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Indomalayan realm

The Indomalayan realm, also known as the Oriental realm, is one of Earth's eight major biogeographic realms, encompassing a vast tropical region across South and Southeast that includes the , the Indochinese Peninsula, the , and parts of southern . Covering approximately 7.5 million square kilometers, it is defined by its distinct evolutionary history, shaped by the collision of the Indian and Eurasian plates, and features a mosaic of ecosystems from Himalayan foothills to island rainforests. This realm is divided into three primary subrealms: the , characterized by diverse habitats from deserts to wet evergreen forests; the Southeast Asian Forests, spanning subtropical broadleaf woodlands and montane regions across Indochina and the ; and the & Western subrealm, dominated by moist broadleaf forests, mangroves, and island archipelagos. These subrealms support extraordinary , including one-fifth of the world's plant, animal, and marine , with high levels of driven by isolation and climatic variation. The region includes three —, , and the —and four of the 36 global biodiversity hotspots, such as the , , , and the . Key flora consists of tropical and subtropical moist broadleaf forests, dipterocarp-dominated rainforests, and seasonal dry forests, while is highlighted by iconic species such as the (Panthera tigris tigris), (Elephas maximus), (Pongo spp.), (Hylobates spp.), wild cattle like (Bos gaurus) and (Bos javanicus), as well as pheasants, hornbills, and over 1,000 species, many endemic. Despite its ecological wealth, the Indomalayan realm confronts severe threats from , agricultural expansion, , and , which have led to habitat loss across much of its protected areas—now covering a significant portion of the region but requiring enhanced management for sustainability.

Geography and Extent

Boundaries and Location

The Indomalayan realm, also known as the Oriental realm, encompasses a vast tropical and subtropical region spanning much of South and , characterized by its distinct biogeographic boundaries that separate it from adjacent realms. It spans approximately from 35°N to 11°S in and from 60°E to 125°E in , covering diverse landforms from continental plateaus to archipelagos. The northern boundary of the Indomalayan realm is delineated by the southern edge of the , roughly along the Himalayan mountain range and the , extending eastward to the Yunnan-Guizhou Plateau in southern , where temperate Palearctic fauna transitions to tropical Indomalayan elements. To the west, the realm begins at the eastern borders of and , encompassing the up to the valley in eastern and , beyond which drier Palearctic influences dominate. The eastern limit follows Wallace's Line, a faunal boundary proposed by in 1863 that runs through the Indonesian archipelago—separating the Asian biota to the west from the to the east—specifically through the between and , the between and , and extending northwards, with the included on the Indomalayan side and the realm also encompassing lowland and the of . The southern extent includes the (Borneo, Sumatra, Java, and surrounding smaller islands) but excludes , the transitional zone of islands like Sulawesi and the Moluccas that bridge Indomalayan and Australasian faunas. This realm covers approximately 7.5 million square kilometers and includes parts of at least 12 countries, such as , , , , , , , , , southern , , and , with the often incorporated due to its biogeographic affinities with the Asian mainland. Key transitional zones refine these boundaries: Huxley's Line, a 1868 modification of Wallace's original by Thomas Huxley, shifts the division slightly eastward to include the group of islands in the Indomalayan realm, emphasizing stronger Asian floral and faunal links. Weber's Line, proposed in 1902, further adjusts the boundary between and , highlighting a steeper faunal divide in the deep-water channels of the region and better separating placental mammals from marsupials. These lines collectively underscore the realm's isolation by deep seas and mountain barriers, shaping its unique evolutionary trajectory. Adjacent to the realm are the marine waters of the Indo-West Pacific province, which exert significant influences on coastal and island ecosystems through currents and larval dispersal, though the realm itself is defined by terrestrial biogeography.

Physical Features and Climate

The Indomalayan realm features remarkable topographical diversity, ranging from the Himalayan mountain range in the north, which rises to elevations exceeding 8,000 meters and acts as a natural barrier against northern cold fronts, to the vast alluvial formed by sediment accumulation from Himalayan rivers. Further south, the dominates peninsular with its ancient basaltic landscapes and elevations averaging 600 meters, while the in represents a low-relief depositional plain shaped by fluvial processes. The realm's eastern and southern extents include the volcanic islands of the , characterized by active tectonics, rugged terrains, and chains like the , contributing to a mosaic of coastal and montane features. Major river systems play a pivotal role in shaping the realm's landscapes through sediment deposition and habitat formation. The and Brahmaputra rivers, originating in the , transport approximately 1 billion tons of annually, depositing it to build the and the expansive Ganges-Brahmaputra Delta, which spans over 100,000 square kilometers and fosters fertile floodplains essential for ecological stability. Similarly, River in delivers substantial Himalayan-derived sediments to its delta, creating nutrient-rich wetlands that support dynamic aquatic environments, while the Mekong River in Indochina carries around 160 million tons of sediment yearly, forming the Mekong Delta's intricate network of channels and supporting vast areas of productive riparian zones. Climatic conditions across the Indomalayan realm are predominantly tropical monsoon, classified under Köppen categories Af () and Am (tropical monsoon), with year-round high temperatures averaging 25–30°C and annual rainfall often exceeding 2,000 mm concentrated in wet seasons that drive seasonal flooding and soil replenishment. Northern regions transition to subtropical humid climates (Cwa), featuring hot summers and cooler, drier winters with mean temperatures dropping below 18°C in the coldest month, while effects in areas like the result in semi-arid conditions with rainfall under 1,000 mm annually. Seasonal patterns are governed by alternating southwest and northeast s, with the southwest from June to September delivering 70–90% of annual precipitation via moisture-laden winds from the , fostering lush vegetation growth. El Niño events disrupt this cycle by enhancing subsidence over the , often reducing rainfall by 10–20% and causing droughts in lowland areas, whereas montane microclimates exhibit cooler temperatures (decreasing 6.5°C per 1,000 m ) and more persistent compared to humid, flood-prone lowlands. As of 2025, climate variability in the Indomalayan realm has intensified due to , with regional temperatures rising at nearly twice the global average rate of 0.2°C per decade, leading to more frequent heatwaves exceeding 40°C in subtropical zones. Altered rainfall patterns include increased intensity, with extreme events up 20–30% in some areas, interspersed with prolonged dry spells that exacerbate in regions.

Historical Development

Biogeographic Classification

The biogeographic classification of the Indomalayan realm traces its origins to the foundational work of 19th-century naturalists who delineated global faunal regions based on observable discontinuities in animal distributions. Philip Lutley Sclater first proposed a system of six zoogeographic regions in 1858, including the "Indian Region" to encompass the of South and Southeast Asia, drawing primarily from avian distributions to identify natural boundaries shaped by geography and historical isolation. expanded and refined this framework in his seminal 1876 publication The Geographical Distribution of Animals, renaming Sclater's Indian Region as the "Oriental Region" and emphasizing faunal transitions, particularly the sharp biogeographic divide at Wallace's Line—a boundary between Asian and Australasian biotas marked by deep marine barriers that limited species dispersal. Wallace's analysis, grounded in extensive field observations from , established the Oriental Region as a distinct unit characterized by placental mammals, monkeys, and tropical forest avifauna, contrasting with the marsupial-dominated Australasian fauna to the east. The terminology evolved in the mid-20th century to reflect greater precision in delineating subcontinental faunal affinities, shifting from "Oriental" to "Indo-Malayan" or "Indomalayan" by the and through refinements by subsequent biogeographers. This change, influenced by Sclater's and Wallace's systems, aimed to highlight the realm's dual Indian and Malaysian components while accounting for transitional zones; for instance, J. Darlington's 1957 work on adopted similar boundaries but emphasized ecological gradients. A pivotal advancement came with Miklos D. F. Udvardy's 1975 classification, which formalized eight terrestrial biogeographic realms worldwide, designating "Indomalayan" as one and extending it from across to the , replacing outdated terms like "Oriental" to better align with evolutionary patterns. Udvardy's schema contrasted with earlier six-region models by incorporating oceanic and Antarctic realms, providing a more comprehensive global framework that integrated biotic provinces within each realm. In the 1980s, the Indomalayan realm gained prominence in conservation-oriented through its integration into systems like the classifications, which built on Udvardy's realms to map 825 terrestrial ecoregions by the early 2000s, emphasizing the Indomalayan's role in hotspots. This marked a departure from pre-1970s continent-based models, prioritizing faunal over political boundaries and facilitating targeted habitat protection across the realm's diverse provinces. Key debates in the late centered on boundary ambiguities, such as the inclusion of and Japan's southern islands (e.g., Ryukyu chain), often classified variably between Palearctic and Indomalayan due to mixed faunal elements, and Sulawesi's transitional status bridging Indomalayan and Australasian influences via . By the 2000s, consensus resolved these through analyses of amphibian, reptile, and mammalian distributions, affirming and the Ryukyus within the Indomalayan based on southern affinities, while retaining Sulawesi despite its hybrid biota. Into the 21st century, the Indomalayan classification has been refined within frameworks of the International Union for Conservation of Nature (IUCN) and , incorporating genetic and phylogenetic data to validate boundaries and assess evolutionary distinctiveness as of 2025. The IUCN's Phylogenetic Diversity , in its 2024-2025 report, highlights how molecular phylogenies confirm the realm's integrity while identifying hotspots of unique avian and reptilian lineages, aiding Red List assessments for over 45,000 globally. Similarly, 's BIRDBASE , updated in 2025, integrates biogeographic realms with 78 ecological traits across 11,589 bird species, using phylogenetic reconstructions to underscore the Indomalayan's role in global avian diversity patterns driven by climatic and tectonic histories. These updates emphasize quantitative phylogenetic metrics, such as evolutionary divergence times, to support conservation priorities without altering core boundaries established earlier.

Geological and Evolutionary History

The geological evolution of the Indomalayan realm was profoundly influenced by the collision of the with the , which commenced approximately 50 to 40 million years ago in the Eocene epoch. This convergence, driven by , crumpled the intervening sediments into vast fold-thrust belts, culminating in the uplift of the —a mountain chain spanning 2,900 kilometers with peaks exceeding 8,000 meters—and the subsequent elevation of the to an average height of 4,500 meters. The process involved no due to the buoyancy of continental crusts of comparable , instead resulting in crustal shortening and thickening to about 75 kilometers. These events created a massive orographic barrier that isolated southern faunal communities from northern Eurasian influences, fostering unique ary trajectories in the realm's tropical lowlands by redirecting patterns and altering moisture regimes. The realm's biota also reflects ancient vicariance stemming from the breakup of the supercontinent Gondwana during the Late Cretaceous, around 100 million years ago, when tectonic rifting separated key landmasses including proto-India. Molecular timetrees and dispersal-vicariance analyses of Gondwanan lineages, such as amphibians in the families Microhylidae and Natatanura, indicate congruent diversification events tied to plate separations, with early splits between Indo-Madagascar, Africa, Australia-New Guinea, and South America occurring in the Late Cretaceous (95% confidence intervals spanning 121–165 million years ago). These vicariance processes fragmented ancestral populations, promoting endemism in Indomalayan tetrapods as isolated fragments like the Indian subcontinent rafted northward, carrying relict Gondwanan taxa that later intermixed with Laurasian elements post-collision. Subsequent key climatic and sea-level fluctuations further shaped the realm's evolutionary landscape. During the (23–5 million years ago), global cooling episodes—flanking the Miocene Climatic Optimum—drove and intensification in , enhancing rainforest diversification by expanding seasonal habitats and facilitating adaptive radiations among flora and fauna. The Pleistocene ice ages (2.6 million to 11,700 years ago) exposed the through sea-level drops of up to 120 meters, forming extensive land bridges that connected the Indochinese mainland with islands like , , and , thereby enabling widespread faunal exchanges and gene flow across . This culminated in the Mid-Pleistocene Revolution around 1.2–0.6 million years ago, which amplified glacial-interglacial cycles and boosted dispersal of taxa such as amphibians and mammals. However, post-glacial sea-level rise, peaking around 6,000 years ago, inundated these bridges, re-isolating populations and reinforcing insular . Fossil records from the Siwalik Hills in northern and illuminate Miocene mammalian assemblages, spanning 10.7–5.7 million years ago and comprising over 115 species across ten orders, including , , and . These deposits, from the Nagri and Dhok Pathan formations, document turnover pulses at 10.3, 7.8, and 7.3–7.0 million years ago, coinciding with the spread of grasslands around 7.4 million years ago amid climatic drying, which shifted ecosystems from closed forests to more open habitats. Recent phylogenetic studies in the , leveraging genomic data, have affirmed the of core Indomalayan clades through analyses of mitochondrial and nuclear markers, underscoring the realm's cohesive evolutionary history despite its composite origins.

Biodiversity

Flora

The Indomalayan realm supports an exceptionally diverse , encompassing a wide array of adapted to its varied tropical and subtropical environments. Estimates indicate that the region, spanning South and , hosts tens of thousands of , contributing significantly to Asia's overall botanical richness of approximately 29,000 across 314 families. High levels of characterize this diversity, particularly in hotspots; for instance, alone accounts for about 30% endemic among its roughly 18,000 flowering . Tropical rainforests dominate much of the landscape, forming dense, multi-layered canopies that cover substantial portions of the realm's lowland areas and support intricate ecological interactions. Dominant plant families underscore the realm's botanical prominence, with standing out as a key group in Southeast Asian forests, featuring towering emergent trees such as species of that form the upper canopy in lowland habitats. Other influential families include and , which are prevalent in montane regions, alongside the Orchidaceae, renowned for its extraordinary exceeding 25,000 globally but with a substantial concentration in the humid tropics of the Indomalayan area, including slipper orchids like Paphiopedilum. Vegetation types vary markedly across elevations and climates, ranging from lowland dipterocarp forests in the to montane cloud forests in the , where rhododendrons thrive in misty highlands; coastal mangroves, such as those in the featuring Avicennia species, provide critical buffers against salinity; and seasonal deciduous forests prevail in monsoon-influenced zones. Unique adaptations enable plants to exploit the realm's environmental gradients, including abundant epiphytes and climbing vines that capitalize on the light-scarce understories of humid tropical forests, enhancing structural complexity. In areas affected by seasonal droughts, species like teak (Tectona grandis) exhibit resilience through deciduous habits and deep root systems suited to monsoon variability. Recent assessments highlight conservation concerns, with many plant species in the region facing endangerment primarily from habitat loss, underscoring the urgency of protecting this floral heritage amid ongoing environmental pressures.

Fauna

The Indomalayan realm hosts a remarkable diversity of , shaped by its tropical forests, montane habitats, and island archipelagos, supporting thousands of animal species adapted to varied ecological niches. This realm's animal life includes approximately 1,090 mammal species, more than 1,800 bird species, over 1,000 reptile species, and nearly 1,000 amphibian species, many of which play critical roles in , , and within their ecosystems. Mammal diversity in the realm includes approximately 1,090 species, encompassing a range of and smaller endemics that occupy diverse roles from apex predators to frugivores. Key examples include the Bengal tiger (Panthera tigris tigris), a keystone predator in grasslands and forests that regulates populations; the Asian elephant (Elephas maximus), an facilitating forest regeneration through its foraging; and the critically endangered Sumatran rhinoceros (Dicerorhinus sumatrensis), a browser confined to dense rainforests. are particularly prominent, with species like the orangutans (Pongo spp.), arboreal frugivores vital for in Southeast Asian dipterocarp forests, and the (Nasalis larvatus), a specialized in ecosystems. Avian richness includes approximately 1,800 species, representing about 18% of global landbird diversity, with many endemics contributing to pollination and insect control in tropical canopies. Characteristic groups include the hornbills (family Bucerotidae), large frugivores such as the (Buceros bicornis) that disperse seeds across forest gaps, and pheasants (family ), ground-dwelling omnivores like the (Lophophorus impejanus) adapted to alpine meadows. The realm serves as a major , with migratory patterns across the involving over 200 species, including waterfowl and raptors that link Palearctic breeding grounds to Indomalayan wintering sites. Reptiles number over 1,000 , while amphibians total 999 native , with high concentrations in humid forests where they function as bioindicators of environmental health. Notable reptiles include the king cobra (Ophiophagus hannah), the world's longest and a top predator in lowland forests that controls populations. Amphibian diversity is dominated by anurans, with over 500 in wet forest habitats, exemplified by the Bornean rainbow toad (Ansonia latidiscula), whose vivid coloration and toxic skin secretions deter predators and highlight adaptations. Invertebrate fauna is equally prolific, with butterflies exceeding 1,300 in alone, serving as pollinators and prey in food webs. Prominent examples include birdwing butterflies (tribe Troidini), such as the Rajah Brooke's birdwing (Trogonoptera brookii), large nectar-feeders endemic to Southeast Asian rainforests, and jewel beetles (family ), iridescent herbivores that bore into wood and aid nutrient cycling. The evolutionary history of Indomalayan reflects ancient n origins for certain groups, such as cyprinid fishes, whose lineages trace back to vicariance events following the breakup of around 90 million years ago, with subsequent radiations in freshwater systems. Recent genetic studies as of 2025 indicate an overall rate of approximately 25% across faunal groups, underscoring the realm's role in preserving ancient biodiversities amid ongoing . As of 2025, ongoing surveys continue to reveal new endemic , with genetic studies refining estimates.

Ecological Regions

Indian Subcontinent

The , encompassing India, Pakistan, , , , , and portions of , forms a core subrealm of the Indomalayan realm characterized by extreme ecological diversity spanning arid deserts to montane highlands. This region features the in the northwest, with its sparse xerophytic vegetation adapted to low rainfall, contrasting sharply with the lush, monsoon-influenced along the southwest coast. These varied landscapes support a mosaic of habitats, including tropical dry deciduous forests dominated by sal trees (Shorea robusta), which thrive in areas receiving 1,000–1,500 mm of annual rainfall and play a key role in nutrient cycling and wildlife corridors. Wetlands such as , Asia's largest brackish lagoon, serve as critical foraging grounds for migratory birds and like the Irrawaddy dolphin (Orcaella brevirostris), hosting over 150,000 waterfowl during peak seasons. In the northeast, montane ecosystems of the exhibit , from subtropical broadleaf forests at lower elevations to alpine meadows above 3,000 meters, fostering high through steep environmental gradients. Biodiversity in the Indian subcontinent is exceptionally rich, with the Western Ghats alone harboring 4,000–5,000 plant species, many of which exhibit high endemism due to the region's isolation and climatic stability over millennia. Notable mammals include the Indian leopard (Panthera pardus fusca), a versatile predator distributed across forests and grasslands from the Himalayas to the southern peninsula, and the sloth bear (Melursus ursinus), which relies on termites and fruits in dry deciduous habitats. Among birds, the Indian peafowl (Pavo cristatus) symbolizes the realm's avian diversity, inhabiting open woodlands and agricultural edges while facing localized threats from habitat fragmentation. These species underscore the subcontinent's role as a refuge for Indomalayan endemics, with over 500 bird species recorded in key ecoregions. Human activities have profoundly shaped the subcontinent's landscapes, particularly through , which has converted vast expanses—once supporting migratory herbivores—into croplands, reducing native grass cover by up to 50% in some areas and altering fire regimes essential for maintenance. Conversely, traditional practices like sacred groves, small forest patches protected for religious reasons, have preserved hotspots; alone hosts over 100,000–150,000 such sites, safeguarding rare plants and serving as gene banks amid surrounding deforestation. Recent conservation efforts highlight progress, as evidenced by 2025 WWF assessments showing (Panthera tigris) populations in recovering to over 3,600 individuals—more than double the 2006 estimate—largely due to , launched in 1973, which has expanded protected reserves and enhanced anti-poaching measures across 53 tiger habitats.

Indochina

Indochina, encompassing , , , , southern , and eastern , forms a critical portion of the Southeast Asian Forests subrealm within the Indomalayan realm, characterized by dramatic mountain systems such as the and expansive floodplains along major river systems. These features create a of isolated habitats that foster high , with the serving as a barrier to species dispersal and a refuge for ancient lineages shaped by tectonic uplift and climatic shifts. The region's transitions from rugged peaks exceeding 2,000 meters in to low-lying alluvial plains, supporting a gradient of ecosystems influenced by the monsoon climate. Key habitats in Indochina include dense evergreen rainforests in the Cardamom Mountains, where annual rainfall surpasses 2,000 mm, sustaining multilayered canopies dominated by dipterocarp trees and understories rich in ferns and orchids. In contrast, the Khorat Plateau hosts seasonal dry forests adapted to prolonged droughts, featuring deciduous species like teak (Tectona grandis) and bamboo thickets that regenerate during brief wet periods. Further south, the Mekong Delta's peat swamps represent unique wetland formations, with acidic, waterlogged soils supporting mangroves, palms, and floating aquatic vegetation that buffer against salinity intrusion. These habitats collectively cover over 1 million square kilometers, though fragmentation from agriculture has reduced contiguous forest blocks by approximately 20% since the 1990s. Biodiversity in Indochina is exemplified by flagship endemics such as the (Pseudoryx nghetinhensis), a restricted to the Annamite forests of and , where populations are estimated at fewer than 100 individuals due to habitat loss and . The region also harbors diverse reptiles, including the (Tomistoma schlegelii), a slender-snouted crocodilian inhabiting peat swamps and slow-moving rivers in , , and . Avian endemics like (Lophura edwardsi), confined to central 's seasonal tropical forests, highlight the area's ornithological richness, with this species classified as owing to and hunting pressures. Overall, Indochina supports over 1,000 vertebrate species, many adapted to the interface between terrestrial and aquatic environments. Seasonal dynamics are profoundly shaped by the River's annual flooding, which from to inundates up to 70% of the and habitats, creating dynamic aquatic-terrestrial interfaces that recharge , deposit nutrient-rich sediments, and trigger mass migrations of and amphibians. This flood pulse supports by connecting isolated wetlands, enabling nutrient cycling that sustains over 1,000 species and enhances forest productivity in adjacent areas. However, upstream dam construction has altered these patterns, reducing flood volumes by up to 30% in recent decades and disrupting ecological . Recent assessments of the Annamite , updated through 2025, underscore ongoing discoveries amid escalating threats, with over 20 new species documented since 2020, including cryptic frogs in caves and streamside . These findings, part of broader Greater surveys, reveal the ecoregion's role as a global for evolutionary novelty, though habitat conversion rates exceeding 1% annually imperil undescribed taxa. efforts emphasize protected areas like the Annamite Chain Landscape, which safeguard these emerging treasures.

Sunda Shelf

The , underlying the , , , , and surrounding islands, constitutes the core of the Malaysia & Western Indonesia subrealm, with ecosystems shaped by Pleistocene land bridges that facilitated faunal exchanges and subsequent isolation. This geologically stable platform supports ancient tropical rainforests, peatlands, and volcanic highlands across approximately 1.9 million square kilometers of land. Key habitats include vast lowland evergreen forests dominated by dipterocarps such as and species, forming canopies up to 50 meters tall in areas like Borneo’s Heart of Borneo; extensive peat swamp forests in Sumatra and Kalimantan, which cover over 20 million hectares and harbor specialized adapted to waterlogged, nutrient-poor soils; and montane cloud forests on peaks like , featuring rhododendrons and orchids above 1,500 meters. Coastal mangroves and freshwater swamps along rivers like the Rajang provide essential breeding grounds for aquatic species. Biodiversity on the is unparalleled, with over 25,000 species (45% endemic), 700 species including endemics like the (Neofelis diardi) and (Tapirus indicus), and more than 2,500 fish species in associated freshwater systems. Flagship animals include the (Pongo pygmaeus), (Nasalis larvatus), and (Dicerorhinus sumatrensis), alongside diverse avifauna such as the (Buceros bicornis) and over 600 bird species overall. The region's isolation has driven high speciation rates, particularly in invertebrates and reptiles. Human pressures, including commercial , palm oil plantations, and peatland drainage, have resulted in approximately 50% loss of primary forests since the , exacerbating fires and carbon emissions. As of 2025, rates remain high at over 1 million hectares annually in alone, threatening endemic with . Conservation initiatives like the network and the Heart of Borneo agreement protect about 15% of the area, focusing on transboundary corridors and sustainable land use to mitigate ongoing .

Philippines

The Philippine archipelago, comprising over 7,641 islands situated east of the and isolated by deep oceanic waters, exhibits volcanic origins that have fostered exceptional levels of through prolonged geographic isolation. This isolation, a consequence of tectonic activity and never-complete land connections to mainland except for limited cases like , has driven evolutionary divergence, resulting in unique assemblages of and adapted to insular conditions. Key habitats in the Philippines include montane rainforests, particularly on where elevations above 1,000 meters support diverse cloud-shrouded forests along the range, harboring specialized epiphytes and understory plants. Ultramafic soils, derived from formations on islands like and , sustain unique flora such as metal-tolerant trees and shrubs in the family , which thrive in nutrient-poor, serpentine environments. Coastal mangroves, fringing much of the archipelago's 36,000 kilometers of shoreline, provide critical nurseries for marine life and buffer against storms, with species like dominating these tidal ecosystems. Biodiversity in the Philippines is marked by high , with over 100 of the 165 native unique to the , including 52 non-volant endemic to alone. Iconic examples include the (Pithecophaga jefferyi), a raptor restricted to remnant forests on , , , and , and the ( mindorensis), a dwarfed wild buffalo surviving only on Island. The boasts over 1,500 orchid , many endemic like the Vanda sanderiana (), alongside carnivorous pitcher plants () with at least 50 endemic taxa adapted to nutrient-scarce peat swamps and ultramafic ridges. Island biogeographic effects are pronounced across the , with smaller exhibiting dwarfed faunas due to resource limitations and the "island rule," where large mammals evolve reduced body sizes, as seen in records of extinct dwarf elephants and modern insular bovids like the . Habitat fragmentation from volcanic activity and sea-level changes has amplified , contributing to approximately 35% bird among over 530 , many confined to single or island groups. Recent assessments by the Department of Environment and Natural Resources (DENR) in 2025 highlight over 700 across taxa, underscoring vulnerabilities exacerbated by habitat loss, with new protected areas established following devastating 2020 typhoons like Rolly and to enhance in key biodiversity zones. These efforts include expanded marine protected areas and initiatives targeting montane and habitats to mitigate ongoing isolation-driven risks.

Conservation and Threats

Endemism and Biodiversity Hotspots

The Indomalayan realm exhibits notable levels of , with approximately 20-30% of its unique to the region, driven by geographic isolation such as island archipelagos and mountain barriers that promote . Endemism rates are particularly elevated in insular and montane areas, reaching over 50% for terrestrial vertebrates in the , where more than half of the 1,238 known are found nowhere else. Similarly, in the , about 40% of the roughly 4,000 flowering plant are endemic, reflecting the region's role as a refugium for ancient lineages. Within the Indomalayan realm, several areas qualify as biodiversity hotspots under criteria established by , requiring at least 1,500 endemic and more than 70% loss of original . Key examples include the hotspot, spanning with over 7,000 endemic plants; Sundaland, encompassing and with exceptional faunal diversity; the Mountains of Southwest , harboring unique alpine flora; and the hotspot, noted for its archipelagic isolation fostering high vertebrate . These hotspots collectively support more than 10,000 endemic plant across the realm. Flagship species exemplify the realm's endemism, such as ( nigropalmatus), an iconic gliding restricted to the rainforests of within the , where it demonstrates adaptations like webbed feet for arboreal gliding that highlight genetic uniqueness from prolonged isolation. Globally, Indomalayan hotspots are disproportionately significant, containing approximately 20% of the world's plant species despite occupying only 3% of Earth's land surface, underscoring their critical role in planetary . Evolutionary drivers of this endemism trace to Pleistocene ice ages, when refugia in humid lowlands and highlands of the Indomalayan realm preserved diverse lineages through climatic oscillations, enabling divergence and survival of isolated populations.

Human Impacts and Current Challenges

The Indomalayan realm faces profound pressures, primarily from driven by commercial , , and production. Since 1990, tropical forests in , encompassing much of the realm, have experienced substantial losses, with rates peaking at 4.6 million hectares per year in the 1990s before slowing; the FAO's Global Forest Resources Assessment 2025 reports ongoing annual of around 10.9 million hectares globally, with Southeast Asia contributing significantly due to these activities. Poaching exacerbates threats to , particularly through the illegal rhino horn trade, which fuels networks across and beyond, endangering the already critically low populations of Sumatran and Javan rhinos. Climate change compounds these issues, with projected warming of approximately 2°C by 2050 under moderate emissions scenarios intensifying risks across the realm. , expected to accelerate, threatens ecosystems vital for coastal , potentially submerging large areas and disrupting reliant on these habitats. Altered patterns, driven by rising temperatures and atmospheric moisture, are forecasted to impact and wildlife, with studies indicating shifts that could affect diversity and broader floral evolution in monsoon-dependent regions. The realm's human population, exceeding 2.5 billion people and concentrated in densely populated areas like the (covering about 40% of the realm's land with high densities), drives and the introduction of . This fragmentation isolates wildlife populations, reduces , and facilitates invasives like alligator weed, which spread via human activities and outcompete native . Conservation efforts offer some countermeasures, including the ASEAN Biodiversity Plan 2024–2030, which aims to halt and reverse biodiversity loss through regional cooperation on protected areas and sustainable use. India maintains over 1,000 protected areas, including 107 national parks, safeguarding key habitats. Rewilding initiatives, such as the Sumatran rhino breeding program at Way Kambas National Park, have seen success with a fifth calf born in 2025, bolstering the captive population to 10 individuals. Despite these advances, gaps persist: India's tiger population has rebounded to an estimated 3,682 individuals by 2022, contributing to a global total of about 5,574 as of 2023, yet numbers continue to decline sharply, with Bornean populations having dropped by over 80% from 1950 levels by 2025 due to habitat loss. Community-based approaches, integrating local involvement in and , show promise in addressing these imbalances but require expanded funding and enforcement to bridge ongoing threats.

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