Seasonally dry tropical forests are distributed across Latin America and the Caribbean and are highly threatened, with less than 10% of their original extent remaining in many countries. Using 835 inventories covering 4660 species of woody plants, we show marked floristic turnover among inventories and regions, which may be higher than in other neotropical biomes, such as savanna. Such high floristic turnover indicates that numerous conservation areas across many countries will be needed to protect the full diversity of tropical dry forests. Our results provide a scientific framework within which national decision-makers can contextualize the floristic significance of their dry forest at a regional and continental scale. N eotropical seasonally dry forest (dry forest) is a biome with a wide and fragmented distribution, found from Mexico to Argentina and throughout the Caribbean (1, 2) ( Fig. 1). It is one of the most threatened tropical forests in the world (3), with less than 10% of its original extent remaining in many countries (4).Following other authors (5, 6), we define dry forest as having a closed canopy, distinguishing it from more open, grass-rich savanna. It occurs on fertile soils where the rainfall is less thañ 1800 mm per year, with a period of 3 to 6 months receiving less than 100 mm per month (5-7), during which the vegetation is mostly deciduous. Seasonally dry areas, especially in Peru and Mexico, were home to pre-Columbian civilizations, so human interaction with dry forest has a long history (8). The climates and fertile soils of dry forest regions have led to higher human population densities and an increasing demand for energy and land, enhancing degradation (9). More recently, destruction of dry forest has been accelerated by intensive cultivation of crops, such as sugar cane, rice and soy, or by conversion to pasture for cattle.Dry forest is in a critical state because so little of it is intact, and of the remnant areas, little is protected (3). For example, only 1.2% of the total Caatinga region of dry forest in Brazil is fully protected compared with 9.9% of the Brazilian Amazon (10). Conservation actions are urgently needed to protect dry forest's unique biodiversity-many plant species and even genera are restricted to it and reflect an evolutionary history confined to this biome (1).We evaluate the floristic relationships of the disjunct areas of neotropical dry forest and highlight those that contain the highest diversity and endemism of woody plant species. We also explore woody plant species turnover across geographic space among dry forests. Our results provide a framework to allow the conservation significance of each separate major region of dry forest to be assessed at a continental scale. Our analyses are based on a subset of a data set of 1602 inventories made in dry forest and related semi-deciduous forests from Mexico and the Caribbean to Argentina and Paraguay that covers 6958 woody species, which has been compiled by the Latin American and Caribbean Seasonally Dry Tropica...

No abstract

This is an open access article under the terms of the Creative Commons Attribution License, which permits use, distribution and reproduction in any medium, provided the original work is properly cited.

Los bosques primarios intactos de la Amazonía peruana se comportan como sumideros de carbono: un servicio ecosistémico clave a nivel mundial. Este sumidero fue cuantificado en 0.54 Mg C ha-1 año-1 (1990-2017) para los bosques amazónicos intactos de las Áreas Naturales Protegidas (ANPs) de Perú y las zonas de amortiguamiento. En otras palabras, la conservación de bosques intactos en ANPs ayudó a remover 9.6 millones de toneladas de carbono de la atmósfera por año, lo cual equivale aproximadamente al 85% de las emisiones de la quema de combustibles fósiles del país durante el 2012. Este servicio de remoción de CO2 atmosférico es necesario incluir en el inventario nacional de gases de efecto invernadero, y en los compromisos nacionales de reducción de emisiones, por dos razones. Primero, debido a ser un flujo importante, nos ayudaría a tener una aproximación más real del balance de carbono en Perú. Segundo, fortalecería la necesidad de mantener la integridad de estos bosques tanto por el servicio de almacenamiento de carbono (evitar emisiones) como el servicio de sumidero (remoción de emisiones) y la diversidad biológica que albergan. La provisión del servicio de sumidero solo se asegurará con una gestión efectiva y adaptativa de las ANPs. El reporte de este servicio ambiental a nivel nacional debe ser implementado a través del monitoreo a largo plazo de la dinámica del carbono y el impacto del cambio climático a través de la red de parcelas forestales permanentes de RAINFOR (Red Amazónica de Inventarios Forestales) y el proyecto MonANPeru. El establecimiento de este sistema de monitoreo permitirá el desarrollo de los mecanismos financieros para cerrar la brecha y lograr la sostenibilidad de la conservación de los bosques en las ANPs de Perú.

Attempts at historical reconstruction are based on limited data. We are more likely to produce accurate historical reconstructions by utilizing information from diverse sources and pooling data within the relevant research communities which will allow us to build up a moving picture of the geological, climatic, and biological evolution of our planet. We suggest that dated phylogenies of plants can contribute greatly to a better understanding of Earth history. Timing of phylogenetic splits of lowland restricted lineages on either side of the Andes could provide information on the timing of montane uplift and associated climatic changes. The timing of the arrival and diversification of organisms restricted to specific climatic regimes at a particular altitude can provide information on the age at which mountains reached a height adequate for that climate once corrected for global climate changes. As a model for study, we discuss how dated phylogenies in biome rich Colombia may contribute to an understanding of geological and climatic change in north‐western South America. Lowland wet forest restricted lineages separated from the mid‐Miocene, whereas lineages primarily restricted to mid‐altitude cloud forests began to diversify from the mid‐ to late‐Miocene and the majority of high‐altitude Páramo lineages began to diversify during the Pliocene. The age of diversification of altitudinally restricted lineages therefore gives an indication of the age at which particular altitudes may have been reached.