a beautiful super rare (only 4 in the entire Fossil Record) Termitaphidid or Termite Bug
in an authentic Dominican Amber Gemstone
excavated in the La Toca amber mine in late Autumn of 2008
examined by paleoentomologists at the American Museum of Natural History
DR8938
$3,7
50.00 No Reserve


a beautiful super rare (only 4 in the entire Fossil Record) Termitaphidid or Termite Bug
in an authentic Dominican Amber Gemstone
excavated in the La Toca amber mine in late Autumn of 2008
examined by paleoentomologists at the American Museum of Natural History
DR8938
$67
50.00 No Reserve

Some photos of our amber excavations in August 2007 at La Toca and La Bucara amber mines









Description
This is a beautiful super rare (only 4 in the entire Fossil Record) Termitaphidid or Termite Bug in an authentic Dominican Amber Gemstone excavated in the La Toca amber mine in late Autumn of 2008. Examined by paleoentomologists at the American Museum of Natural History. This amber specimen amazingly also has a termite head inclusion right next to the Termitaphidid! as well as lots of termite frass.

No Termitaphidids are known in Baltic amber, Dr. Poinar published on a Termitaphidid in Mexican amber in 1992, Dr. Grimaldi and Dr. Engel published on the 1st known Termitaphidids in Dominican amber in June of 2008.

DR8938
$6,750.00 No Reserve


From Novitates June 2008 ..." The most remarkable observation is the presence of two T. avitinquilinus specimens preserved in an amber piece with a worker termite of Mastotermes electrodominicus Krishna and Grimaldi (Mastotermitidae) . It is highly likely that this termite represents the host of the fossil species given that termitaphidids occur in isolation from their associated termites probably very infrequently. In fact, the specimen from Mexican amber (Poinar and Doyen, 1992) was reported in a piece also containing two wingless termites (it was not mentioned whether these were dealates or workers, and the termite genus was not identified). Given the difficulty in locating modern termitaphidids (which may be easily overlooked) and the scarcity of data available for them, it has to be wondered whether additional, modern termitaphidid species will eventually be discovered in the nests of other families of termites. Thus far, no termitaphidids have been found in the nests of the most basal living termite, Mastotermes darwiniensis Froggatt from Australia (N. Lo, personal commun.), so if the association indeed no longer exists then the fossilized association represents a dramatically new one and raises questions regarding the fidelity of termitaphidids with ‘‘higher’’ termite hosts. Poinar and Doyen (1992) hypothesized that the termitaphidids were ancient and predate the breakup of Pangaea 175 Ma. The rationale for an estimate of such antiquity is based on what appears to be the extremely limited vagility of these bugs, but yet they are circumtropical, so their ancestral distribution was presumably fragmented by drifting continents. Most species of Termitaradus are known from Central and South America (guianae [Morrison], jamaicensis Myers, mexicanus [Silvestri], panamensis Meyers, and trinidadensis [Morrison]), but with one species each in India, Australia, and Africa (annandalei [Silvestri], australiensis [Mjo¨ rberg], and subafra Silvestri, respectively). Despite such a distribution, we maintain that a pre-Pangaean existence of termitaphidids is completely unrealistic, and that their distribution can be dated almost certainly to a time 100 Ma or more younger than that posited by Poinar and Doyen. The Termitaphididae probably originated in the latest Cretaceous or Early Tertiary because, first, the Pentatomomorpha (to which the Aradoidea is the sister group) appears to have originated in either the latest Jurassic or earliest Cretaceous (Grimaldi and Engel, 2005). For example, the earliest and most primitive aradoid is Archaearadus burmensis Heiss and Grimaldi in mid-Cretaceous amber fromMyanmar (Heiss and Grimaldi, 2001), so it is inconceivable that such a specialized group of pentatomomorphans would far predate the age of the infraorder. Second, the earliest fossil termites occur in the Barremian (Engel et al., 2007a), and termites as a whole did not originate until the latest Jurassic or earliest Cretaceous (Grimaldi and Engel, 2005). Indeed, the higher termites, upon which modern termitaphidids specialize, did not radiate until the Tertiary (Grimaldi and Engel, 2005; Engel et al., 2007a, 2007b). All of this evidence suggests that diversification of Termitaphididae was largely Tertiary, and in such case their circumtropical distribution could be a result of dispersion during globally tropical and subtropical conditions during the Eocene, as is known for myriad other insect groups (Grimaldi and Engel, 2005).
Perhaps most significantly, there are indications that termitaphidids phylogenetically may be highly derived members of the Aradidae. Termitaphidids have the same uniquely modified maxillary and mandibular
stylets that are coiled within the head capsule that are characteristic of Aradidae (this is even seen in fossil M3515A, in which the external cuticle is translucent: fig. 3). Aradids have repeatedly become brachypterous and apterous, and in the subfamilies Mezirinae and Carventinae in particular many species are wholly apterous. Mezirinae and 8 AMERICAN MUSEUM NOVITATES NO. 3619 Termitaphididae also share the derived feature of a rostral base situated within a closed atrium (fig. 4C), although four mezirine genera have an open atrium (Chiastoplonia China, Daulocoris Usinger and Matsuda, Euchelonocoris Hoberlandt, and Pseudomezira
Heiss), and four Carventinae genera have a closed atrium (Apteraradus Drake, Libiocoris Kormilev, eocarventus Usinger and Matsuda, and Notoplocaptera Usinger and Matsuda). Also, the seventh abdominal ventrite in female termitaphidids and Mezirinae is divided into hemiventrites. Many mezirines have lateral lobes on the pronotum and/or abdomen that extend beyond the body, such as Chlonocoris Usinger and Matsuda, Dysodiellus Hoberlandt, Oroessa Usinger, and Matsuda, and Rossius Usinger and Matsuda (Usinger and Matsuda, 1959).
Many of these even have small setigerous tubercles on the dorsal surface of the body and the lateral margins, much like the lobules and marginal setae (e.g., fig. 5B) of termitaphidids. Furthermore, the arrangement of segments within tagmata of termitaphidids is essentially the same as that of apterous genera of Mezirinae and Carventinae (E. Heiss, personal commun., 2007). Lastly, the structure of the male genital capsules in some mezirines and in termitaphidids is similar. Circumstantial biological evidence for a termitaphidid-mezirine relationship lies in the fact that several mezirine aradids are apparently facultative inquilines in the colonies of termites, and one species (Aspisocorus termitophilus Kormilev, from southwest Australia) is morphologically specialized and thus appears to be an obligate inquiline in the nests of a ‘‘higher’’ termite, Occasitermes
occasus (Silvestri) (Isoptera: Termitidae: Nasutitermitinae) (Kormilev, 1967; Monteith, 1997). Aspisocoris has distinctively reduced compound eyes and hemelytra (such reduction is taken to an extreme in termitaphidids,
where they are lost altogether), pale coloration, and small size. Other putative termitophiles in Mezirinae are not morphologically specialized and have also been found away from termites under decaying bark. Interestingly, though, those facultative inquilines occur in the nests of primitive termites such as Zootermopsis (e.g., Mezira reducta Van Duzee) or Archotermopsis (e.g., Pseudomezira termitophila [Kormilev]), both of
the basal family Termopsidae. The presently documented hosts of modern termitaphidids are exclusively among the higher termites (Rhinotermitidae and Termitidae). Thus, the possibility should be considered that termitaphidids are highly specialized aradids, in or near the Mezirinae or Carventinae. In such a scenario, and with the exception of the fossilized host association we report here, the termite host associations of
modern aradioids roughly reflect a phylogenetic pattern: those mezirines (presumably basal to termitaphidids) facultatively occur in colonies of Termopsidae (one species obligately with a termitid), and the more derived and younger termitaphidids subsist in colonies of higher termites of the Rhinotermitidae and Termitidae. There is even divergence between the two main lineages of termitaphidids: Termitaphis is known from Termitidae, and
this genus is clearly the sister group to the more specialized, flattened, laminate, and monophyletic Termitaradus, which live with Rhinotermitidae. Unfortunately, the only phylogenetic hypotheses for Aradidae are slim and superficial, using only 15–25 characters and treating subfamilies as terminal taxa (Va´sa´ rhely,
1987; Grozeva and Kerzhner, 1992). The monophyly of these subfamilies cannot be assumed. So, confronting a putative mezirinetermitaphidid relationship must await a comprehensive phylogenetic analysis, but our
ignorance is far more profound that this. The last extant termitaphidid to have been described was by Myers (1932), even though vast expanses of forests from the Andean and Amazonian regions, the Congo Basin, and the
IndoPacific are unexplored. While it is intriguing to consider how such intimate symbiosis as that between termitaphidids and termites could be evolving for much of the Tertiary, even more fundamental is what
alliances have yet to be discovered.
"

This beautiful authentic Dominican Amber gemstone is offered here with a complete satisfaction guarantee, if you are not satisfied with your purchase you can return any specimen within 14 days for a full refund.

 
Dominican Amber 
In the Dominican Republic, Hymenaea trees are called Algorrobo. The Hymenaea tree exudes vast amounts of resin which over millions of years of pressure hardens into amber. Generally amber is found because a landslide along a steep slope in the mountains exposes veins of black lignite. If the lignite contains amber it is gradually extracted by digging along the vein with picks and shovels. After the amber is found it is chiseled by hand out of the shaft walls, put into burlap sacks and passed out of the mine where it is separated from the rock by machete. Larger chunks of amber make it possible to view inclusions almost immediately by holding the amber up to sunlight to determine if a large inclusion has been discovered. Fossil bearing amber is polished locally.To view photos and videos of our some of our amber excavations in the blue amber mines in mountains of the Dominican Republic and to see a small java applet of the amber mines click here - (opens in a new browser window).

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About Us
We have been collecting amber in the field and prepping rough fossil amber specimens since 1993. Photographs of our specimens have appeared in National Geographic, Nature, Science, Scientific American, Discover, Time, Newsweek, The New York Times and others. We have been featured in PaleoWorld's The Amber Hunters. We offer authentic museum quality Dominican Amber display specimens of rare insects in amber and also authentic rare Dominican rough unprepared amber for sale. Our collections include museum quality rare insects in amber, unusual botanicals and flowers in amber and also rough unprepared Dominican Amber gemstones. We have traveled many times to the Dominican Republic where we have chiseled beautiful amber gemstones out of the lignite layers deep in the amber mines north of Santiago. We have excavated in the Palo Quemado and Los CaCaos blue amber mines and also in La Nueva Toca and the world famous La Toca amber mines way up in the mountains north of Santiago. For many years we have extensively collected mid Cretaceous New Jersey amber in the Raritan formation of central New Jersey and have traveled many times to collect late Cretaceous and early Paleocene amber in the Hanna formation of eastern Wyoming. We have collected mid Cretaceous amber in the Black Creek formation of eastern North Carolina and we have spent weeks collecting mid Cretaceous amber in the northern most Tundra of Alaska. Some of our most recent collecting trips have been in October of 2003 to the western Aleutian Islands some 1000 miles west of Anchorage to explore and collect Miocene amber, August of 2004 and April of 2006 we were back in the Dominican Republic to collect Miocene amber from the Palo Quemado amber mines which have recently closed due to the miners finding little amber, we were back to the Dominican Republic in April of 2006 to video in the La Toca amber mines, and most recently in August of 2007 we excavated in La Toca and La Bucara. The La Toca amber mines had much water whereas on the other ridgeline the La Bucara amber mines were nearly dry! We collected much amber from both La Toca and La Bucara.
We have donated many hundreds of amber specimens to museums in the United States and have several dozen new species of insects in amber named after us. We have examined several thousand specimens of rough Burmese amber and have prepped many new Burmese fossil amber specimens. We have traveled to Europe with colleagues to examine unusual spectacular Dominican Amber specimens in private collections and we consider the amber curators of the museums in Santo Domingo, Puerto Plata and New York City our friends. Exploring for and collecting amber along with the examination and research of amber is our passion.
To view photos and videos of our some of our amber excavations in the amber mines in mountains of the Dominican Republic and to see a small java applet of the amber mines click here - (opens in a new browser window). Our amber comes direct from the Dominican Republic amber mines east of the world famous La Toca amber mine. These specimens do not go through any middle men, we acquire these specimens from the miners and mine owners directly at the amber mines.

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