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Measurements of net primary productivity (NPP) and litter decomposition from tropical peatlands are severely lacking, limiting our ability to parameterise and validate models of tropical peatland development and thereby make robust predictions of how these systems will respond to future environmental and climatic change. Here, we present total NPP (i.e., above- and below-ground) and decomposition data from two floristically and structurally distinct forested peatland sites within the Pastaza Marañón Foreland Basin, northern Peru, the largest tropical peatland area in Amazonia: (1) a palm (largely Mauritia flexuosa) dominated swamp forest and (2) a hardwood dominated swamp forest (known as 'pole forest', due to the abundance of thin-stemmed trees). Total NPP in the palm forest and hardwood-dominated forest (9.83 ± 1.43 and 7.34 ± 0.84 Mg C ha-1 year-1, respectively) was low compared with values reported for terra firme forest in the region (14.21-15.01 Mg C ha-1 year-1) and for tropical peatlands elsewhere (11.06 and 13.20 Mg C ha-1 year-1). Despite the similar total NPP of the two forest types, there were considerable differences in the distribution of NPP. Fine root NPP was seven times higher in the palm forest (4.56 ± 1.05 Mg C ha-1 year-1) than in the hardwood forest (0.61 ± 0.22 Mg C ha-1 year-1). Above-ground palm NPP, a frequently overlooked component, made large contributions to total NPP in the palm-dominated forest, accounting for 41% (14% in the hardwood-dominated forest). Conversely, Mauritia flexuosa litter decomposition rates were the same in both plots: highest for leaf material, followed by root and then stem material (21%, 77% and 86% of mass remaining after 1 year respectively for both plots). Our results suggest potential differences in these two peatland types' responses to climate and other environmental changes and will assist in future modelling studies of these systems.

Mediciones de la productividad primaria neta (PPN) y la descomposición de materia orgánica de las turberas tropicales son escasas, lo que limita nuestra capacidad para parametrizar y validar modelos de desarrollo de las turberas tropicales y, en consecuencia, realizar predicciones sólidas sobre la respuesta de estos sistemas ante futuros cambios ambientales y climáticos. En este estudio, presentamos datos de PPN total (es decir, biomasa aérea y subterránea) y descomposición de la materia orgánica colectada en dos turberas boscosas con características florísticas y estructurales contrastantes dentro de la cuenca Pastaza Marañón al norte del Perú, el área de turberas tropicales más grande de la Amazonia: (1) un bosque pantanoso dominado por palmeras (principalmente Mauritia flexuosa) y (2) un bosque pantanosos dominado por árboles leñosos de tallo delgado (conocido como 'varillal hidromórfico'). La PPN total en el bosque de palmeras y el varillal hidromórfico (9,83 ± 1,43 y 7,34 ± 0,84 Mg C ha­1 año­1 respectivamente) fue baja en comparación con los valores reportados para los bosques de tierra firme en la región (14,21­15,01 Mg C ha­1 año­1) y para turberas tropicales en otros lugares (11,06 y 13,20 Mg C ha­1 año­1). A pesar de que la PPN total fue similar en ambos tipos de bosque, hubo diferencias considerables en la distribución de la PPN. La PPN de las raíces finas fue siete veces mayor en el bosque de palmeras (4,56 ± 1,05 Mg C ha­1 año­1) que en el varillal hidromórfico (0,61 ± 0,22 Mg C ha­1 año­1). La PPN de la biomasa aérea de las palmeras, un componente ignorado frecuentemente, contribuyó en gran medida a la PPN total del bosque de palmeras, representando el 41% (14% en el varillal hidromórfico). Por el contrario, la tasa de descomposición de materia orgánica de Mauritia flexuosa fue la misma en ambos sitios: la más alta corresponde a la hojarasca, seguida por las raíces y luego el tallo (21%, 77% y 86% de la masa restante después de un año, respectivamente para ambos sitios). Nuestros resultados sugieren diferencias potenciales en la respuesta de estos dos tipos de turberas al clima y otros cambios ambientales, y ayudarán en futuros estudios de modelamiento de estos sistemas.

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Resumen: El crecimiento diamétrico arbóreo (CDA) es un componente fundamental de la productividad primaria neta (PPN) y del almacenamiento de carbono en ecosistemas boscosos, por lo cual cumple un papel importante en la mitigación del cambio climático global. Se ha planteado la hipótesis de que en los bosques lluviosos tropicales de baja altitud el CDA está limitado por la disponibilidad edáfica de nutrientes; sin embargo, pocas evidencias experimentales la apoyan, especialmente en bosques con alta precipitación (>5 000 mm anuales). Este estudio evalúa los efectos de la fertilización del suelo sobre el CDA en bosques pluviales tropicales del Pacífico Colombiano, una de las zonas más lluviosas del mundo. Tales efectos se evaluaron a nivel de localidades, categorías diamétricas, densidad de madera y grupos funcionales. Para ello, se realizaron dos inventarios arbóreos (2014 y 2015), se aplicaron cinco tratamientos de fertilización (nitrógeno-N, fósforo-P, potasio-K, NPK y Control) y se determinó el CDA en cinco parcelas permanentes de una hectárea. Se encontró que la aplicación de N y NPK tuvo poco efecto sobre el CDA con respecto al control, mientras que la adición de P y K produjo reducción significativa en la tasa de crecimiento relativo arbórea con respecto al control a nivel de las localidades, en árboles pequeños y medianos, en todas las densidades de madera (baja, media y alta) y en el grupo de plantas dicotiledóneas. Aunque los resultados no corroboraron la hipótesis de limitación de nutrientes sobre el CDA en los bosques estudiados, se evidenció que durante los primeros años de fertilización (principalmente con P y K) ocurrieron cambios en los patrones de PPN aérea y subterránea, probablemente para maximizar la fotosíntesis y la adquisición de nutrientes del suelo.

Abstract: The tree diameter growth (CDA) is a fundamental component of net primary productivity (NPP) and carbon storage in forest ecosystems; therefore, it plays a key role in mitigating global climate change. It has been hypothesized that CDA in lowland tropical rain forests is limited by the availability of soil nutrients, yet little experimental evidence is available, especially in forest of high precipitation (>5 000 mm per year). This study evaluated the effects of soil fertilization on CDA in tropical rainforests of the Colombian Pacific, one of the wettest areas of the world. Such effects were assessed at the level of localities, diametric categories, wood density, and functional groups. To do this, two arboreal inventories (2014 and 2015) were performed, five fertilization treatments (Nitrogen-N, Phosphorus-P, Potassium-K, NPK and Control) were applied, and the CDA was determined in five permanent plots of one hectare. We found that the application of N and NPK had little effect on CDA as compared to the control; while the addition of P and K produced significant reduction of the trees relative growth rate, with respect to the control at the level of localities, in small and medium sized trees, in all wood densities (low, medium and high), and in the group of dicotyledonous species. Although these results did not corroborate the hypothesis of nutrient limitation on CDA in the studied forests, it was found that during the early years of fertilization (mainly with P and K), different patterns of aboveground and belowground NPP occurred to maximize photosynthesis and soil nutrient acquisition. Rev. Biol. Trop. 65 (3): 1161-1173. Epub 2017 September 01.

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Resumen:Las raíces finas juegan un papel importante en la adquisición de agua y minerales del suelo, el balance global del carbono y la mitigación del cambio climático. La dinámica (productividad-PRF y recambio-RRF) de raíces finas es esencial para el ciclo de nutrientes y balance de carbono de los ecosistemas forestales. La disponibilidad de agua y nutrientes determina de manera significativa la PRF y el RRF. Se ha planteado la hipótesis de que la dinámica de raíces finas aumenta con la disponibilidad de los recursos del suelo en bosques tropicales. Para probar esta hipótesis en las selvas tropicales del Chocó (ecosistemas con las más altas tasas de precipitación en el mundo), se establecieron cinco parcelas permanentes de una hectárea en las localidades de Opogodó y Pacurita, donde la PRF y RRF se midieron a 0-10 cm y 10-20 cm de profundidad. La medición de la PRF se realizó por el método de cilindros de crecimiento. La tasa de RRF se midió como la PRF/ biomasa media anual. Además, se midieron los parámetros de fertilidad del suelo (pH, nutrientes y textura) y se evaluó su asociación con PRF y RRF. Se encontró que ambos sitios presentan suelos pobres en nutrientes. Las localidades difieren en características edáficas; Opogodó tiene suelos arenosos y topografía plana, y Pacurita tiene suelos arcillosos, ricos en aluminio y topografía montañosa. En Opogodó la PRF fue (media ± DE) de 6.50 ± 2.62 t/ha.año. En Pacurita la PRF fue 3.61 ± 0.88 t/ha.año. Igualmente, en Opogodó el RRF fue mayor que en Pacurita (1.17 /año y 0.62 /año, respectivamente). El RRF y la PRF fueron mayores en la superficie del suelo (10 cm de profundidad). La PRF y el RRF mostraron correlación positiva con el pH, MO, N total, K, Mg, y arena; mientras que, las correlaciones fueron negativas con la CICE, Al, limo y arcilla. El porcentaje de arena fue el parámetro que mejor explica la variación en la PRF. La tasa negativa de la RRF fue explicada por la disponibilidad de Al. Los resultados evidenciaron un aumento en la dinámica de las raíces finas con la fertilidad del suelo a escala local, lo que sugiere que en selvas tropicales con suelos oligotróficos, las raíces finas tienden a proliferar rápidamente en pequeños parches de suelo ricos en arena y nutrientes.

Abstract:The fine roots play an important role in the acquisition of water and minerals from the soil, the global carbon balance and mitigation of climate change. The dynamics (productivity and turnover) of fine roots is essential for nutrient cycling and carbon balance of forest ecosystems. The availability of soil water and nutrients has significantly determined the productivity and turnover of fine roots. It has been hypothesized that fine roots dynamics increases with the availability of soil resources in tropical forest ecosystems. To test this hypothesis in tropical rainforests of Chocó (ecosystems with the highest rainfall in the world), five one-ha permanent plots were established in the localities of Opogodó and Pacurita, where the productivity and turnover of fine roots were measured at 0-10 cm and 10-20 cm depth. The measurement of the fine root production was realized by the Ingrowth core method. The fine root turnover was measured like fine roots production divided mean annual biomass. In addition, soil fertility parameters (pH, nutrients, and texture) were measured and their association with productivity and turnover of fine roots was evaluated. It was found that the sites had nutrient-poor soils. The localities also differ in soil; Opogodó has sandy soils and flat topography, and Pacurita has clay soils, rich in aluminum and mountainous topography. In Opogodó fine root production was 6.50 ± 2.62 t/ha.yr (mean ± SD). In Pacurita, fine root production was 3.61 ± 0.88 t/ha.yr. Also in Opogodó, the fine root turnover was higher than in Pacurita (1.17 /y and 0.62 /y, respectively). Fine root turnover and production in the upper soil layers (10 cm upper soil) was considerably higher. Productivity and turnover of fine roots showed positive correlation with pH and contents of organic matter, total N, K, Mg, and sand; whereas correlations were negative with ECEC and contents of Al, silt, and clay. The percentage of sand was the parameter that best explained the variations of fine root production. The fine root turnover was negatively explained by soil Al availability. Results suggested the increase of fine root dynamics with soil fertility at a local scale, which also indicates that under the oligotrophic conditions of soils in tropical rainforests, fine roots tend to proliferate rapidly in small patches of soil rich in sand and nutrients. Rev. Biol. Trop. 64 (4): 1709-1719. Epub 2016 December 01.

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Understanding the relationship between photosynthesis, net primary productivity and growth in forest ecosystems is key to understanding how these ecosystems will respond to global anthropogenic change, yet the linkages among these components are rarely explored in detail. We provide the first comprehensive description of the productivity, respiration and carbon allocation of contrasting lowland Amazonian forests spanning gradients in seasonal water deficit and soil fertility. Using the largest data set assembled to date, ten sites in three countries all studied with a standardized methodology, we find that (i) gross primary productivity (GPP) has a simple relationship with seasonal water deficit, but that (ii) site-to-site variations in GPP have little power in explaining site-to-site spatial variations in net primary productivity (NPP) or growth because of concomitant changes in carbon use efficiency (CUE), and conversely, the woody growth rate of a tropical forest is a very poor proxy for its productivity. Moreover, (iii) spatial patterns of biomass are much more driven by patterns of residence times (i.e. tree mortality rates) than by spatial variation in productivity or tree growth. Current theory and models of tropical forest carbon cycling under projected scenarios of global atmospheric change can benefit from advancing beyond a focus on GPP. By improving our understanding of poorly understood processes such as CUE, NPP allocation and biomass turnover times, we can provide more complete and mechanistic approaches to linking climate and tropical forest carbon cycling.

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The functional role of herbivores in tropical rainforests remains poorly understood. We quantified the magnitude of, and underlying controls on, carbon, nitrogen and phosphorus cycled by invertebrate herbivory along a 2800 m elevational gradient in the tropical Andes spanning 12°C mean annual temperature. We find, firstly, that leaf area loss is greater at warmer sites with lower foliar phosphorus, and secondly, that the estimated herbivore-mediated flux of foliar nitrogen and phosphorus from plants to soil via leaf area loss is similar to, or greater than, other major sources of these nutrients in tropical forests. Finally, we estimate that herbivores consume a significant portion of plant carbon, potentially causing major shifts in the pattern of plant and soil carbon cycling. We conclude that future shifts in herbivore abundance and activity as a result of environmental change could have major impacts on soil fertility and ecosystem carbon sequestration in tropical forests.

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Macrophyte net primary productivity (NPP) is a significant but understudied component of the carbon budget in large Amazonian floodplains. Annual NPP is determined by the interaction between stem elongation (vertical growth) and plant cover changes (horizontal expansion), each affected differently by flood duration and amplitude. Therefore, hydrological changes as predicted for the Amazon basin could result in significant changes in annual macrophyte NPP. This study investigates the responses of macrophyte horizontal expansion and vertical growth to flooding variability, and its possible effects on the contribution of macrophytes to the carbon budget of Amazonian floodplains. Monthly macrophyte cover was estimated using satellite imagery for the 2003-2004 and 2004-2005 hydrological years, and biomass was measured in situ between 2003 and 2004. Regression models between macrophyte variables and river-stage data were used to build a semiempirical model of macrophyte NPP as a function of water level. Historical river-stage records (1970-2011) were used to simulate variations in NPP, as a function of annual flooding. Vertical growth varied by a factor of ca. 2 over the simulated years, whereas minimum and maximum annual cover varied by ca. 3.5 and 1.5, respectively. Results suggest that these processes act in opposite directions to determine macrophyte NPP, with larger sensitivity to changes in vertical growth, and thus maximum flooding levels. Years with uncommonly large flooding amplitude resulted in the highest NPP values, as both horizontal expansion and vertical growth were enhanced under these conditions. Over the simulated period, annual NPP varied by ca. 1.5 (1.06-1.63 TgC yr(-1) ). A small increasing trend in flooding amplitude, and by extension NPP, was observed for the studied period. Variability in growth rates caused by local biotic and abiotic factors, and the lack of knowledge on macrophyte physiological responses to extreme hydrological conditions remain the major sources of uncertainty.

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Recently, the hypothesis that the geographic distribution of species could be influenced by the shape of the domain edges, the so-called Mid-Domain Effect (MDE), has been included as one of the five credible hypotheses for explaining spatial gradients in species richness, despite all the unsuccessful current attempts to prove empirically the validity of MDE. We used data on spatial worldwide distributions of Falconiformes to evaluate the validity of MDE assumptions, incorporated into two different sorts of null models at a global level and separately across five domains/landmasses. Species richness values predicted by the null models of the MDE and those values predicted by Net Primary Productivity, a surrogate variable expressing the effect of available energy, were compared in order to evaluate which hypothesis better predicts the observed values. Our tests showed that MDE continues to lack empirical support, regardless of its current acceptability, and so, does not deserve to be classified as one possible explanation of species richness gradients.

Recentemente, a hipótese de que a distribuição geográfica das espécies poderia ser influenciada pela forma das bordas continentais, conhecida como Efeito do Domínio Médio (EDM), foi incluída como uma das cinco hipóteses prováveis para explicar os gradientes espaciais de riqueza de espécies, apesar das últimas tentativas infrutíferas de prová-la empiricamente. Usamos os dados globais de distribuição espacial dos Falconiformes para avaliar os pressupostos do EDM, por meio de dois tipos de modelos nulos, em uma análise global e, também, separadamente por cinco domínios/continentes. Os valores de riqueza de espécies preditos pelos modelos nulos do EDM e pela produtividade primária líquida, uma variável substitutiva para expressar o efeito da energia disponível, foram comparados para avaliar qual hipótese prediz melhor os valores observados. Nossos testes mostraram que o EDM permanece sem suporte empírico, apesar da corrente notoriedade, não merecendo, portanto, ser classificado como uma das explicações possíveis para os gradientes de riqueza de espécies.