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Horseshoe crab

Family of basal chelicerates

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A female Indo-Pacific horseshoe crab, photographed in the West Bengal-Odisha coastal region on the Indian coastline of the Bay of Bengal. It was carried by a local fisher man from the seabed to the co
Shubham Chatterjee · CC BY-SA 3.0

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Through Marine life, Fresh water and Blood

Only four species of horseshoe crab are extant today, the Atlantic horseshoe crab (Limulus polyphemus), native to the eastern coasts of Mexico and the United States, as well as the mangrove horseshoe crab (Carcinoscorpius rotundicauda), tri-spine horseshoe crab (Tachypleus tridentatus) and Indo-Pacific horseshoe crab (Tachypleus gigas), which are native to South, South East, and East Asia.

Most horseshoe crabs are marine, though the mangrove horseshoe crab is often found in brackish water, and the Atlantic horseshoe crab is resident in brackish estuarine ecosystems, such as the Delaware and Chesapeake bays. Additionally, certain extinct species transitioned to living solely in freshwater. Horseshoe crabs primarily live at the water's bottom but they can swim if needed.

Horseshoe crabs are often caught for their blood, which contains Limulus amebocyte lysate, a chemical used to detect bacterial endotoxins. Additionally, they are used as fishing bait in the United States and eaten as a delicacy in some parts of Asia. In recent years, horseshoe crabs have experienced a population decline. This is mainly due to coastal habitat destruction and overharvesting. To ensure their continued existence, many areas have enacted regulations on harvesting and established captive breeding programs.

Phylogeny and evolution

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. The earliest appearance of modern horseshoe crabs 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

  • Incertae sedis
    • †Albalimulus? Bicknell & Pates, 2019 Ballagan Formation, Scotland, Early Carboniferous (Tournaisian) (Considered Xiphosura incertae sedis by Lamsdell, 2020)
    • †Casterolimulus Holland, Erickson & O'Brien, 1975 Late Cretaceous (Maastrichtian) Fox Hills Formation, North Dakota, USA (Inconsistently placed in this family)
    • †Heterolimulus gadeai Vıa & Villalta, 1966 Alcover Limestone Formation, Spain, Middle Triassic (Ladinian)
    • †Limulitella? Størmer, 1952 Middle-Upper Triassic, France, Germany, Tunisia, Russia
    • †Sloveniolimulus Bicknell et al., 2019 Strelovec Formation, Slovenia Middle Triassic (Anisian)
    • †Tarracolimulus Romero & Vıa Boada, 1977 Alcover Limestone Formation, Spain, Middle Triassic (Ladinian)
    • †Victalimulus Riek & Gill, 1971 Lower Cretaceous (Aptian) Korumburra Group, NSW, Australia
    • †Yunnanolimulus Zhang et al., 2009 Middle Triassic (Anisian), Guanling Formation, Yunnan, China
    • †Mesolimulus Middle Triassic-Late Cretaceous England, Spain, Siberia, Germany, Morocco
    • †Ostenolimulus Lamsdell et al. 2021 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. This assumption was challenged when a genetics-based phylogeny found horseshoe crabs to be the sister group to the ricinuleids, thereby making them an arachnid. 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.

Whole genome duplication

The common ancestor of arachnids and xiphosurans (the group that includes horseshoe crabs) underwent a whole-genome duplication (WGD) event. This was followed by at least two, possibly three, WGDs in a common ancestor of the living horseshoe crabs. This gives them unusually large genomes for invertebrates (the genomes of C. rotundicauda and T. tridentatus being approximately 1.72 Gb each). Evidence for the duplication events includes similarity in structure between chromosomes (synteny), and clustering of homeobox genes. Over time, many of the duplicated genes have changed through processes of neofunctionalization or subfunctionalization, meaning their functions are different from what they originally were.

Evolution of sexual size dimorphism

Several hypotheses have been given as possible reasons why a size difference exists between male and female 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:

  1. First, females take a year longer to mature and undergo an additional molt, giving them a larger average body size.
  2. 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.

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