Nemonychidae
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Nemonychidae is a small family of weevils, placed within the ''primitive weevil'' group because they have straight rather than geniculate (elbowed)
antenna Antenna ( antennas or antennae) may refer to: Science and engineering * Antenna (radio), also known as an aerial, a transducer designed to transmit or receive electromagnetic (e.g., TV or radio) waves * Antennae Galaxies, the name of two collid ...
e. They are often called pine flower weevils. As in the Anthribidae, the labrum appears as a separate segment to the clypeus, and the maxillary palps are long and projecting. Nemonychidae have all ventrites free, while Anthribidae have ventrites 1-4 connate or partially fused. Nemonychidae lack lateral carinae on the pronotum, while these are usually present, though may be short, in Anthribidae. Nemonychidae are historically divided into three subfamilies: Nemonychinae of the palearctic region with the single genus ''Nemonyx'' and an unusual host, the angiosperm ''
Delphinium ''Delphinium'' is a genus of about 300 species of annual and perennial flowering plants in the family Ranunculaceae, native throughout the Northern Hemisphere and also on the high mountains of tropical Africa. The genus was erected by Carl Linn ...
''. Most species of the other two subfamilies are associated with
Pinales The order Pinales in the division Pinophyta, class Pinopsida, comprises all the extant conifers. The distinguishing characteristic is the reproductive structure known as a cone produced by all Pinales. All of the extant conifers, such as cedar, ...
feeding on the pollen of the male
inflorescence An inflorescence is a group or cluster of flowers arranged on a stem that is composed of a main branch or a complicated arrangement of branches. Morphologically, it is the modified part of the shoot of seed plants where flowers are forme ...
s. Cimberidinae are found in the Northern hemisphere, while Rhinorhynchinae occur largely in the Southern hemisphere, especially found on
Podocarpaceae Podocarpaceae is a large family of mainly Southern Hemisphere conifers, known in English as podocarps, comprising about 156 species of evergreen trees and shrubs.James E. Eckenwalder. 2009. ''Conifers of the World''. Portland, Oregon: Timber P ...
and
Araucariaceae Araucariaceae – also known as araucarians – is an extremely ancient family of coniferous trees. The family achieved its maximum diversity during the Jurassic and Cretaceous periods and the early Cenozoic, when it was distributed almost worldw ...
. Recent phylogenetic research indicates that the Cimberidinae are sister to all of the remaining
Curculionoidea Weevils are beetles belonging to the superfamily Curculionoidea, known for their elongated snouts. They are usually small, less than in length, and herbivorous. Approximately 97,000 species of weevils are known. They belong to several families, ...
, and it has been proposed to elevate the group to family rank. Both Nemonychidae adults and larvae feed primarily on pollen. When mature, the larvae will drop to the ground from the male cones or flowers they resided in to pupate in the soil less than five centimeters from the surface. There exists a fairly extensive fossil record of Nemonychidae reaching from the upper Jurassic to tertiary
amber Amber is fossilized tree resin that has been appreciated for its color and natural beauty since Neolithic times. Much valued from antiquity to the present as a gemstone, amber is made into a variety of decorative objects."Amber" (2004). In M ...
.


Extant Taxa

Cimberidinae: *''
Acromacer ''Acromacer'' is a genus of pine flower snout beetles in the family Nemonychidae Nemonychidae is a small family of weevils, placed within the ''primitive weevil'' group because they have straight rather than geniculate (elbowed) antennae. The ...
'' *''
Cimberis ''Cimberis'' is a genus of pine flower snout beetles in the family Nemonychidae Nemonychidae is a small family of weevils, placed within the ''primitive weevil'' group because they have straight rather than geniculate (elbowed) antennae. They ...
'' *''
Doydirhynchus ''Doydirhynchus'' is a genus of beetles belonging to the family Nemonychidae Nemonychidae is a small family of weevils, placed within the ''primitive weevil'' group because they have straight rather than geniculate (elbowed) antennae. They ar ...
'' *''
Lecontellus ''Lecontellus'' is a weevil genus.Kuschel, G. 1989: The Nearctic Nemonychidae (Coleoptera: Curculionoidea). Entomologica Scandinavica, 20: 121-171. References External links * Weevil genera {{Weevil-stub ...
'' *'' Pityomacer'' Nemonychinae: *'' Nemonyx'' Rhinorhynchinae: *'' Aragomacer'' *'' Araucomacer'' *'' Atopomacer'' *'' Basiliogeus'' *'' Basiliorhinus'' *'' Brarus'' *'' Bunyaeus'' *'' Eutactobius'' *'' Idiomacer'' *'' Mecomacer'' *'' Nannomacer'' *'' Notomacer'' *'' Pagomacer'' *''
Rhinorhynchus ''Rhinorhynchus'' is a weevil genus. References External links * Weevil genera {{Weevil-stub ...
'' *'' Rhynchitomacer'' *'' Rhynchitomacerinus'' *'' Rhynchitoplesius'' *'' Stenomacer'' *'' Zimmiellus''


Extinct Taxa

*'' Kuschelomacer''Riedel, A. (2010). A new tribe, genus and species of Nemonychidae from Baltic amber (Coleoptera: Curculionoidea: Nemonychidae: Cimberidinae). ''Insect Systematics & Evolution'', 41, 29–38. *†subfamily Brenthorrhininae Arnoldi 1977 **†tribe Brenthorrhinini Arnoldi 1977 ***†subtribe Brenthorrhinina Arnoldi 1977 ****†'' Abrenthorrhinus'' Legalov 2009
Karabastau Formation The Karabastau Formation ( kk, Qarabastaý svıtasy) is a geological formation and lagerstätte in the Karatau Mountains of southern Kazakhstan whose strata date to the Middle to Late Jurassic. It is an important locality for insect fossils that ...
, Kazakhstan,
Callovian In the geologic timescale, the Callovian is an age and stage in the Middle Jurassic, lasting between 166.1 ± 4.0 Ma (million years ago) and 163.5 ± 4.0 Ma. It is the last stage of the Middle Jurassic, following the Bathonian and preceding the ...
/ Oxfordian ****†'' Brenthorrhinus'' Arnoldi 1977 Karabastau Formation, Kazakhstan, Callovian/Oxfordian ****†'' Gobibrenthorrhinus'' Gratshev and Legalov 2009 Ulugei Formation, Mongolia,
Tithonian In the geological timescale, the Tithonian is the latest age of the Late Jurassic Epoch and the uppermost stage of the Upper Jurassic Series. It spans the time between 152.1 ± 4 Ma and 145.0 ± 4 Ma (million years ago). It is preceded by ...
***†subtribe Brenthorrhinoidina Legalov 2003 ****†'' Brenthorrhinoides'' Gratshev and Zherikhin 1995 Karabastau Formation, Kazakhstan, Callovian/Oxfordian **†tribe Distenorrhinini Arnoldi 1977 ***†'' Buryatnemonyx'' Legalov 2010 Khasurty locality, Russia,
Aptian The Aptian is an age in the geologic timescale or a stage in the stratigraphic column. It is a subdivision of the Early or Lower Cretaceous Epoch or Series and encompasses the time from 121.4 ± 1.0 Ma to 113.0 ± 1.0 Ma (million years ag ...
***†'' Distenorrhinus'' Arnoldi 1977 Karabastau Formation, Kazakhstan, Callovian/Oxfordian,
La Pedrera de Rúbies Formation The La Pedrera de Rúbies Formation is an Early Cretaceous ( late Berriasian to early Barremian geologic formation in Catalonia, Spain. The formation crops out in the area of the Montsec in the Organyà Basin. At the La Pedrera de Meià loc ...
, Las Hoyas, Spain,
Barremian The Barremian is an age in the geologic timescale (or a chronostratigraphic stage) between 129.4 ± 1.5 Ma (million years ago) and 121.4 ± 1.0 Ma). It is a subdivision of the Early Cretaceous Epoch (or Lower Cretaceous Series). It is preceded ...
Khasurty locality, Russia, Aptian ***†'' Megabrenthorrhinus'' Gratshev and Zherikhin 1995 Karabastau Formation, Kazakhstan, Callovian/Oxfordian ***†'' Microbrenthorrhinus'' Gratshev and Zherikhin 2000 La Pedrera de Rúbies Formation, Spain, Barremian ***†'' Talbragarus'' Oberprieler and Oberprieler 2012 Talbragar Fossil bed, Australia, Tithonian **†tribe Eccoptarthrini Arnoldi 1977 ***†'' Astenorrhinus'' Gratshev and Zherikhin 1995 Karabastau Formation, Kazakhstan, Callovian/Oxfordian ***†'' Cratonemonyx'' Legalov 2014
Crato Formation The Crato Formation is a geologic formation of Early Cretaceous (Aptian) age in northeastern Brazil's Araripe Basin. It is an important Lagerstätte (undisturbed fossil accumulation) for palaeontologists. The strata were laid down mostly during ...
, Brazil, Aptian ***†'' Eccoptarthrus'' Arnoldi 1977 Karabastau Formation, Kazakhstan, Callovian/Oxfordian ***†'' Procurculio'' Arnoldi 1977 Karabastau Formation, Kazakhstan, Callovian/Oxfordian *†subfamily Cretonemonychinae Gratshev and Legalov 2009 **†tribe Cretonemonychini Gratshev and Legalov 2009 ***†'' Cretonemonyx'' Gratshev and Legalov 2009
Zaza Formation The Zaza Formation is a geological formation located in Buryatia (Russia). It dates to the Lower Cretaceous period. It is Aptian in age and consists of sandstones, siltstones, marls and bituminous shales, deposited in a stratified lake. It is s ...
, Russia, Aptian ***†'' Pseudonemonyx'' Gratshev and Legalov 2009 Zaza Formation, Russia, Aptian ***†'' Turononemonyx'' Legalov 2014 Kzyl-Zhar, Kazakhstan,
Turonian The Turonian is, in the ICS' geologic timescale, the second age in the Late Cretaceous Epoch, or a stage in the Upper Cretaceous Series. It spans the time between 93.9 ± 0.8 Ma and 89.8 ± 1 Ma (million years ago). The Turonian is preceded b ...
**†tribe Eocaenonemonychini Legalov 2013 ***†'' Eocaenonemonyx'' Legalov 2013
Green River Formation The Green River Formation is an Eocene geologic formation that records the sedimentation in a group of intermountain lakes in three basins along the present-day Green River in Colorado, Wyoming, and Utah. The sediments are deposited in very f ...
, United States,
Eocene The Eocene ( ) Epoch is a geological epoch that lasted from about 56 to 33.9 million years ago (mya). It is the second epoch of the Paleogene Period in the modern Cenozoic Era. The name ''Eocene'' comes from the Ancient Greek (''ēṓs'', ...
***†"''Eugnamptus" decemsatus'' Scudder 1878 Green River Formation, United States, Eocene ***†"''Sitona" grandaevus'' Scudder 1876 Green River Formation, United States, Eocene *†subfamily Eobelinae Arnoldi 1977 **†tribe Eobelini Arnoldi 1977 ***†'' Archaeorrhynchoides'' Legalov 2009 Karabastau Formation, Kazakhstan, Callovian/Oxfordian ***†'' Archaeorrhynchus'' Martynov 1926 Karabastau Formation, Kazakhstan, Callovian/Oxfordian ***†'' Eobelus'' Arnoldi 1977 Karabastau Formation, Kazakhstan, Callovian/Oxfordian ***†'' Martynovirhynchus'' Legalov 2010 Karabastau Formation, Kazakhstan, Callovian/Oxfordian **†tribe Karataucarini Legalov 2009 ***†'' Ampliceps'' Arnoldi 1977 Karabastau Formation, Kazakhstan, Callovian/Oxfordian **†tribe Oxycorynoidini Arnoldi 1977 ***†'' Oxycorynoides'' Arnoldi 1977 Karabastau Formation, Kazakhstan, Callovian/Oxfordian
Weald Clay Weald Clay or the Weald Clay Formation is a Lower Cretaceous sedimentary rock unit underlying areas of South East England, between the North and South Downs, in an area called the Weald Basin. It is the uppermost unit of the Wealden Group of ...
, United Kingdom, Barremian Gurvan-Eren Formation, Mongolia, Aptian ***†'' Microprobelus'' Liu et al. 2006
Yixian Formation The Yixian Formation (; formerly transcribed as Yihsien Formation) is a geological formation in Jinzhou, Liaoning, People's Republic of China, that spans the late Barremian and early Aptian stages of the Early Cretaceous. It is known for its exq ...
, China, Aptian ***†'' Khetoxycorynoides'' Legalov 2011 Emanra Formation, Russia, Turonian ***†'' Cratomacer'' Zherikhin and Gratshev 2004 Crato Formation, Brazil, Aptian **†tribe Probelini Legalov 2009 ***†'' Belonotaris'' Arnoldi 1977 Karabastau Formation, Kazakhstan, Callovian/Oxfordian ***†'' Probelus'' Arnoldi 1977 Karabastau Formation, Kazakhstan, Callovian/Oxfordian **''Incertae sedis'' ***†'' Longidorsum'' Zhang 1997 Dalazi Formation, China, Aptian * †subfamily Paleocartinae Legalov 2003 ** †tribe Metrioxenoidini Legalov 2009 *** †'' Brasilnemonyx'' Legalov 2009 Crato Formation, Brazil, Aptian *** †'' Cretoxenoides'' Legalov 2010 Huhtyk Formation, Mongolia,
Hauterivian The Hauterivian is, in the geologic timescale, an age in the Early Cretaceous Epoch or a stage in the Lower Cretaceous Series. It spans the time between 132.9 ± 2 Ma and 129.4 ± 1.5 Ma (million years ago). The Hauterivian is preceded by th ...
*** †'' Khetanamonyx'' Legalov 2009 Emanra Formation, Russia, Turonian *** †'' Megametrioxenoides'' Gratshev and Legalov 2009
Tsagaantsav Formation The Tsagaantsav Formation, Tsagantsab Formation or Tsagan-Tsab Formation (Russian: Tsagaantsav Svita) is an Early Cretaceous (Hauterivian to Barremian) geologic formation in Mongolia.Valanginian In the geologic timescale, the Valanginian is an age or stage of the Early or Lower Cretaceous. It spans between 139.8 ± 3.0 Ma and 132.9 ± 2.0 Ma (million years ago). The Valanginian Stage succeeds the Berriasian Stage of the Lower Cretace ...
*** †'' Metrioxenoides'' Gratshev et al. 1998
Lulworth Formation The Lulworth Formation is a geologic formation in England. It dates from the late Tithonian to the mid Berriasian. It is a subunit of the Purbeck Group. In Dorset, it consists of three members, which are in ascending order, the Mupe Member, the ...
, United Kingdom,
Berriasian In the geological timescale, the Berriasian is an age/stage of the Early/Lower Cretaceous. It is the oldest subdivision in the entire Cretaceous. It has been taken to span the time between 145.0 ± 4.0 Ma and 139.8 ± 3.0 Ma (million years ag ...
** †tribe Paleocartini Legalov 2003 *** †subtribe Nebrenthorrhinina Legalov 2007 **** †'' Nebrenthorrhinus'' Legalov 2003 La Pedrera de Rúbies Formation, Spain, Barremian *** †subtribe Paleocartina Legalov 2003 **** †'' Paleocartus'' Legalov 2003 Karabastau Formation, Kazakhstan, Callovian/Oxfordian ** †tribe Selengarhynchini Gratshev and Legalov 2009 *** †'' Selengarhynchoides'' Legalov 2010 Sharin-Gol Formation, Mongolia, Barremian *** †'' Selengarhynchus'' Gratshev and Legalov 2009 Sharin-Gol Formation, Mongolia, Barremian *Subfamily Rhinorhynchinae Voss 1922 **Tribe Mecomacerini Kuschel 1994 ***†'' Burmomacer'' Legalov 2018
Burmese amber Burmese amber, also known as Burmite or Kachin amber, is amber from the Hukawng Valley in northern Myanmar. The amber is dated to around 100 million years ago, during the latest Albian to earliest Cenomanian ages of the mid-Cretaceous period. The ...
, Myanmar,
Cenomanian The Cenomanian is, in the ICS' geological timescale, the oldest or earliest age of the Late Cretaceous Epoch or the lowest stage of the Upper Cretaceous Series. An age is a unit of geochronology; it is a unit of time; the stage is a unit in ...
***†'' Burmonyx'' Davis and Engel 2014 Burmese amber, Myanmar, Cenomanian ***†'' Guillermorhinus'' Clarke and Oberprieler 2018 Burmese amber, Myanmar, Cenomanian ***†'' Renicimberis'' Legalov 2009 Yixian Formation, China, Aptian ****


References


External links


Images of Nemonychidae species in New Zealand
{{DEFAULTSORT:Nemonychidae Weevils Beetle families