Subfossil lemurs are lemurs from Madagascar that are represented by recent (subfossil) remains dating from nearly 26,000 years ago to approximately 560 years ago (from the late Pleistocene until the Holocene). They include both extant and extinct species, although the term more frequently refers to the extinct giant lemurs. The diversity of subfossil lemur communities was greater than that of present-day lemur communities, ranging from as high as 20 or more species per location, compared with 10 to 12 species today. Extinct species are estimated to have ranged in size from slightly over to roughly . Even the subfossil remains of living species are larger and more robust than the skeletal remains of modern specimens. The subfossil sites found around most of the island demonstrate that most giant lemurs had wide distributions and that ranges of living species have contracted significantly since the arrival of humans.
Despite their size, the giant lemurs shared many features with living lemurs, including rapid development, poor day vision, relatively small brains, and female-dominated hierarchies. They also had many distinct traits among lemurs, including a tendency to rely on terrestrial locomotion, slow climbing, and suspension instead of leaping, as well as a greater dependence on leaf-eating and seed predation. The giant lemurs likely filled ecological niches now left vacant, particularly seed dispersal for plants with large seeds. There were three distinct families of giant lemur, including the Palaeopropithecidae (sloth lemurs), Megaladapidae (koala lemurs), and Archaeolemuridae (monkey lemurs). Two other types were more closely related and similar in appearance to living lemurs: the giant aye-aye and Pachylemur, a genus of "giant ruffed lemurs".
Subfossil remains were first discovered on Madagascar in the 1860s, but giant lemur species were not formally described until the 1890s. The paleontological interest sparked by the initial discoveries resulted in an overabundance of new species names, the allocation of bones to the wrong species, and inaccurate reconstructions during the early 20th century. Discoveries waned during the mid-20th century; paleontological work resumed in the 1980s and resulted in the discovery of new species and a new genus. Research has recently focused on diets, lifestyle, social behavior, and other aspects of biology. The remains of the subfossil lemurs are relatively recent, with all or most species dating within the last 2,000 years. Humans first arrived on Madagascar around that time and hunting likely played a role in the rapid decline of the lemurs and the other megafauna that once existed on the large island. Additional factors are thought to have contributed to their ultimate disappearance. Oral traditions and recent reports of sightings by Malagasy villagers have been interpreted by some as suggesting either lingering populations or very recent extinctions.
Diversity
Extinct giant lemurs
Until recently, giant lemurs existed in Madagascar. Although they are only represented by subfossil remains, they were modern forms, having adaptations unlike those seen in lemurs today, and are counted as part of the rich lemur diversity that has evolved in isolation for up to 60 million years. All 17 extinct lemurs were larger than the extant forms, including the largest living lemurs, the indri (Indri indri) and diademed sifaka (Propithecus diadema), which weigh up to . The estimated weights for the subfossil lemurs have varied. Techniques used for these weight estimations include the comparison of skull lengths, tooth size, the head diameter of the femur, and more recently, the area of cortical bone (hard bone) in long bones (such as the humerus). Despite the variations in the size estimates for some species, all subfossil lemurs were larger than living species, weighing or more, and one species may have weighed as much as .
All but one species, the giant aye-aye, are thought to have been active during the day. Not only were they unlike the living lemurs in both size and appearance, they also filled ecological niches that no longer exist or are now left unoccupied. Their remains have been found in most parts of the island, except for the eastern rainforests and the Sambirano domain (seasonal moist forests in the northwest of the island), where no subfossil sites are known. Radiocarbon dates for subfossil lemur remains range from approximately 26,000 years BP (for Megaladapis in northern Madagascar at the Ankarana Massif) to around 500 years BP (for Palaeopropithecus in the southwest).