Arxiu d'etiquetes: living fossil

Horseshoe crabs: “living fossils” among arthropods

Xiphosurans or horseshoe crabs are probably the most ancient living arthropods known nowadays. These prehistoric-like, marine and currently scarce organisms related to arachnids have survived since ancient times without suffering almost any obvious change…until now. In this article, we will introduce you the main traits of these arthropods, as well as their current threats.

What are xiphosurans?

Xiphosurans (from Ancient Greek xíphos ‘sword’ and ourá ‘tail’), commonly known as horseshoe crabs, are a group of marine arthropods dating from as far back as the Ordovician (485,4 ±1,9 – 443,8 ±1,5 myr), in the Palaeozoic Era. Originally, they represented an important fraction of marine fauna; however, their number is extremely scarce nowadays, with only 4 extant species belonging to one order (Limulida) being the sole survivors of a once great radiation. The rest of members are fossils.

To know more about fossils: Knowing fossils and their age“.

Limulus polyphemus or Atlantic horseshoe crab. Source: Public Domain.

Current xiphosuran species are considered ‘living fossils as they haven’t undergone obvious morphological changes in comparison with Carboniferous and Triassic fossil forms. Moreover, they are the only ones that survived different extinction events.

Xiphosurans’ place on the tree of life

Like pycnogonids or sea spiders, xiphosurans’ place on the tree of life has been widely discussed. Until recently, xiphosurans were classified along with the eurypterids or sea scorpions (currently extinct) forming the Merostoma group, because they seemed to share some morphological traits. However, some deeper analyses showed that these organisms weren’t related, so ‘Merostomata’ is considered an artificial group nowadays.

To know more about pycnogonids: ‘Spiders from the deep sea: Pycnogonida’.

Eurypterus, the most common eurypterid fossil and also the first described genus. Author: Obsidian Soul, CC.

Currently, the most accepted stance is that xiphosurans constitute a class of arthropods by themselves (Xiphosura) inside the superclass Chelicerata (subphylum Cheliceromorpha). Moreover, they are classified within the euchelicerates along with two more classes: Arachnida and Eurypterida.

And above everything…despite their appearance and their marine habits, they’re NOT related to crustaceans!

Source: Tree of Life Web Project.

External and internal anatomy

As most of modern cheliceromorphs, the xiphosurans have the body divided in two parts or tagmata (prosoma and opisthosoma), the head not differentiated from the thorax, and antennae and mandibles absent. However, the defining trait of cheliceromorphs is the presence of chelicerae, a pair of modified preoral appendages mostly linked to feeding functions. In spiders, the chelicerae form fangs that most species use to inject venom.

Modern xiphosurans reach up to 60 cm in adult length, but their Paleozoic relatives were usually smaller, sometimes as small as 1 to 3 cm long. Dorsally, their body is covered with a not-segmented tough chitinous cuticle divided in two articulated parts more or less equivalent to the prosoma and the opisthosoma:

Dorsal view. Modified picture, original photography property of Didier Descouens, CC.

Now, let’s see the main anatomical traits of living xiphosurans (Limulida):

Tagmata: prosoma and opisthosoma

In the prosoma, the cuticle has three ridges: one median ridge and two lateral ridges. In the anterior part of the median ridge there are located two small ocelli, while in the external surface of lateral ridges the are located the compound eyes. The cuticle extends laterally towards the opisthosoma forming a kind of wings called genal spines. Ventrally and anteriorly, the cuticle forms a wide triangular area known as hypostome where some sensorial organs are located (e.g. ventral ocelli and frontal organ).

Opisthosomal segments appear fused in the modern xiphosurans (on the contrary, they are differentiated in all specimens of the order ‘Synziphosurina’, currently extinct); however, opisthosomal segments can still been distinguished by the lateral opisthosomal spines and the dorsal fossae (a total of 6 pairs, corresponding to the 6 segments of the opisthosoma). The opisthosoma terminates in a long caudal spine, commonly referred to as a telson.

Dorsal view. Modified picture, original photography property of Didier Descouens, CC.

Appendages

Xiphosurans have 6 pairs of prosomal appendages: one pair of chelicerae to capture preys (or other food particles) and 5 pairs of walking legs. Xiphosurans’ legs have a double function: besides allowing them to walk and swim, the legs’ bases have hard and sharped teeth to grind the food (gnathobase). These special bases make contact medially forming a duct (endostome) through which food is transported to the mouth. All legs end in well-developed pincers, except the first pair in males. In both sexes, the last pair has an organ called flabella they use to analyse water composition.

In the prosoma, we can also see a pair of appendages morphologically related to the first pair of opisthosomal appendages: the chilaria. These appendages, which are thought to be vestiges of the first opisthosomal segment’s legs, act as block for food to not escape behind the last pair of moving legs.

Prosomal appendages (ventral view). Modified picture, original photography property of Wayne marshall, CC on Flickr.

The opisthosoma has 6 pairs of modified appendages: one pair of genital operculum more or less fused and 5 pairs of book gills to breath under water, which are protected by the operculum flaps.

Opisthosomal appendages (ventral view). Modified picture, original photography property of KatzBird, CC on Flickr.

A very special circulatory system

Despite being arthropods, xiphosurans have a well-developed circulatory system with ‘veins’ and ‘arteries’ that resemble of which of more complex organisms. Their blood contains two cellular types: amebocytes, equivalent to leucocytes, and cyanocites, equivalent to erythrocytes but with hemocyanin instead of hemoglobin. When the hemocyanin is attached to oxygen molecules or is exposed to air, xiphosurans’ blood acquires a characteristic blue tonality.

The blue liquid is its blood!. Author: Dan Century, CC on Flickr.

Biology

Reproduction and life cycle

During mating seasons, horseshoe crabs move to shallow waters, shore of beaches and estuaries in massive groups. Males climb onto the back of females, gripping them with their rudimentary first pair of pincers; then, females move to the shore with a male on their backs while looking for a good place to bury the eggs. Females usually lay from 200 to 300 not fertilised eggs. Finally, males cover the eggs with sperm (external fertilization).

Author: U.S. Fish and Wildlife Service Northeast Region, CC on Flickr.

After hatching, xiphosurans go through two pelagic larval stadiums before reaching the adult form linked to the substrate: trilobite larvae, which has the opisthosomal appendages uncompletely developed and a short telson, and prestwiquianela larvae, which has all the appendages completely developed. They have a 20 years life span.

Ecology and distribution

All living horseshoe crabs live in shallow marine waters, despite some of their fossil relatives also inhabited freshwaters and brackish water habitats. They usually live on sandy and silty substrates at 3-9 metres deep. They’re specialized on digging, for what they use both the margins of their though cuticle and the first four pairs of moving legs; at the same time, they use the telson to lift the opisthosoma so that the fifth pair of moving legs could analyse and filter the surrounding water.

When swimming, they do it upside down, as we can see in the following video property of Wayne Brear:

Horseshoe crabs are generally predators of different species of annelids, molluscs, as well as of other groups of benthic invertebrates. However, they can also feed on algae.

Current diversity of xiphosurans is represented by 4 species, all of them belonging to the order Limulida: Limulus polyphemus (Atlantic coast of North America), Tachypleus tridentatus, Tachypleus gigas and Carcinoscorpius rotundicauda (Indo-Pacific coast).

Rough distribution of the 4 living xiphosuran species. Source: Charmichael & Brush, 2012.

What is their current conservation status?

Humans have done it again. Despite of been living on Earth since prehistoric eras and even been survived to different extinction events, the horseshoe crabs are now more threatened than ever due to anthropic causes. Among the main threats horseshoe crabs must face we can list the ones that follow:

  • Habitat alteration: water temperature changes due to global warming, contamination and declining of quality of water, and destruction of shores and shallow water environments (essential for these organisms to accomplish mating). This is, probably, the most problematic threat.
  • They are used as baits for fishing industries.
  • They are used for biomedical purposes: xiphosurans’ blood is used to produce a bacterial endotoxin indicator called ‘Limulus amebocyte lysate’ (LAL). The amoebocytes of their blood react against some bacterial endotoxins, forming blood clots. So, the LAL test is used to detected different bacteria in a wide variety of materials. Currently, the way to extract blood from their bodies is quite invasive so, despite returning them to their native habitats after the extraction, they still experience a big mortality rate.
  • They are harvested for being used in researches about vision, endocrinology and other physiological processes.
  • They are captured to be commercialized as food: in some Asian countries, horseshoe crabs are served in traditional dishes and rituals, even though this not seems to be the major threat they must face.
  • They are commercialized as pets.
Blood extraction for LAL. Source: National Geographic/Getty Images.
Dish based on horseshoe crab in Si Racha (Thailand). Author: Marshall Astor, CC.

There exist scarce data about the conservation status of the living species of xiphosurans. The most part of information comes from the American species Limulus polyphemus, which is now classified as ‘Vulnerable‘ and with a decreasing population trend since the last 100 years by the IUCN.

Recently, horseshoe crabs have been recognized as important components of benthic food webs, and their eggs supplement the diet of migratory shorebirds along the Atlantic coast of the USA. So, there is considerable interest in propagating and restoring horseshoe crab populations to support these valuable economic, biomedical, ecological and cultural services.

.           .           .

Solving the phylogenetic relationships of a group mainly composed by extinct organisms is not a piece of cake. But now that we start to glimpse them, we are slowly condemning these organisms to their disappearance. Nor the living fossils are safe from the sixth extinction!

References

  • Carmichael, R. H. & Brush, E. (2012). Three decades of horseshoe crab rearing: a review of conditions for captive growth and survival. Reviews in Aquaculture, 4(1): 32-43.
  • Chacón, M. L. M. & Rivas, P. (2009). Paleontología de invertebrados. IGME.
  • Grimaldi, D. & Engel, M. S. (2005). Evolution of the Insects. Cambridge University Press.
  • Marshall, A. J., & Williams, W. D. (1985). Zoología. Invertebrados (Vol. 1). Reverté.
  • Pujade-Villar, J. & Arlandis, J. S. (2002). Fonaments de zoologia dels artròpodes (Vol. 53). Universitat de València.
  • The IUCN Red List of Threatened Species: Horseshoe crabs.
  • Xifosuros: Animales de la realeza. Boletín Drosophila.

Main photo property of Didier Descouens, CC.

Knowing fossils and their age

In All You Need Is Biology we often make reference to fossils to explain the past of living beings. But what is exactly a fossil and how is it formed? Which is the utility of fossils? Have you ever wondered how science knows the age of a fossil? Read on to find out!

WHAT IS A FOSSIL?

If you think of a fossil, surely the first thing that comes to your mind is a dinosaur bone or a petrified shell that you found in the forest, but a fossil is much more. Fossils are remnants (complete or partial) of  living beings that have lived in the past (thousands, millions of years) or traces of their activity that are preserved generally in sedimentary rocks. So, there are different types of fossils:

  • Petrified and permineralized fossils: are those corresponding to the classical definition of fossil in which organic or hollow parts are replaced with minerals (see next section). Its formation can leave internal or external molds in which the original material may disappear.

    cangrejo herradura, fósil, cosmocaixa, mireia querol rovira, horseshoe crab
    Petrified fossil of horseshoe crab and its footsteps. CosmoCaixa. Photo: Mireia Querol Rovira
  • Ichnofossils (trace fossils): traces of the activity of a living being that are recorded in the rock and give information about the behavior of the species. They may be changes in the environment (nests and other structures), traces (footprints), stools (coprolites -excrements-, eggs …) and other traces such as scratches, bites…
    Cosmocaixa, huevos, dinosaurio, nido, mireia querol rovira
    Dinosaur eggs (nest). CosmoCaixa. Photo: Mireia Querol Rovira

    coprolitos, cosmocaixa, excrementos fósiles, mireia querol rovira
    Coprolites, CosmoCaixa. Photo: Mireia Querol Rovira
  • Amber: fossilized resin of more than 20 million years old. The intermediate state of amber is called copal (less than 20 million years) old. The resin, before becoming amber can trap insects, arachnids, pollen… in this case is considered a double fossil.

    Pieza de ámbar a la lupa con insectos en su interior. CosmoCaixa. Foto: Mireia Querol Rovira
    Piece of amber with insects inside, CosmoCaixa. Photo: Mireia Querol Rovira
  • Chemical fossils: are fossil fuels like oil and coal, which are formed by the accumulation of organic matter at high pressures and temperatures along with the action of anaerobic bacteria (bacteria that don’t use oxygen for metabolism).
  • Subfossil: when the fossilization process is not completed the remains are known as subfossils. They don’t have more than 11,000 years old. This is the case of our recent ancestors (Chalcolithic).

    Ötzi a subfossil. It is Europe’s oldest natural mummy. He lived during the Chalcolithic (Copper Age) and died 5300 years ago. Photo: Wikimedia Commons
  • Living fossils: name given to today’s living organisms very similar to species extinct. The most famous case is the coelacanth, it was believed extinct for 65 million years until it was rediscovered in 1938, but there are other examples such as nautilus.

    ammonites, nautilus, cosmocaixa, fósil, mireia querol rovira
    Comparison between the shell of a current nautilus (left) with an ammonite of millions of years old (right). CosmoCaixa. Photo: Mireia Rovira Querol
  • Pseudofossils: are rock formations that seem remains of living beings, but in reality they are formed by geological processes. The best known case is pyrolusite dendrites that seem plants. 
Infiltraciones de priolusita en piedra calcárea. CosmoCaixa. Foto: Mireia Querol
Pirolusita infiltrations in limestone. CosmoCaixa. Photo: Mireia Querol

Obviously fossils became more common after the appearance of hard parts (shells, teeth, bones …), 543 million years ago (Cambrian Explosion). The fossil record prior to this period is very scarce. The oldes tknown fossils are stromatolites, rocks that still they exist today formed by the precipitation of calcium carbonate because of the activity of photosynthetic bacteria.

The science of fossils is Paleontology.

stromatolite, estromatòli, estromatolito, mireia querol rovira, fossil, fósil
Stromatolite 2,800 million years old, Australian Museum. Photo: Mireia Querol Rovira

HOW A FOSSIL IS FORMED?

The fossilization can occur in five ways:

  • Petrifaction: is the replacement of organic material by minerals from the remains of a living being buried. An exact copy of the body is obtained in stone. The first step of petrificationis  permineralizationthe pores of the body are filled with mineral but organic tissue is unchanged. It is the most common method of fossilized bones).
  • Gelling: the body becomes embedded in the ice and don’t suffer transformations .
  • Compression : the dead body is on a soft layer of soil, such as clay, and is covered by layers of sediment .
  • Inclusion : organisms trapped in amber, or petroleum .
  • Impression: organisms leave impressions in the mud and the trace is preserved until the clay hardens.
    Fossilization processes and resulting fossils. Unknown author

    UTILITY OF FOSSILS

  • Fossils give us information on how living things were in the past, resulting in evidence of the biological evolution and help to establish the lineages of living things today.
  • Allow analyzing of cyclical phenomena such as climate change, atmosphere-ocean dynamics and even orbital perturbations of the planets.
  • Those who are of a certain age can be use to date the rocks in where they are found (guide fossils).
  • They give information of geological processes such as the movement of the continents, the presence of ancient oceans, formation of mountains…
  • The chemical fossils are our main source of energy .
  • They give climate information from the past, for example, studying the growth of rings in fossilized trunks or deposition of organic matter in the glacial varves.
    mireia querol rovira, tronco fósil, xilópalo, AMNH
    Fossil trunks where growth rings are observed. American Museum of Natural History. Photo: Mireia Querol Rovira

    DATING FOSSILS

    To determine the age of fossils there are indirect methods (relative dating) and direct (absolute dating). As there is no perfect method and accuracy decreases with age, the sites are often dated with more than one technique.

    RELATIVE DATING

    The fossils are dated according to the context in which they are found, if they are associated with other fossils (guide fossils) or objects of known age and it depends on the stratum they are found.

    In geology, stratums are different levels of rocks that are ordered by their depth: according to stratigraphy, the oldest ones are found at greater depths, while the modern ones are more superficial, as the sediments have not had much time to deposit on the substrate. Obviously if there are geological disturbances dating would be wrong if there were only this method.

    stratigraphic chart fossils
    Stratigraphic timescale. Picture: Ray Troll

    ABSOLUTE DATING

    This methods are more accurate and are based on the physical characteristics of matter.

    RADIOMETRIC DATING

    They are based on the rate of decay of radioactive isotopes in rocks and fossils. Isotopes are atoms of the same element but with different number of neutrons in their nuclei. Radioactive isotopes are unstable, so they are transformed into a more stable ones at a rate known to scientists emitting radiation. Comparing the amount of unstable isotopes to stable in a sample, scientits can estimate the time that has elapsed since the fossil or rock formed.

    Carbon 14 cycle. Unknown author
    Carbon-14 cycle. Unknown author
  • Radiocarbon (Carbon-14): in living organisms, the relationship between C12 and C14 is constant, but when they die, this relationship changes: the uptake of C14 stops and decay with a descomposing rate of 5730 years. Knowing the difference between C12 and C14 of the sample, we can date when the organism died. The maximum limit of this method are 60,000 years, therefore only applies to recent fossils.
  • Aluminum 26-Beryllium 10: it has the same application as the C14, but has a much greater decaying period, allowing  datings up to 10 datings millions of years, and even up to 15 million years.
  • Potassium-Argon (40K/40Ar): is used to date rocks and volcanic ash older than than 10,000 years old. This was the method used to date the Laetoli footprints, the first traces of bipedalism of our lineage left by Australopithecus afarensis.
  • Uranium Series (Uranium-Thorium): various techniques with uranium isotopes. They are sed in mineral deposits in caves (speleothems) and in calcium carbonate materials (such as corals).
  • Calcium 41: allows to date bones in a time interval from 50,000 to 1,000,000 years .

PALEOMAGNETIC DATING

The magnetic north pole has changed throughout the history of Earth and its geographical coordinates are known in different geological eras.

Some minerals have magnetic properties and are directed towards the north magnetic pole when in aqueous suspension, for example clays. But when laid on the ground, they are fixed to the position that the north magnetic pole was at the time. If we look at what coordinates are oriented such minerals at the site, we can associate it with a particular time.

Deposición de partículas magnéticas orientadas hacia el polo norte magnético. Fuente: Understanding Earth, Press and Seiver, W.H. Freeman and Co.
Deposition of magnetic particles oriented towards the magnetic north pole. Source: Understanding Earth, Press and Seiver, W.H. Freeman and Co.

This dating is used on clay remains and as the magnetic north pole has been several times in the same geographical coordinates, you get more than one date. Depending on the context of the site, you may discard some dates to reach a final dating.

THERMOLUMINESCENCE DATING AND  OPTICALLY STIMULATED LUMINESCENCE (OSL)

Certain minerals (quartz, feldspar, calcite …) accumulate in its crystal structure changes due to radioactive decay of the environment. These changes are cumulative, continuous and time dependent to radiation exposure. When subjected to external stimuli, mineral emits light due to these changes. This luminescence is weak and distinct as apply heat (TL), visible light (OSL) or infrared (IRSL).

Fluorite's thermoluminescence. Photo: Mauswiesel
Fluorite’s thermoluminescence. Photo: Mauswiesel

Can be dated samples that were protected from sunlight and heat to more than 500 ° C, otherwise the “clock” is reset as the energy naturally releases.

ELECTRON PARAMAGNETIC RESONANCE (ESR)

The ESR (electro spin resonance) involves irradiating the sample and measuring the energy absorbed by the sample depending on the amount of natural radiation which it has been subjected during its history. It is a complex method which you can get more information here.

REFERENCES