Pyroraptor Olympius. Only a few bones have been found of this species after a forrest fire in the Provence/South France.
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13. 10. 2005 - Sebastián Apesteguía, Federico Agnolín Novas and Peter Makovicky discover the remains of Buitreraptor gonzalezorum in the sandstones of La Buitrera, Rio Negro, in the north-west of Patagonia, Argentina. The new species displays characters also known from Troodontidae and Aves. It also is remarkable for it's completely unserrated teeth!
2. 12. 2005 - A new specimen of Archaeopteryx has surfaced from a private collection and become available for research. Several characters, which were not well visible in previous known Archaeopteryx-Fossils or not well preserved, are clearly visible in the "new" excellently preserved specimen . As did the Deinonychosauria, Archaeopteryx possessed an enlarged hyperextendable second pedal ungual (claw on the 2nd toe) and the hallux (1st toe) was not opposable to the other toes. While the former is yet further proove that our modern birds are truly theropods, the latter points strongly towards Archaeopteryx never spent as much time in trees as many thought it would have (thus strengthening the "grounds up" - hypothesis concerning the evolution of powered flight)!
Introduction
Dromaeosauridae
Troodontidae
Microraptoria
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The first step in order to understand the importance of the Deinonychosauria for palaeontology in general is to understand the relationships between the different species. This cladogramm done by Michael Mortimer explains these relations very nicely (comments in brackets ( ) explain scientifical language):

Format:

Alpha
|--Beta
`--Gamma
   |--Delta
   |*-Epsilon
   `--Zeta
      |?-Eta
      `--Theta 
Beta and Gamma are sister taxa (Species) within the clade (group) Alpha. Delta is within Gamma, but not a member of Zeta. Epsilon, however, is Gamma incertae sedis (uncertain position). Eta is only tentatively placed within Zeta. Nomina nuda ("Naked name" species description considered invalid because either the specimen/s it was based on was/were lost or the material was considered inadequate) are non-italicized and placed in quotation marks, while unpublished taxa [as recognized by the ICZN] are designated the same way, but followed by an asterisk. Nomina dubia (Species "in doubt" meaning it's not for certain, wether this actually is a valid species) are not distinguished from valid taxa, as which taxa are indeterminate is a subjective question.

Theropoda
|
Avepoda
Averostra
Neotheropoda
|
Ceratosauroidea
|
Tetanurae
|
Avetheropoda
|
Coelurosauria
|
Avipluma
Tyrannoraptora
|
Metatheropoda
|
Maniraptoriformes
|
Maniraptora
|
Paraves
Eumaniraptora
|
|--Deinonychosauria                                       
|  Dromaeosauridae
|  |--Microraptoria
|  |  |--Graciliraptor lujiatunensis
|  |  |--Sinornithosaurus millenii
|  |  `--+--Cryptovolans pauli
|  |     |--Microraptor gui
|  |     `--Microraptor zhaoianus
|  |--Bambiraptor feinbergi
|  |*?"Airakoraptor"
|  |*-"Dromaeosaurus" gracilis
|  |*?"Ichabodcraniosaurus"
|  |*-Itemirus medullaris
|  |*-"Laelaps" explanatus
|  `--+--Velociraptorinae                                                                  
|     |  `--Velociraptor mongoliensis
|     |?-Saurornitholestes langstoni                                                       
|     |*-"Koreanosaurus koreanensis"
|     |*-Ornithodesmus cluniculus
|     |*-Pyroraptor olympius
|     |*-Variraptor mechinorum
|     `--Dromaeosaurinae
|        |--Deinonychus antirrhopus
|        `--+--Atrociraptor marshalli
|           |?-Dromaeosauroides bornholmensis
|           `--+--Dromaeosaurus albertensis
|              |?-Adasaurus mongoliensis
|              |--Achillobator giganticus
|              `--Utahraptor ostrommaysorum
|--Troodontidae
|  |*-Yaverlandia bitholus
|  |--Mei long
|  `--+--Sinovenator changiae
|     |--Jinfengopteryx elegans
|     `--+--Sinusonasus magnodens
|        |--Koparion douglassi                                                             
|        |*?"Ornithomimus" tenuis
|        `--+--Byronosaurus jaffei
|           `--+--Sinornithoides youngi
|              `--+*-Borogovia gracilicrus
|                 |*-Saurornithoides? asiamericanus
|                 |*-Saurornithoides? isfarensis
|                 |*-Tochisaurus nemegtensis
|                 |--Troodon formosus
|                 `--+--Saurornithoides mongoliensis
|                    `--Saurornithoides junior
`--Avialae

The main informations we can get out of this cladogramm are the following:
1. Deinonychosauria were a sister group to birds. More so were the Troodontidae.
2. Deinonychosauria (and Troodontidae) represent a group of highly specialized, "advanced" animals.
3. Deinonychosauria shared a common ancestor with the Avialae (birds) and the Troodontidae which explains why they were so bird-like.

Distribution: Fossil remains of Deinonychosauria (including Troodontidae) have been described from all over the world.

Timeline: The following table shows when the different species lived and who described them ("correctly" - according to present knowledge) for the first time.

Species nameAuthor/sDescribed inLocationTime period
Troodontidae
Sinovenator changiiXu, Norell, Wang, Makovicky & Wu2002Lujiatun Beds of Yixian Formation, Liaoning, ChinaHauteverian, Early Cretaceous
Koparion douglassiChure1994Brushy Basin Member of the Morrison Formation, Utah, U.S.Tithonian, Late Jurassic
Saurornithoides asiamericanusNessov / Olshevsky1985 / 1991Khodzhakul Formation, Sheykhdzeyli, UzbekistanEarly Cenomanian, Late Cretaceous
Saurornithoides isfarensisNessov / Olshevsky1995 / 2000Yalovach Formation, Kyzyl-pilyal, TadhzikistanEarly Santonian, Late Cretaceous
Sinornithoides youngiRussell & Dong1994Ejinhoro Formation, Inner Mongolia; Xinminbao Group, Gansu, ChinaAlbian, Early Cretaceous
Borogovia gracilicrusOsmolska1987Nemegt Formation, MongoliaLate Campanian - Early Maastrichtian, Late Cretaceous
Tochisaurus nemegtensisKurzanov & Osmolska1991Nemegt Formation, MongoliaLate Campanian - Early Maastrichtian, Late Cretaceous
Troodon formosusLeidy1856Dinosaur Park Formation, Oldman Formation, Two Medicine Formation, Alberta, Canada; Prince Creek Formation, Alaska, Judith River Group, Upper Two Medicine Formation, Montana, Fruitland Formation, Kirtland Formation, Utah, U.S.Late Campanian - Early Maastrichtian, Late Cretaceous
Ornithomimus teniusMarsh1890Judith River Formation, Montana, U.S.Late Campanian, Late Cretaceous
Jinfengopteryx elegansQiang, Shu'an, Junchang, Hailu, Wen, Yongqing & Yanxue2005Qiaotu Formation, Hebei, ChinaLate Jurassic - Early Cretaceous
Byronosaurus jaffeiNorell, Makovicky & Clark2000Ukhaa Tolgod, MongoliaLate Cretaceous
Mei longXing Xu & Mark A. Norell2004Lujiatun, western Liaoning, ChinaBerreasian - Hauteverain, Early Cretaceous
Microraptoria
Microraptor zhaoianusXu, Zhou & Wang2000Yixian Formation, Liaoning, ChinaBarremian, Early Cretaceous
Microraptor guiXu, Zhou, Wang, Kuang, Zhang & Du2003Jiufotang Formation, Liaoning, ChinaEarly Aptian, Early Cretaceous
Cryptovolans pauliCzerkas, Zhang, Li & Li2002Jiufotang Formation, Liaoning, ChinaEarly Aptian, Early Cretaceous
Sinornithosaurus MilleniiXu, Wang & Wu1999Jianshangu Member of Yixian Formation, Liaoning, ChinaMiddle Barremian, Early Cretaceous
Graciliraptor lujiatonensisXu & Wang2004Yixian Formation, Liaoning, ChinaHauterivian, Early Cretaceous
Dromaeosauridae
Bambiraptor feinbergiBurnham, Derstler, Currie, Bakker, Zhou & Ostrom2000Upper Two Medicine Formation, Montana, U.S.Campanian, Late Cretaceous
Variraptor mechinorumLe Loeff & Buffetaut1998Gres a Reptiles Formation, FranceLate Campanian - Early Maastrichtian, Late Cretaceous
Pyroraptor olympiusAllain & Taquet2000La Boucharde, Bouches-du-Rhone, FranceLate Campanian - Early Maastrichtian, Late Cretaceous
Ornithodesmus cluniculusSeeley1887Upper Weald Clay, EnglandBarremian, Early Cretaceous
Dromaeosaurus albertensisMatthew & Brown1922Dinosaur Park Formation, Foremost Formation, Oldman Formation, Alberta, Canada; Prince Creek Formation, Alaska, Judith River Group, Lower Two Medicine Formation, Montana, U.S.Late Campanian - Maastrichtian, Late Cretaceous
Dromaeosauroides bornholmensisChristiansen & Bonde2003Jydegaard Formation, DenmarkLate Berriasian, Early Cretaceous
Deinonychus antirrhopusOstrom1969Unknown Formation, Arizona, Arundel Formation, Maryland, Cloverly Formation, Montana, Antlers Formation, Oklahoma, Trinity Group, Texas, middle Cedar Mountain Formation, Utah, U.S.Aptian - Albian, Early Cretaceous
Saurornitholestes langstoniSues1978Dinosaur Park Formation, Foremost Formation, Milk River Formation, Oldman Formation, Two Medicine Formation, Alberta, Canada; Prince Creek Formation, Alaska, Judith River Group, Lower Two Medicine Formation, Montana, Menefee Formation, New Mexico, U.S.Early Campanian - Maastrichtian, Late Cretaceous
Velociraptor mongoliensisOsborn1924Barun Goyot Formation, Djadochta Formation, MongoliaLate Santonian - Early Campanian, Late Cretaceous
IchabodcraniosaurusNovacek1996Djadochta Formation, MongoliaCampanian, Late Cretaceous
AirakoraptorPerle, Norell & Clark1999MongoliaLate Cretaceous
Adasaurus mongoliensisBarsbold1983Nemegt Formation, MongoliaMiddle Maastrichtian, Late Cretaceous
Achillobator giganticusPerle, Norell & Clark1999Bayan Shireh Formation, MongoliaSantonian - Campanian, Late Cretaceous
Utahraptor ostrommaysorumKirkland, Gaston & Burge1993Yellow Cat Member of Cedar Mountain Formation, Utah, U.S.Barremian, Early Cretaceous
Neuquenraptor argentinusNovas & Pol2005Portezuelo Formation, Neuquen Province, ArgentinaConiacian, Early Cretaceous
Unnamed dromaeosaur*Rauhut & Werner1995Wadi Milk Formation, SudanCenomanian, Late Cretaceous
* = this specimen was added in order to illustrate the presence of dromaeosaurids on the African continent.

Besides the fossil material that was used to describe and name the species listed above, there still exists plenty of undescribed and unnamed fossil material. Some of these fossils belong to the Troodontidae and Dromaeosauridae and mostly consist of teeth. The time periods these unnamed and undescribed fossils belong to range from the late Jurassic to the late Cretaceous time. All this data so far available allows to conclude that Deinonychosauria were present from the late Jurassic until the end of the Cretaceous time. This means they were around for an impressive 85 million years which underlines the success of the group as such!

The following table gives a good oversight throughout what timespan Deinonychosauria and Troodontidae were actually present on our planet. It covers only those periods during which Deinonychosauria or Troodontidae were present. The Mesozoic era covers also the Triassic period and those parts of the Jurassic which are actually not displayed in this table. The Titonian age began about 150,7 million years ago.

The period of time during which the Deinonychosauria were present on earth. Age estimates are in millions of years.
EraPeriodEpochAgeEnd
MesozoicCretaceousLateSenonianMaastrichtian65
Campanian71
Santonian83,5
Coniacian85,8
GallicTuronian89,9
Cenomanian93,5
EarlyAlbian98,9
Aptian112,2
Barremian121
NeocomianHauterivian127
Valanginian132
Berriasian137
JurassicLateMalmTitonian144,2