Chelicerata
Evolution
Chelicerata Classification
Kingdom Animalia Phylum Arthropoda Clade Arachnomorpha Subphylum Chelicerata Class Arachnida Order Acarina (mites and ticks) Order Amblypygi (whip spiders and whip scorpions) Order Araneae (spiders - 109 ) Order Haptopoda (one species - Plesiosiro madeleyi) † Order Opiliones (harvestmen) Order Palpigradi (microwhip scorpion) Order Phalangiotarbida † (enismatic) Order Pseudoscorpionida (pseudoscorpions) Order Ricinulei (hooded tickspiders) Order Schizomida (shorttailed whipscorpion) Order Scorpiones (scorpions) Order Solifugae (camel spiders) Order Thelyphonida (vinegaroons) Order Trigonotarbida (early arachnid) † Class Pycnogonida (sea spiders) Order Pantopoda - 10 families Class Merostomata Order Eurypterida (sea scorpions) Order Xiphosura (horseshoe crabs)
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The
chelicerata fossil record tends
to be sparse because their soft, chitinous exoskeletons poorly
preserved. The best soft tissue preservation occur in lagerstätten
sites and fossil
amber. There is considerable disagreement in classifying
older fossils as chelicerates, as is the case of many early
arthropods. For example, there is debate about whether Fuxianhuia
protensa from the early Cambrian Chengjiang
Maotianshan Shales (525 million years ago), was a chelicerate.
Similarly, Kodymirus, is a an arthropod known from the Czech
republic for which there is debate as to its taxonomy as a
eurypterid, aglaspid or chelicerate.
Sanctacaris and Sidneyia, from the Burgess
Shale (505 million years ago) have been classified as chelicerates
(or stem or crown group chelicerates), the former because of
its pattern of tagmosis (how the segments are grouped, especially
in the head) and the latter because of appendages that resemble
those of horseshoe crabs, (Chelicerata
Order Xiphosura); however, cladistic analyses that consider
wider ranges of characteristics place neither as chelicerates.
Resolving the early arthropod debate is hindered by a gap in
the fossil record of some 40 million years between these equivocal
chelicerates, or close relatives, and unequivocal chelicerate
fossils, or at least those for which there exists scientific
consensus.
Palaeotarbus
jerami (picture to lowerleft), an trigonotarbid, is considered
the
oldest known arachnid. The Order Trigonotarbida is an extinct
group of arachnids whose fossil record extends from the late
Silurian
to the early Permian (i.e., some 419 to 290 million years). The
trigonotarbids have been found in European and North America
localities
and in Argentina. Trigonotarbids are mostly found in Carboniferous
coal forest deposits (around 300 million years old) but are
known
from as early as the Late Silurian (around 415 million years
ago). The Rhynie Chert
Lagerstätte of Scotland has pruduced
some especially well-preserved specimens. Trigonotarbids looked
like
spiders, but ostensibly lacked silk spinnerets to produce silk
and were probably not venomous. The Devonian Attercopus fimbriunguis
(386 million years ago) shows the earliest silk spigots
known in the fossil record, but not true spinnerets of true
spiders.
The most scorpion-like of the Eurypterids (and possibly ancestral
to the scorpions), is a diverse group of often spiny Eurypterids
of Superfamily Mixopteracea. Many of these animals were clearly
amphibious, as is indicated by a trail in the Silurian of Ringerike,
Norway, believed to have been made by a large Mixopterus. Carcinosoma
scorpionis late Silurian (Ludlow) of New York reached a length
a half meter. The Late Silurian
Proscorpius has been classified as a scorpion, but differs from
modern ones in that it seems entirely aquatic because it had
gills rather than book lungs or tracheae, and its mouth was
completely
under its head and almost between the first pair of legs, as
in the extinct eurypterids and living horseshoe crabs. Fossils
of
terrestrial scorpions with book lungs have been found in Early
Devonian rocks form about 402 million years ago. Chelicerates
mostly creep people out, as arachnophobes abound, and who can
blame them, as vividly clear from the picture of the yellow
mite
(Prostigmata family Tydeidae) to the above right. If you are
going to look for a fossil yellow mite , look in amber, with
a very powerful
microscope.
Spider
Evolution - Arachnida Order Araneae
Spiders are a more modern rendering of Chelicerata,
and comprise a hugely diverse (with more than 40,000 species
distributed across more than 100 families) taxon of mostly very
skilled and well-armed (e.g., venom and silk)
predators, all honed through several million years of adaptation.
It is fairly undisputed that spiders are monophyletic, comprising
a last common ancestor and all descendants, though their prior
closest ancestor is a long-running dispute. The orb-weaver spiders
of Family Araneidae represent about a quarter of spider diversity
with some 168 genera and more than three thousand species. The
orb weavers are particularly noted for beautiful their webs and
sexual size dimorphism (females up to nine fold larger than males).
They are infamous for their sexual cannibalism. Ostensibly, a
relatively
diminutive
male
was selected
which
enabled a stealthy approach in her highnesses web in dedicated
pursuit of his manly duties - if not stealthy enough,
he became a snack.
If successful and satisfied, he became lunch anyway.
Subphylum
Chelicerata Fossils
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Eurypterus
remipes
Class Merostomata
Order
Eurypterida
Upper Silurian
Bertie Group, New York |
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Liocranid
Spider
Class Arachnida
Order Araneae
Eocene - Oligocene
Kaliningrad District, Russia |
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Jumping
Spiders
Class Arachnida
Order Araneae
Pliocene to Pleistocene
Andes Mountains, Colombia |
Spider
Class Arachnida
Order Araneae
Miopcene
Central Nevada |
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