecossistemas montanos. No sul do Brasil as encostas íngremes dos rios da bacia hidrográfica do rio Pelotas abrigam importantes remanescentes florestais montanos, apesar da pressão antrópica histórica exercida pela extração madeireira, agropecuária, silvicultura e nas últimas décadas, principalmente pela exploração hidrelétrica. O represamento de rios é um dos mais proeminentes impactos aos ecossistemas de água doce, com reflexos sobre a vegetação ripária. A construção de reservatórios hidrelétricos em rios montanos com vales estreitos como aqueles da bacia hidrográfica do rio Pelotas causa a elevação artificial do nível e do lençol freático podendo afetar a vegetação ripária situada acima do novo nível dos rios. Portanto são esperadas diferenças estruturais entre florestas de encosta que margeiam reservatórios hidrelétricos e áreas controle. Este estudo foi desenvolvido em florestas de encosta de três tributários do rio Pelotas, em Campo Belo do Sul, SC. Foram instaladas 90 unidades amostrais (0,9 ha) em encostas que margeiam o reservatório da UHE Barra Grande e em encostas controle. Foram amostradas todas as árvores e arbustos vivos com DAP ≥ 5 cm. O desenho amostral permitiu comparar a heterogeneidade topográfica, a estrutura florestal e a composição de espécies (separadamente) entre rios, e em cada um deles o tratamento efeito da barragem através de análises de variância uni e multivariadas. Também foi utilizada uma análise de espécies indicadoras para determinar as espécies mais afins a cada encosta. A riqueza de espécies foi comparada por meio de curvas de rarefação baseadas na amostra. Neste trabalho foi utilizado o conceito de número efetivo de espécies (diversidade verdadeira) para calcular a diversidade de árvores. Foram amostradas 1233 árvores de 87 espécies e 40 famílias. As análises estatísticas revelaram heterogeneidade topográfica entre as encostas, que se refletiu na estrutura florestal e na composição de espécies. Essas diferenças também foram observadas em cada um dos rios para o tratamento efeito da barragem. Riqueza e diversidade de espécies se mostraram relativamente homogêneas. Os resultados corroboram o papel da heterogeneidade ambiental na estruturação das comunidades. As diferenças estruturais e em composição de espécies observadas para o tratamento efeito da barragem sugerem efeitos sobre a vegetação. Por outro lado, múltiplos fatores podem ter relações causais com essas diferenças, e, portanto, são necessários estudos complementares. / Plant communities are affected by topography in different spatial scales, acting as an environmental filter to species distribution and abundance. This influence is prominent in montane ecosystems. In southern Brazil, steep slopes of the Pelotas river watershed has important montane forest remnants, despite the pressure exerted by anthropic historical logging, agriculture, forestry, and in recent decades, hydroelectric exploitation. The damming of rivers is one of the most prominent impacts on freshwater ecosystems, with impacts on the riparian vegetation. The hydroelectric reservoir construction in a montane river with narrow valleys like those of the Pelotas river watershed causes the artificial increase of river water level and the groundwater affecting the riparian vegetation located above the new level of rivers. So, are expected structural differences between slope forest bordering Barra Grande hydroelectric reservoir and control areas. This study was carried out in slope forests of the three tributaries of Pelotas river in Campo Belo do Sul, SC. Were installed 90 sample plots (0.9 ha) on slope forests bordering the reservoir and control areas. We sampled all trees and shrubs alive with DBH ≥ 5 cm. The sample design allowed us to compare topography, forest structure and species composition (separately) between rivers, and the effect of the dam treatment through univariate and multivariate analysis of variance. It was also used an indicator species analysis to determine indicator species to each slope. Species richness was compared using rarefaction curves based on the sample. In this study we used the concept of effective number of species (true diversity) to calculate trees diversity. We sampled 1233 trees of 87 species and 40 families. Statistical analysis revealed topographic heterogeneity among the slopes, which was reflected in forest structure and species composition. These differences were also observed in each of the rivers for the effect of the dam treatment. Richness and true diversity proved relatively homogeneous. Our results support the role of environmental heterogeneity on forest communities. The forest structure and species composition differences observed for the effect of the dam treatment suggest effects on vegetation. On the other hand, multiple factors may have causal relationships with these differences, and therefore further studies are needed.

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