Peru is one of the richest peatland countries in the tropics. Its peatlands extend over all three of its regions, with a significant area in the Amazon. These peatlands provide key ecosystem services – storing immense amounts of carbon, uptaking carbon dioxide, nurturing unique biodiversity, regulating water at local and regional levels, and providing both livelihoods and cultural values for local people. The country’s peatlands have deteriorated through anthropogenic activities, including infrastructure construction and resource extraction (e.g. oil, minerals), and unsustainable uses or practices of varying intensity (e.g. overgrazing, peat extraction, palm felling, overhunting); such practices both threaten them and increase their vulnerability. Climate changes also compromise their stability. The Peruvian regulatory framework includes norms and instruments for the sustainable management of wetlands, but peatland-specific regulations are yet to be developed. Recent advances include the elaboration of a national definition for peatlands; however, peatlands are yet to be explicitly included in climate change strategies like REDD+ and NDCs. There is a critical lack of scientific research on Peruvian peatlands; they need to be mapped and inventoried, and their ecological properties and economic and social values characterized. If they are to be sustainably managed, it is also essential to identify and value the knowledges and practices of indigenous communities. The opportunities for the conservation and good management of these key ecosystems are many, including consolidation of mechanisms of payment for ecosystem services, implementation of sustainable resource management plans by the local population, expansion of protected natural areas, and recognition of communities’ tenure rights.

Key messagesIndonesia and Peru harbor some of the largest lowland tropical peatland areas. Indonesian peatlands are subject to much greater anthropogenic activity than Peru's resulting in high GHG and particulate emissions.We explored patterns of impact in both countries and compared predisposing factors. Impacts differ greatly among Indonesian regions and the Peruvian Amazon in the order: Sumatra > Kalimantan > Papua > Peru.All impacts, except fire, are positively related to population density.Current peatland integrity in Peru arises from a confluence of factors that has slowed development, with no absolute barriers protecting Peruvian peatlands from a similar fate to Indonesia's.If the goal is to maintain the integrity of Peruvian peatlands, government policies recognizing unique peatland functions and sensitivities will be necessary.

What is peat? Peat is a type of organic soil which is made up of partly decomposed vegetation and is formed over centuries in waterlogged conditions. Peat has been on our planet for around 360 million years. Some peatlands in existence today took more than 10,000 years to develop. Where is it found? Peat exists in a variety of climates around the world. From high altitudes to coastal areas and from tropical rainforests to permafrost regions towards the poles, where soil has been frozen year round for at least two years. The vast majority of peatlands can be found in colder climates, in temperate or boreal areas. Tropical countries with large stores of peat include the Democratic Republic of the Congo, Indonesia and Peru. 68% of tropical peatlands are found in Southeast Asia.

A thoroughly updated and accessible textbook featuring topical issues such as sea level rise, eutrophication, facilitation, restoration and conservation. This third edition is richly illustrated in colour, packed with examples from every major continent and wetland type, and features end-of-chapter questions to review and extend students' learning.

A transdisciplinary approach to investigating relationships between biomass burning and human health outcomes Environmental degradation is causing severe impacts on the various Earth ecosystems. Unsustainable development and anthropogenic pressure have altered the natural balance. From this perspective, sustainability has become a major issue to frame a greener and cleaner Earth for future generations. It can be argued that the worst example of unsustainable development is habitat degradation. Therefore, ecorestoration and other ecological practices are becoming increasingly important in our march toward sustainability. The present book covers all the aspects of ecorestoration and sustainability and how various areas intersect in this space. Environmental degradation is increasing all over the world at an unprecedented rate. This includes air, water, soil, and other natural resources resulting in the depletion of natural resources and an unsustainable planet. Therefore, it is incredibly important to restore the ecosystem’s health and services to maintain homeostasis. In this context, ecorestoration approaches in the form of eco-friendly technologies need to be formulated to promote the protection and conservation of various ecosystems. These approaches include freshwater bodies, soil and mined-out wasteland, degraded forest, biodiversity, and other degraded ecosystems. This important new volume from Wiley-Scrivener tackles these problems from a practical perspective, offering solutions and new methods for restoring our suffering global ecosystem. Edited by a team of experts, this collaboration of papers on these issues is a further step in our march toward sustainability. Whether for the engineer, scientist, or student, it is a must-have for any library.

Amazonian forests comprise almost 10% of stored carbon (C) in the world's land ecosystems. This C is held both in above-ground biomass (AGB) and in the soil. AGB in an individual plant depends on plant size, often measured in trees as height (H) and diameter (D), and the density of plant tissues, often approximated in trees by wood density (WD). Soil C storage depends on the balance between inputs from AGB due to mortality and senescence and outputs due to decay and erosion. Peatlands, wetlands recently described in northern Peruvian Amazonia, show unusually high rates of soil C accumulation. For these habitats information on C budget contributions from peatland plants is unavailable. In this study I estimated AGB in various peatlands of northern Peruvian Amazonia, and asked why some of these peatlands store more AGB than others. I first set out to estimate the relative contribution of inter- and intra-specific variation to variation in AGB among individual peatland trees. I found that 80% of the variation in AGB among individual trees was due to inter-specific variation. Then I assessed the extent to which the three traits that determine AGB (i.e., D, H and WD) contribute to inter- and intra-specific variation in AGB among peatland trees. I found variation in D and the interaction between D and H contributed most to inter- and intra-specific variation in AGB among trees. Last, I estimated the extent to which variation in AGB among peatland locations was due to variation in species composition, stem density and intra-specific variation in AGB. I found that species composition and intra-specific variation, but not stem density, explained nearly equal amounts of variation in AGB among peatland locations. In summary, detailed knowledge of tree size can provide good estimates of species level biomass estimates in the peatlands of northern Peruvian Amazonia. Additionally, what species are present, as well as how their biomass varies (intra-specifically) from site to site drives AGB variation among peatland locations.

The vast peat deposits in the Peruvian Amazon are crucial to the global climate. Palm swamp, the most extensive regional peatland ecosystem faces different threats, including deforestation and degradation due to felling of the dominant palm Mauritia flexuosa for fruit harvesting. While these activities convert this natural C sink into a source, the distribution of degradation and deforestation in this ecosystem and related C emissions remain unstudied. We used remote sensing data from Landsat, ALOS-PALSAR, and NASA's GEDI spaceborne LiDAR-derived products to map palm swamp degradation and deforestation within a 28 Mha area of the lowland Peruvian Amazon in 1990-2007 and 2007-2018. We combined this information with a regional peat map, C stock density data and peat emission factors to determine (1) peatland C stocks of peat-forming ecosystems (palm swamp, herbaceous swamp, pole forest), and (2) areas of palm swamp peatland degradation and deforestation and associated C emissions. In the 6.9 ± 0.1 Mha of predicted peat-forming ecosystems within the larger 28 Mha study area, 73% overlaid peat (5.1 ± 0.9 Mha) and stored 3.88 ± 0.12 Pg C. Degradation and deforestation in palm swamp peatlands totalled 535,423 ± 8,419 ha over 1990-2018, with a pronounced dominance for degradation (85%). The degradation rate increased 15% from 15,400 ha y-1 (1990-2007) to 17,650 ha y-1 (2007-2018) and the deforestation rate more than doubled from 1,900 ha y-1 to 4,200 ha y-1. Over 1990-2018, emissions from degradation amounted to 26.3 ± 3.5 Tg C and emissions from deforestation were 12.9± 0.5 Tg C. The 2007-2018 emission rate from both biomass and peat loss of 1.9 Tg C yr-1 is four times the average biomass loss rate due to gross deforestation in 2010-2019 reported for the hydromorphic Peruvian Amazon. The magnitude of emissions calls for the country to account for deforestation and degradation of peatlands in national reporting.