Mesolenellus
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''Mesolenellus'' is an extinct
genus Genus (; : genera ) is a taxonomic rank above species and below family (taxonomy), family as used in the biological classification of extant taxon, living and fossil organisms as well as Virus classification#ICTV classification, viruses. In bino ...
of
trilobite Trilobites (; meaning "three-lobed entities") are extinction, extinct marine arthropods that form the class (biology), class Trilobita. One of the earliest groups of arthropods to appear in the fossil record, trilobites were among the most succ ...
s that lived during the lower
Cambrian The Cambrian ( ) is the first geological period of the Paleozoic Era, and the Phanerozoic Eon. The Cambrian lasted 51.95 million years from the end of the preceding Ediacaran period 538.8 Ma (million years ago) to the beginning of the Ordov ...
(
Botomian Cambrian Stage 4 is the still unnamed fourth stage of the Cambrian and the upper stage of Cambrian Series 2. It follows Cambrian Stage 3 and lies below the Wuliuan. The lower boundary has not been formally defined by the International Commission ...
), found in Greenland and Spitsbergen.


Etymology

''Mesolenellus'' is a contraction of and ''Olenellus'', the genus from which it was split off. The
epithet An epithet (, ), also a byname, is a descriptive term (word or phrase) commonly accompanying or occurring in place of the name of a real or fictitious person, place, or thing. It is usually literally descriptive, as in Alfred the Great, Suleima ...
''hyperborea'' is a contraction of (Greek ) and ''Boreas'' (), god of the North Wind in Greek mythology, referencing the current geographical position of the deposits of its type location. ''M. svalbardensis'' has been named for the Norwegian island group Svalbard or Spitsbergen, where it was originally collected.


Taxonomy

It was considered a subgenus of ''
Olenellus ''Olenellus'' is an extinct genus of redlichiida, redlichiid trilobites, with species of average size (about long). It lived during the Botomian and Toyonian stages of the Lower Cambrian (''Olenellus''-zone), , in what is currently North America ...
'' before. The nearest relatives of ''Mesolenellus'' are the species of the genus '' Mesonacis'', with which it constitutes the subfamily
Mesonacinae The Mesonacinae comprise an extinct subfamily of trilobites that lived during the Botomian Cambrian Stage 4 is the still unnamed fourth stage of the Cambrian and the upper stage of Cambrian Series 2. It follows Cambrian Stage 3 and lies below ...
.


Distribution

* ''Mesolenellus hyperborea'' occurs in the Botomian ( ''Nevadella''-zone) of the
paleocontinent A paleocontinent or palaeocontinent is a distinct area of continental crust that existed as a major landmass in the geological past. There have been many different landmasses throughout Earth's time. They range in sizes; some are just a collection ...
Laurentia Laurentia or the North American craton is a large continental craton that forms the Geology of North America, ancient geological core of North America. Many times in its past, Laurentia has been a separate continent, as it is now in the form of ...
, now Greenland (Upper
Buen Formation The Buen Formation is a Formation (geology), geologic formation and Lagerstätte in Peary Land, North Greenland. The shale preserves fossils dating back to the Early Cambrian Period (geology), period (Atdabanian in the local timescale, about 520 ...
, above Brillesø, 1.5 km east of Borglum Elv,
Peary Land Peary Land is a peninsula in northern Greenland, extending into the Arctic Ocean. It reaches from Victoria Fjord in the west to Independence Fjord in the south and southeast, and to the Arctic Ocean in the north, with Cape Morris Jesup, the nor ...
, North-Eastern end of the island). The occurrence of ''M. hyperborea'' has been specified as the early mudstone layer of the Upper Buen Formation. The famous
Sirius Passet Sirius Passet is a Cambrian Lagerstätte in Peary Land, Greenland. The Sirius Passet Lagerstätte was named after the Slædepatruljen Sirius, Sirius sledge patrol that operates in North Greenland. It comprises six places in Nansen Land, on the eas ...
fauna (e.g. '' Kleptothule'' and '' Aaveqaspis'') occurs in the lowest (sandy) member of the Buen Formation and thus predates ''Mesolenellus''. * ''M. svalbardensis'' has been found in the Botomian (''Nevadella''-zone) of Laurentia, now Svalbard/Spitsbergen (lower Slakli Series, Sofiekammen Formation, northern side of the Hornsund, West-Spitsbergen). A specimen that probably belongs to ''M. svalbardensis'' or is closely related was found in Greenland (Schley Fjord Formation, Peary land). There is a further mention of the occurrence in Greenland for the late mudstone layer of the Upper Buen Formation, indicating that ''M. hyperborea'' predated ''M. svalbardensis''.


Habitat

The mudstone in which both species were found indicates deeper, quiet waters.


Ecology

''Mesolenellus hyperborea'' occurs together with '' Limniphacos perspiculum'', ''Serrodiscus'', hyoliths, ''Petrianna fulmenta'' (
Bradoriida Bradoriida, also called bradoriids, are an extinct order of small marine arthropods with a bivalved carapace, which globally distributed, forming a significant portion of the Cambrian and Early Ordovician soft-bodied communities. Affinity Whil ...
), and inarticulate brachiopods.


Description

As with most early trilobites, ''Mesolenellus'' has an almost flat exoskeleton, that is only thinly calcified, and has crescent-shaped eye ridges. As part of the suborder Olenellina, ''Olenellus'' lacks dorsal sutures. Like all other members of the superfamily Olenelloidea, the eye-ridges spring from the back of the frontal lobe (L4) of the central area of the cephalon, that is called glabella. ''Mesolenellus'' also shares the typical character of the whole family Olenellidae that the frontal (L3) and middle pair (L2) of lateral lobes of the glabella are partially merged. This creates two very typical, isolated slits. ''Mesolenellus'' is a genus within the Mesonacinae, with eye-ridges curved but almost parallel to the midline. The back of the eye-ridges is opposite the most backward ring of the glabella (L0 or occipital ring). Genal spines are 6-8 times as long as L0. The outer furrows of the
glabella The glabella, in humans, is the area of skin between the eyebrows and above the nose. The term also refers to the underlying bone that is slightly depressed, and joins the two brow ridges. It is a cephalometric landmark that is just superior ...
are parallel to the midline between the back of the cephalon and the furrow between side lobes L2 and L3. The thorax is 3 times as wide as the axis at the 3rd segment. ''Mesolenellus'' can be distinguished from the sister-genus '' Mesonacis'', where the back of the eye-ridge extends only to the most backward side lobes (L1), genal spines are only 1-5 times as long as L0, and the glabella widens forwards along L1 and L2. Except for in ''Mesonacis fremonti'' the curved eye-ridges are at an angle of 15°-20° with the midline. A third genus ''Olenellus'', that constitutes the second subfamily of the family Olenellidae differs from ''Mesolenellus'' in having genal spines 4-5 times as long as L0, the glabella widens forwards along L1 and L2, and the thorax 4-4½ times wider that the axis at the 3rd segment.


Key to the species


References


External links


'' Trilobite info''
{{Taxonbar, from=Q16985426 Olenellidae Redlichiida genera Cambrian trilobites Cambrian trilobites of Europe Cambrian genus extinctions