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Malesia
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Map 1: A very broad definition of Malesia includes both the World Geographical Scheme for Recording Plant Distributions's Malesia (green) and most of its Papuasia (orange).

Malesia is a biogeographical region straddling the Equator and the boundaries of the Indomalayan and Australasian realms. It is a phytogeographical floristic region in the Paleotropical kingdom. It was first recognized as a distinct region in 1857 by Heinrich Zollinger, a Swiss botanist and explorer.[1] The precise boundaries used to define Malesia vary. The broadly defined area used in Flora Malesiana consists of the countries of Malaysia, Singapore, Indonesia, Brunei, the Philippines, Timor-Leste and Papua New Guinea.[2] The original definition by the World Geographical Scheme for Recording Plant Distributions (WGSRPD) covered a similar area, but New Guinea and some offshore islands were split off as Papuasia in its 2001 version.

Floristic region

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Map 2 (based on Johns, 1995: fig. 2[3])

Definitions of Malesia:

Areas:

  • A = Western Malesia (Sundaland)
  • B = Central Malesia
  • C = Eastern Malesia (Sahul Shelf)
  • C+D = Papuasia

Malesia was first recognized as a distinct floristic region in 1857 by Heinrich Zollinger, a Swiss botanist and explorer. In 1948 and 1950, Cornelius G. G. J. van Steenis developed the idea of Malesia, and put forward plans for a Flora Malesiana.[3][4] Van Steenis defined the area of Malesia through the concept of 'demarcation knots': lines across which there are major changes in the genera present in the flora. There were three clear boundaries: between the Malay Peninsula (including part of southern Thailand) and mainland Asia (line 1 in map 2); between the Philippines and Taiwan (line 2 in map 2); and along the Torres Strait between New Guinea and Australia (line 3 in map 2).[1] The eastern boundary was less clear; van Steenis somewhat arbitrarily placed it between the Bismarck and Solomon Islands and the other Pacific islands (line 4 in map 2).[5] Van Steenis initially used Zollinger's name 'Malesia'. He later anglicized it to 'Malaysia', but when the country of Malaysia was formed in 1963, it was necessary to return to the original name.[5][6]

The first edition of the World Geographical Scheme for Recording Plant Distributions (WGSRPD) used the same definition, but in the second edition of 2001, New Guinea and the Bismarck Archipelago were removed from Malesia and united with the Solomon Islands, previously placed in the WGSRPD's Southwestern Pacific region, and placed into a new region, Papuasia, whose eastern boundary extends to line 5 in map 2.[7]

Using the Flora Malesiana definition, Malesia has a shared tropical flora derived mostly from Asia, but also with numerous elements of the Antarctic flora. Malesia is a hotspot of global biodiversity. In 1995, it was estimated that there were 42,000 species of vascular plants, of which 70% were endemic. By comparison, Europe, which is about three times the area, had 11,000 species of vascular plants, of which about 30% were endemic.[8]

Western Malesia (Sundaland)

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Main article: Sundaland

Western Malesia includes the Malay Peninsula and the islands of Sumatra, Java, Bali, and Borneo (area A in map 2). It shares the large mammal fauna of Asia and is known as Sundaland. These islands are on Asia's relatively shallow continental shelf, and were linked to Asia during the ice ages, when sea levels were lower. The south-eastern edge of Sundaland (line 6 in map 2) is the Wallace Line, named after Alfred Russel Wallace, the nineteenth-century British naturalist who noted the difference in fauna between islands on either side of the line.

Dipterocarps are predominant trees in the lowland forests of Sundaland.[9] Sundaland has the greatest diversity of Dipterocarp species, with 10 to 14 native genera and approximately 450 native species, including approximately 267 species on Borneo, 155 on the Malay Peninsula, and 106 on Sumatra.[10]

Central Malesia

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The eastern boundary of central Malesia (area B in map 2) is formed by Lydekker's Line (line 7 in map 2).[5] Central Malesia can be divided into two subareas: the Philippines in the north and Wallacea in the south.

Philippines

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Main article: Ecoregions in the Philippines

The Philippines form the northern part of central Malesia. Most of the Philippines were never connected to the Asian mainland, and have a largely Asian-derived flora, and a distinct mammalian fauna.

The Philippines have approximately 50 species of Dipterocarps in 11 genera.[10]

Wallacea

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Main article: Wallacea

The islands between Sundaland and New Guinea, called Wallacea, form the southern part of central Malesia. They were never linked to the neighboring continents, and have a flora and fauna that include Indomalayan and Australasian elements.

Dipterocarps, which are dominant in Sundaland, are less common in Wallacea, with only 13 species in 4 genera.[10]

Eastern Malesia

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As defined in Flora Malesiana, Eastern Malesia consists of New Guinea and the Bismarck Archipelago (area C in map 2). The eastern end of this definition of Malesia, which includes New Guinea and the Aru Islands of eastern Indonesia, is linked to Australia by a shallow continental shelf, and shares many marsupial mammal and bird taxa with Australia. New Guinea also has many additional elements of the Antarctic flora, including southern beech (Nothofagus) and eucalypts. New Guinea has the highest mountains in Malesia and Papuasia, and vegetation ranges from tropical lowland forest to tundra.

In the second version of the WGSRPD, New Guinea and the Bismarck Archipelago, together with the Solomon Islands, are placed in Papuasia (areas C and D in map 2) rather than Malesia.[7]

Assembly and origins of the Malesian flora

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Major contributions to rainforest assembly have come from floristic elements which were carried on the Indian Plate and montane elements which have come from the Australian Plate (Sahul). The Sahul component is now understood to include substantial two-way exchanges with Sunda inclusive of lowland taxa. Evidence for the relative contributions of the great Asiatic floristic interchanges (GAFIs) with India and Sahul, respectively, to the flora of Malesia comes from contemporary lineage distributions, the fossil record, time-calibrated phylogenies, functional traits, and the spatial structure of genetic diversity. Functional trait and biome conservatism are noted features of montane austral lineages from Sahul (e.g., diverse Podocarpaceae), whereas the abundance and diversity of lowland lineages, including groups such as Syzygium (Myrtaceae) and the Asian dipterocarps (Dipterocarpoideae), reflect a less well understood combination of dispersal, ecology, and adaptive radiations. Thus, Malesian rainforest assembly has been shaped by sharply contrasting evolutionary origins and biogeographic histories.[11]

See also

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References

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Revisions and contributorsEdit on WikipediaRead on Wikipedia

Malesia

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Malesia is a phytogeographical floristic region in the Paleotropical kingdom, encompassing a vast area of and the western Pacific known for its exceptional . It includes the southern , the Greater and , the , , the Moluccas, and up to the , bounded on the west by the Kangar-Pattani line and on the north by the Isthmus of Kra. First delineated as a distinct botanical domain in by Swiss Heinrich Zollinger, Malesia represents a transitional zone between the Indomalayan and Australasian realms, featuring a mix of Asian and Australian floral elements. The region is subdivided into four primary subregions—Sundaland (western Malesia), the , (central transitional zone), and Papuasia (eastern area)—each aligning with globally recognized hotspots characterized by high and . Malesia supports approximately 45,000 of vascular , accounting for about 12% of the world's total . Its ecosystems, dominated by tropical rainforests, dipterocarp forests, and montane habitats, have yielded economically important such as cloves, , and various timber , underscoring its significance in global and conservation. The ongoing Flora Malesiana initiative, a collaborative taxonomic project, continues to catalog this diverse , highlighting the region's role in understanding plant evolution and biogeography across Wallace's Line.

Definition and History

Phytogeographical Concept

Malesia is defined as a biogeographical region within the Paleotropical kingdom, characterized by its unique assemblage of tropical species that bridges continental Asian and island Pacific floras. This phytogeographical concept was first proposed in 1857 by Swiss botanist Heinrich Zollinger, who identified the area as a distinct floral based on shared distributions across and adjacent regions. As part of the broader Indo-Malesian realm in the Paleotropical kingdom, Malesia encompasses tropical and portions of , highlighting its role in global patterns of plant evolution and dispersal. The boundaries of Malesia, as standardized in the Flora Malesiana project, include , , (encompassing islands such as , , , , and the Moluccas), , the Philippines, Timor-Leste, and . This delineation focuses on areas with cohesive floral elements, excluding more distant Pacific islands and beyond the . The region is recognized for its high and diversity, serving as a key unit for systematic botanical documentation. Unlike the faunistic Wallacea, which delineates a narrower transition zone for animal distributions between Asian and Australasian biotas, Malesia's phytogeographical framework emphasizes plant patterns and extends further west and east, incorporating and parts of Papuasia. Shared floral elements, such as the dominant family—prominent in lowland rainforests and emblematic of Malesian dominance—illustrate this distinction, with the family exhibiting high diversity and across the region. Malesia functions as a critical transition zone, where approximately 45,000 blend Indo-Malayan and Oceanian elements, underscoring its status.

Historical Development

The phytogeographical concept of Malesia originated in the mid-19th century with Swiss Heinrich Zollinger, who in 1857 first recognized the distinctive flora of and proposed "Flora Malesiana" as a framework for its study, delineating broad boundaries based on limited collections while excluding much of due to evidence of temperate elements there. This early delimitation emphasized the region's isolation and unique composition, suggesting internal subdivisions into northern, central, and southern zones within western peninsular areas. Alfred Russel Wallace's faunistic observations profoundly influenced botanical interpretations, as his 1860 identification of Wallace's Line—separating Asian-influenced western islands from Australian-influenced eastern ones—prompted adaptations for floral patterns, sparking ongoing debates about including or excluding , whose mixed affinities complicated strict boundaries. Building on these foundations, C.G.G.J. van Steenis provided the seminal modern definition in through the initiation of Flora Malesiana, a comprehensive project that refined core boundaries using analysis of 2,178 genera, established four contact zones and three demarcation knots, and more fully incorporated while dividing Malesia into subregions like , , and the . Van Steenis's work solidified Malesia as a cohesive unit; modern estimates place the number of species at approximately 45,000, highlighting its role as a . Post-1950 refinements further clarified Malesia's position within global systems; Armen Takhtajan in 1986 classified it under the Paleotropical Kingdom's Indo-Malayan Region in his floristic regionalization, emphasizing its tropical affinities and evolutionary history. The edition of the World Geographical Scheme for Recording Plant Distributions (WGSRPD) introduced a significant reclassification by separating Eastern Malesia—encompassing , the , and adjacent islands—into the distinct region of Papuasia, recognizing its stronger Australian connections and reducing overlap with core Malesian flora. These classifications continue to be used as of 2025, with no major boundary changes reported.

Geography

Extent and Boundaries

Malesia encompasses a vast tropical area straddling the primarily between 10°N and 10°S and 95°E to 155°E . This extent covers a diverse array of islands and archipelagos in and the western Pacific, forming a transitional zone between the Indomalayan and Australasian biogeographic realms. The region's boundaries are defined both politically and by natural biogeographic lines that reflect sharp transitions in and distributions. Politically, Malesia includes the full territories of , the , , , and Timor-Leste, along with the western portions of —encompassing , , (), , and the —and the Indonesian-administered western portion of island (shared with to the east). This configuration excludes continental Indochina to the northwest and the entirety of to the southeast, focusing instead on the insular core of and adjacent areas. Natural boundaries delineate Malesia through prominent biogeographic divides, including Wallace's Line, which runs between and , separating the Asian-dominated and of the west () from the mixed Australasian elements in the east (). Further east, Lydekker's Line marks the outer limit, positioned along the western edge of and the Aru Islands, beyond which Australasian influences predominate more strongly. These lines highlight Malesia's role as a dynamic transition zone, with exclusions ensuring the focus remains on its unique insular character rather than continental extensions. Definitions of Malesia's extent have evolved, with early interpretations by C.G.G.J. van Steenis (1950) encompassing the region from the Isthmus of Kra south and east to , including Papuasia and reflecting floristic affinities across the area. The modern consensus, aligned with the World Geographical Scheme for Recording Plant Distributions (WGSRPD) at Level 3, favors this inclusive approach, treating Malesia as a cohesive unit that briefly references subregional divisions like and for distributional recording.

Physical Features and Climate

Malesia is characterized by its archipelagic nature, encompassing over 25,000 islands scattered across the equatorial waters between and , forming one of the world's most extensive island groups. The region includes major landmasses such as , the third-largest island globally at 743,330 square kilometers and shared by , , and ; (473,481 km²) and (138,794 km²) in ; the archipelago; and the western (Indonesian) portion of island, which spans approximately 421,000 km². Volcanic activity is prominent, particularly along the Pacific Ring of Fire, with hosting approximately 127 active volcanoes and the about 24, contributing to dynamic landscapes and periodic seismic events that shape the islands' . The topography of Malesia varies dramatically from to high elevations, influencing habitat diversity across the region. Lowland areas below 500 m feature extensive coastal plains and riverine floodplains supporting dense rainforests, while montane zones between 500 and 1,500 m transition to cloud forests on steeper slopes. High mountain ranges rise prominently, including in northern at 4,095 m, the highest peak between the and , and in , summits exceeding 5,000 m such as at 4,884 m. landscapes, formed by soluble limestone dissolution, are especially notable in , creating tower karsts, sinkholes, and underground river systems that add unique topographic complexity. Climatic conditions in Malesia are predominantly equatorial, fostering lush through consistently high humidity and warmth. Average temperatures range from 25°C to 30°C year-round in lowlands, with minimal seasonal variation, while annual rainfall typically falls between 2,000 and 4,000 mm, creating everwet conditions in core areas like . In , seasonal monsoons introduce drier periods with reduced precipitation, contrasting the uniform wetness elsewhere and leading to varied moisture regimes. further modifies the climate, with temperatures dropping about 0.6°C per 100 m elevation gain and increased orographic rainfall on windward slopes, resulting in cooler, wetter montane environments above 1,500 m. Significant river systems drain Malesia's landscapes, facilitating nutrient transport and sediment deposition in lowlands. The in , Indonesia's longest at 1,143 km, originates in the Schwaner Mountains and flows westward into the , supporting extensive wetlands. Other key waterways include the in , (563 km), and tributaries feeding into the Fly River in New Guinea's western lowlands. Soils are predominantly tropical, highly leached and ultisols due to intense under humid conditions, often nutrient-poor but enriched by in active zones, which promotes the growth of dipterocarp-dominated forests through periodic fertility replenishment.

Floristic Subregions

Sundaland

Sundaland encompasses the terrestrial region of spanning the , , , , and , overlying the , a that was largely exposed during Pleistocene glacial lowstands when sea levels dropped by approximately 120 meters. This exposure connected these landmasses into a contiguous area, facilitating extensive dispersal and mixing of l and faunal elements across what is now a fragmented . The resulting biogeographic unity has shaped Sundaland's , blending Asian continental influences with insular adaptations, while subsequent inundations isolated populations and promoted . The flora of is characterized by exceptional diversity in dipterocarp trees, which form the dominant canopy in lowland rainforests and represent the family's global center of diversity. Over 450 species of occur here, including prominent genera such as and , which thrive in the humid, equatorial climate and nutrient-poor soils typical of the region. Ancient lineages with Gondwanan origins, such as , also feature prominently, contributing to the with species adapted to swampy and coastal habitats. Unique vegetation types further define the landscape, including peat swamp forests dominated by species like and extensive kerangas heathlands on sandy, acidic substrates, where stunted trees and ericaceous shrubs prevail in oligotrophic conditions. Endemism is particularly high within , with serving as a key center where approximately one-third of —out of an estimated 15,000—are found nowhere else. This includes numerous dipterocarp endemics, such as 162 restricted to the island, underscoring the role of topographic complexity and isolation in driving diversification. As the core of the , the region harbors more than 25,000 overall, with over 60% endemic, highlighting its status as one of Earth's most floristically rich and threatened areas.

Philippines

The Philippines, comprising approximately 7,100 islands situated between to the north and to the south, forms an isolated archipelago within Malesia, separated from the continental shelf of by deep oceanic features such as the and . This tectonic isolation, persisting since the Tertiary period, has promoted extensive and high levels of in the region's flora, as the deep trenches prevented land connections even during Pleistocene sea-level lows. The Philippine flora encompasses around 9,250 species, with over 50% endemic to the , underscoring its status as one of the world's 36 biodiversity hotspots characterized by exceptional diversity and endemism. Prominent among the endemics is Rafflesia schadenbergiana, a holoparasitic with the largest flower in the , reaching up to 80 cm in diameter and confined to Island. The orchid family (Orchidaceae) exemplifies this diversity, with approximately 1,100 species recorded, of which about 900 are endemic, thriving in the 's varied montane and lowland habitats. Key floral elements include around 50 species of , such as those in the genera Hopea and Parashorea, which dominate lowland rainforests and contribute to the structural complexity of these ecosystems. Unique adaptations are evident in ultramafic soils, prevalent on islands like and , where nickel hyperaccumulators such as Rinorea niccolifera—a shrub capable of sequestering up to 18,000 μg/g in its leaves—have evolved to tolerate and exploit high metal concentrations in serpentine-derived substrates. This edaphic specialization highlights the role of geological heterogeneity in driving Philippine plant diversification within the Malesian context.

Wallacea

Wallacea represents the transitional phytogeographical subregion within Malesia, characterized by its position as a biogeographical crossroads between Asian and Australasian floral influences. This area encompasses the islands of , the Maluku (Moluccas), and the , situated between Wallace's Line to the west—separating it from the —and Weber's Line to the east, which delineates the boundary toward Papuasia. The deep ocean trenches and complex island in this zone have historically impeded straightforward dispersal of plant species, fostering a unique mosaic of floristic elements despite the barriers. The diversity of is estimated at around 10,000 , reflecting its role as a with significant . Approximately 1,500 of these are endemic, accounting for about 15% of the total flora, many of which are adapted to the region's varied elevations and isolation. Notable examples include montane specialists on , such as several endemic in the Vireya subgenus (e.g., Rhododendron ardii and R. tjiasmantoi), which thrive in high-altitude cloud forests and contribute to the subregion's distinct alpine-like vegetation. is particularly pronounced in isolated habitats, underscoring Wallacea's evolutionary significance. Floristically, Wallacea exhibits a blend of Asian and Australasian elements, with low representation of typically dominant Malesian families. Dipterocarpaceae, a hallmark of wet Asian forests, shows markedly reduced diversity here, with only 13 species across three genera east of Wallace's Line, compared to hundreds in Sundaland. Asian genera like Ficus (Moraceae) are common in lowland and coastal areas, while Australasian families such as Myrtaceae gain prominence in eastern sectors, illustrating the gradual shift toward Papuasian affinities. Vegetation varies markedly, from the wet rainforests of Sulawesi and the Moluccas—supporting mixed evergreen formations—to the drier, deciduous forests and savannas of the Lesser Sundas, where seasonal aridity limits canopy density and favors sclerophyllous species.

Papuasia

Papuasia encompasses the eastern portion of the Malesian floristic region, primarily consisting of the island of —divided between and the Indonesian provinces of Papua and West Papua—along with the and the . This subregion was reclassified as a distinct Level 2 botanical unit in the World Geographical Scheme for Recording Plant Distributions (WGSRPD) in 2001, separating it from the broader Malesia to reflect its unique floristic cohesion with Australasian elements, previously grouped under Eastern Malesia. The area's flora shows significant overlap with the , the ancient continental platform linking New Guinea to , facilitating shared biogeographical patterns. The diversity of Papuasia is estimated at approximately 25,000 , with alone hosting over 13,600 across 1,742 genera and 264 families, underscoring its status as the world's most species-rich . is exceptionally high, exceeding 60% in , where more than 9,300 are unique to the , driven by its rugged topography, climatic gradients, and isolation. Cloud forests, particularly in montane zones between 1,000 and 3,000 meters, harbor specialized taxa such as pitcher plants ( spp.), which thrive in nutrient-poor, mossy habitats and exhibit diverse trapping strategies adapted to high humidity and epiphytic growth. Floristically, Papuasia is dominated by Australasian elements, with the conifer family Araucariaceae playing a prominent role in mid- to upper-montane forests; species like Araucaria hunsteinii (klinki pine) form emergent canopies up to 90 meters tall, contributing to the structural complexity of rainforests. Relict populations of Antarctic beech (Nothofagus spp., subgenus Brassospora) persist in these forests, representing Gondwanan lineages that migrated via the Sahul Shelf and now occupy niches on ultramafic soils and slopes up to 3,100 meters. Above 3,000 meters, vegetation transitions to subalpine shrublands and grasslands, featuring tussock grasses (Poa spp.), sedges, and cushion plants in a cool, misty climate that supports peat-forming bogs and reflects adaptations to frost and poor drainage. This altitudinal zonation highlights Papuasia's role as a bridge between Asian Malesian dipterocarp-dominated lowlands—evident in transitions from Wallacea—and the more temperate Australasian assemblages to the south.

Flora and Vegetation

Plant Diversity and Endemism

Malesia harbors approximately 42,000 of vascular , with around 70% endemic to the region. This remarkable diversity is concentrated primarily in lowland rainforests, where environmental conditions support high rates, while declines progressively with due to cooler temperatures and reduced complexity. Endemism patterns reveal key hotspots within Malesia, notably Borneo with an estimated 10,000 endemic vascular plant species and New Guinea with over 8,000. Genus-level endemism is particularly pronounced in families like , which exhibit elevated rates of unique genera across the region, contributing to Malesia's biogeographical distinctiveness. Notable diversity metrics underscore Malesia's floral wealth, including over 1,000 species, more than 300 palm species, and approximately 9,500 species. Despite comprising only about 3% of the Paleotropical land area, Malesia accounts for roughly 25% of the Paleotropical vascular flora, highlighting its status as a global center of plant biodiversity.

Characteristic Families and Habitats

The family, comprising approximately 700 species, serves as the primary canopy dominant in Malesia's lowland rainforests, where its emergent trees form the upper structural layer and contribute significantly to biomass and timber resources. These trees, including genera such as and , exhibit mast fruiting synchronized across populations, enhancing their ecological dominance in nutrient-limited environments. In contrast, the (palm family) is prominent in wetland and habitats, with diverse species adapted to flooded conditions and providing structural support in swampy lowlands. , another key family, thrives as shrubs and small trees, boasting high and contributing to the dense herbaceous and shrub layers through its versatile growth forms. Malesia's habitats reflect a spectrum of tropical ecosystems, with lowland dipterocarp forests representing the archetypal : , multi-layered canopies reaching 40-50 meters, supported by a rich of climbers, ferns, and palms on well-drained, acidic soils. Montane mossy forests, occurring above 1,200 meters, feature stunted trees draped in epiphytes such as orchids, bryophytes, and lichens, which can account for up to 50% of the due to persistent cloud cover and high humidity. Coastal mangroves, dominated by species like , form intertidal zones with prop roots and pneumatophores that stabilize sediments in saline, anaerobic conditions. Plant adaptations in these habitats underscore evolutionary responses to environmental pressures. Buttress roots, prevalent in large dipterocarp trees, provide mechanical stability in shallow, nutrient-poor soils by expanding anchorage without deep taproots. In seasonal or drier margins of Malesia, leaf sclerophylly—characterized by thick, leathery blades with reinforced cuticles—reduces water loss and herbivory in fluctuating rainfall regimes. During climate shifts, many species exhibit altitudinal migration, with upslope range expansions observed in montane as temperatures rise, allowing persistence in cooler refugia. Unique ecosystems further highlight Malesia's floral specialization. Ultramafic flora, on serpentine-derived soils rich in like , supports plants and high , with adaptations including metal-tolerant physiologies and reduced stature. Peat domes, elevated swamp forests with thick organic layers up to 10 meters deep, host acid-tolerant species that thrive in waterlogged, low-oxygen conditions, forming isolated hotspots.

Biogeographical Origins

Geological Influences

The geological framework of Malesia has been fundamentally shaped by major plate tectonic events, beginning with the collision of the Indian Plate with the Eurasian Plate during the Eocene, around 50 million years ago. This convergence uplifted the Himalayan mountain range and altered patterns, intensifying the by diverting moisture-laden winds eastward into . The enhanced monsoon regime contributed to increased across Malesia, fostering conditions conducive to the development of extensive humid environments over the subsequent epochs. In parallel, the northward drift of the during the Miocene, at rates of approximately 7 cm per year, initiated collisions with the Pacific and Indo-Australian plates, leading to the orogenic uplift of New Guinea's Central Range starting around 15 million years ago. This mountain-building episode not only configured the region's eastern landmass but also created barriers that influenced subsequent climatic and biotic patterns. The Pleistocene epoch introduced dynamic fluctuations driven by glacial-interglacial cycles, with global sea levels dropping by up to 120 meters during glacial maxima, such as the around 20,000 years ago. These regressions exposed the vast , connecting the , Sumatra, Java, and Borneo into a contiguous landmass known as and enabling terrestrial connectivity across what are now separated islands. The associated climatic shifts caused habitat contractions, including savanna expansions and rainforest retreats in lowland Borneo and the Thai-Malay Peninsula, followed by recoveries during interglacial warming phases that promoted habitat expansions. Volcanism and orogeny further defined Malesia's landscape, as the region lies along the , where zones fuel frequent eruptions that deposit fine rich in minerals like , , and silica. This activity forms Andisols, highly fertile soils that enhance plant productivity across and the , supporting dense vegetation on otherwise young terrains. Ongoing tectonic compression has driven mountain building in the , through accretion of island arcs in the Southeast Asian Orogen, and in , where uplift in and adjacent islands created isolated highlands that fragmented habitats and promoted allopatric . Paleoclimatic variations overlaid these tectonic changes, with the featuring a global warming phase during the Middle Miocene Climatic Optimum (17–14 million years ago), when temperatures were about 3–6°C higher than today, leading to the widespread expansion of perhumid rainforests across and other parts of Malesia. Conversely, and arid phases, linked to broader global cooling and tectonic influences, affected more severely, with reduced rainfall favoring dry-adapted scrub and floras in inter-island gaps while maintaining wetter conditions elsewhere.

Assembly of the Flora

The assembly of the Malesian flora involved multiple migration routes that introduced diverse plant lineages into the region, primarily during the Cenozoic era. Laurasian elements, which dominate the Malesian flora at the family level, migrated from Indochina across the exposed Sunda Shelf during periods of low sea levels, facilitating the spread of temperate and evergreen broadleaf trees such as Fagaceae (e.g., Quercus species). Southward migrations from Asia occurred via the Greater Asia Floristic Interchanges (GAFIs), with early exchanges (GAFI 1) triggered by the Eocene collision of the Indian Plate around 48 million years ago, while key tropical families like Dipterocarpaceae and Arecaceae were introduced into Sundaland and the Philippines during the subsequent Oligocene to Miocene. Eastward from Australia, Gondwanan relict lineages crossed into Wallacea and Papuasia during the late Oligocene Sahul Shelf exposure around 26 Ma, exemplified by southern temperate trees such as Nothofagus and Podocarpaceae conifers. Diversification of these migrant lineages within Malesia was driven by a combination of in situ speciation, vicariance, and long-distance dispersal. Isolated islands, particularly in the Philippines, promoted rapid speciation, as seen in orchids where over 1,000 species exhibit high endemism due to fragmented habitats and adaptive radiations. Vicariance events, resulting from tectonic uplifts and sea-level fluctuations that created barriers like Wallace's Line, fragmented populations and fostered divergence, notably in montane lineages. Long-distance dispersal, often mediated by birds and buoyant or fleshy-fruited seeds, enabled colonization across oceanic gaps, with examples including the podocarps (e.g., Dacrycarpus) and Myrtaceae like Syzygium, which show evidence of repeated trans-Wallacean jumps. The timeline of floral assembly began in the with the initial integration of core elements through Sunda-Sahul connections, establishing a mixed matrix. radiations, particularly in around 20–23 Ma, coincided with intensification and tectonic activity in , leading to explosive diversification of canopy dominants like and across and the . During the Pleistocene, climatic oscillations confined many lineages to mountain refugia, preserving in high-elevation habitats amid lowland forest contractions. A key component of this assembly was the bidirectional Malesian-Australian floristic interchange through and Papuasia, involving shared genera such as and Elaeocarpaceae, which underwent reciprocal migrations and hybrid zones in transitional areas like . Recent phylogenetic studies suggest complex dispersal routes for major families like , originating from boreotropical forests and reaching Malesia via multiple Paleogene-Neogene pathways. This exchange, enabled by brief land-bridge connections and dispersal corridors, integrated Australasian elements into Malesian montane forests while allowing Asian tropicals to extend eastward.

Modern Dynamics

Naturalizations and Homogenization

Naturalizations in Malesia refer to the establishment of non-native vascular plant species that reproduce and spread without human intervention, contributing to the region's anthropogenic floral changes. A comprehensive assessment identifies 1,177 naturalized vascular plant species across Malesia, representing approximately 3.7% of the total flora when combined with the estimated 30,724 native species. Richness varies significantly by island group, with the Philippines hosting the highest absolute number at 539 species, followed by Java and Sumatra, while the Maluku Islands have the lowest at 87 species. Dominant families among naturalized species include Fabaceae with 160 species and Poaceae with 138 species, often introduced for agricultural or ornamental purposes and thriving in disturbed habitats. These introductions pose risks to the region's high native endemism by competing with and displacing specialized species in fragmented ecosystems. The history of plant naturalizations in Malesia traces back to colonial trade networks from the 16th to 19th centuries, when European powers introduced crops to support expanding settlements and agriculture. For instance, Manihot esculenta (), originating from , was brought to the by Spanish traders in the early colonial period, likely around the , and subsequently spread across the as a staple food crop. This era saw deliberate introductions of utilitarian via maritime routes, facilitated by botanical gardens and plantations established under Dutch, Spanish, and British influence. Rates of naturalization accelerated in the , particularly since 1950, driven by post-colonial , increased , and horticultural exchanges, with about 25% of current naturalized establishing after this period. Naturalizations have contributed to biotic homogenization, reducing floral distinctiveness among Malesian islands through increased compositional similarity. A 2023 phytogeographic analysis revealed taxonomic homogenization across all island pairs, with an average 2% increase in similarity (H = -0.018), primarily in disturbed areas where human modification correlates strongly with these patterns (Mantel's r = 0.48, p < 0.05). Beta-diversity components declined, including turnover (βsim, H = -0.0069) and nestedness (βnes, H = -0.011), indicating that naturalized species fill similar ecological roles across sites, though no major shifts in overall phytogeographic boundaries have occurred. Key drivers include human activities such as and , which create suitable habitats, alongside vectors like international shipping that inadvertently transport seeds and propagules. A prominent example is , a shrub invasive in , where it proliferates in open disturbed areas, suppressing native regeneration and altering community structure through rapid spread and allelopathic effects.

Conservation and Threats

Malesia's flora faces severe threats from anthropogenic activities, with deforestation being the most pressing issue. In , a core part of Malesia, expansion and have driven significant loss, with approximately 1 million hectares of cover lost annually between 2001 and 2023, contributing to broader regional deforestation rates estimated at around 1.5 million hectares per year across and the Pacific islands of Malesia. In , plantations have threatened significant portions of remaining natural , with existing oil palm plantations covering approximately 2.5 million hectares and ongoing expansion posing further risks as of 2024. In , commercial in has predominantly targeted natural for agricultural conversion. exacerbates these pressures by altering altitudinal vegetation zones, as observed on in , where warming temperatures are projected to shift montane distributions upward, potentially compressing habitats for endemic species. Mining activities in ultramafic soils, prevalent in and other parts of Malesia, further endanger hotspots by causing and soil degradation, with edaphic endemics particularly vulnerable to these disturbances. Several subregions of Malesia qualify as biodiversity hotspots under the Critical Ecosystem Partnership Fund (CEPF) criteria, having lost more than 70% of their original habitat since 1900 while harboring high levels of . Sundaland, encompassing much of and , is classified as critically endangered due to extensive and habitat conversion. The Philippines hotspot is critically endangered, with over 70% habitat loss driven by agriculture and urbanization. Wallacea, including and surrounding islands, faces critical status, where ongoing land clearance has reduced forest cover dramatically, threatening thousands of endemic plant species. Conservation initiatives aim to mitigate these threats through protected areas and international collaboration. In , approximately 27% of forested land is designated as protected, including 15.6% as protected forests and 11.7% as conservation areas, covering over 120 million hectares of state forest land as of 2024. The Flora Malesiana project, an ongoing international effort, documents and inventories the region's diversity to support targeted conservation, having advanced taxonomic knowledge for thousands of since its inception. efforts are bolstered by the Strategic Plan of Action for Forestry Cooperation (2016-2025), which promotes sustainable forest management and restoration across member states, including joint initiatives for climate-resilient planting in Malesian landscapes; the plan concluded in 2025 with mixed progress on implementation. Persistent challenges hinder progress, including illegal trade in rare plants such as orchids and species, which fuels and disturbance in and . The disrupted monitoring from 2020 onward, delaying assessments and enforcement in remote areas. As of 2025, the indicates that thousands of Malesian plant species are threatened, with at least 22% of assessed trees in at risk of due to combined loss and exploitation. In 2024, experienced a slight decrease in primary forest loss to 258,000 hectares.

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