'', a
xiphosuran (early relative of horseshoe crabs) from the
Ordovician, around 445 million years ago, which already bears a close resemblance to living horseshoe crabs The fossil record of
Xiphosura, the broader group that includes horseshoe crabs and their extinct relatives, extends back to the
Early Ordovician, around 480 million years ago. Ordovician xiphosurans, such as
Lunataspis, already bear a close resemblance to living horseshoe crabs. For modern horseshoe crabs, their earliest appearance was approximately 250 million years ago during the
Early Triassic. Because they have seen little morphological change since then, extant (surviving) forms have been described as "
living fossils". Horseshoe crabs resemble
crustaceans but belong to a separate subphylum of the
arthropods,
Chelicerata. Horseshoe crabs are closely related to the extinct
eurypterids (sea scorpions), which include some of the largest arthropods ever to have existed, and the two may be
sister groups. The difficult-to-classify
chasmataspidids are also thought to be closely related to horseshoe crabs. The
radiation of horseshoe crabs resulted in 22 known species, of which only 4 remain. The
Atlantic species is sister to the three Asian species, the latter of which are likely the result of two divergences relatively close in time. The last common ancestor of the four extant species is estimated to have lived about 135 million years ago in the
Cretaceous. Limulidae is the only extant
family of the
order Xiphosura, and contains all four living
species of horseshoe crabs: •
Carcinoscorpius rotundicauda, the mangrove horseshoe crab, found in South and Southeast Asia •
Limulus polyphemus, the Atlantic or American horseshoe crab, found along the Atlantic coast of the United States and the Southeast Gulf of Mexico •
Tachypleus gigas, the Indo-Pacific, Indonesian, Indian, or southern horseshoe crab, found in South and Southeast Asia •
Tachypleus tridentatus, the Chinese, Japanese, or tri-spine horseshoe crab, found in Southeast and East Asia
Genera After Bicknell et al. 2021 and Lamsdell et al. 2020
Ballagan Formation, Scotland, Early
Carboniferous (
Tournaisian) (Considered Xiphosura
incertae sedis by Lamsdell, 2020 Early Jurassic (
Sinemurian)
Moltrasio Limestone, Italy • †
Volanalimulus Lamsdell, 2020 Early Triassic, Madagascar. • Subfamily Limulinae Leach, 1819 • †
Crenatolimulus Feldmann et al., 2011 Upper Jurassic (upper
Tithonian)
Kcynia Formation, Poland. Lower Cretaceous (
Albian)
Glen Rose Formation, Texas, USA •
Limulus O. F. Müller, 1785
Pierre Shale,
United States, Late Cretaceous (
Maastrichtian), Atlantic North America, Recent • Subfamily
Tachypleinae Pocock, 1902 •
Carcinoscorpius Pocock, 1902, Asia, Recent •
Tachypleus Leach, 1819 Upper Cretaceous (
Cenomanian) Haqel and
Hjoula Konservat-Lagerstatten, Lebanon, Upper
Eocene Domsen Sands, Germany, Asia, Recent
Phylogeny The horseshoe crab's position within
Chelicerata is complicated. However, most morphological analyses have placed them outside the
Arachnida. In response, a more recent paper has again placed horseshoe crabs as separate from the arachnids. This new study utilized both new and more complete
sequencing data while also sampling a larger number of
taxa. Below is a
cladogram showing the internal relationships of Limulidae (modern horseshoe crabs) based on morphology. It contains both extant and extinct members. This was followed by at least two, possibly three, WGDs in a common ancestor of the living horseshoe crabs. This phenomenon is known as
sexual size dimorphism and results in the females having a larger average size than males. The existence of this trend is likely due to a combination of two things: • First, females take a year longer to mature and undergo an additional molt, giving them a larger average body size. • Second, larger female horseshoe crabs can house more eggs within their bodies. This lets them pass on more genetic material than smaller females during each mating cycle, making larger females more prevalent. == Anatomy and physiology ==