| 词条 | Incognitoolithus |
| 释义 |
|fossil_range = {{fossil range|56|47.8|Early Eocene}} |taxon = Incognitoolithus |authority = |subdivision_ranks = Oospecies |subdivision =
}}Incognitoolithus is an oogenus of medioolithid fossil bird egg. It is notable for bearing evidence of predation, possibly from a bird pecking the eggshell.[1] DistributionIncognitoolithus fragments are found at two localities in the DeBeque Formation in Garfield County, Colorado. Both localities are dated to the Early Eocene.[1]HistoryEggshell fragments of Incognitoolithus were discovered in 1977 and 1979 during two separate field seasons. The oospecies I. ramotubulus was first described in 1997 by Karl Hirsch, Allen Kihm and Darla Zelenitsky.[1] DescriptionI. ramotubulus is known from over 200 eggshell fragments which may represent a single disintegrated egg. When complete, the egg is estimated to have been {{convert|10|-|12|cm|in|abbr=on}} long and {{convert|7.5|-|9|cm|in|abbr=on}}, making it significantly larger than the next largest known Eocene bird egg in North America, which measured only 6.4 x 8.9 cm. The eggshell is 1.27–1.43 mm thick and consists of two structural layers, unlike most modern ratite eggs (which have a third layer, the external layer). The outer layer, called the continuous layer, is three times the thickness of the inner layer (the mammillary layer).[1] It is one of the few fossil eggs to have only two layers and a smooth eggshell.[2]Incognitoolithus has a distinctive pore system. It has both branching and unbranching pores. The openings of these pores on the surface of the eggshell matches the "aepyornithid" type: Pores open in small pits or in grooves which may accommodate multiple pore openings.[1]PaleobiologyParentageThe pore arrangement and structure of Incognitoolithus is similar to that of Aepyornis.[3] The microstructure and lack of ornamentation are similar to modern ratite eggs. However, since no embryonic remains or parental remains were found with Incognitoolithus, it is impossible to infer what kind of bird laid the eggs.[1] PredationMultiple fragments of Incognitoolithus have been found with holes interpreted as peck marks. While it is possible that these were made by a parent assisting the hatching, this behavior is very rare in modern birds. More likely, they are the result of predation. Experiments on modern chicken eggs by Hirsch et al. in 1997 found that Incognitoolithus{{'s}} holes are most consistent with those from a bird's peck. However, the dynamics of a thick eggshell like I. ramotubulus differ from those of chicken eggs, so the possibility that the holes are tooth marks of a mammal or reptile cannot be ruled out.[1] See also{{Portal|Dinosaurs|Paleontology|||}}
References1. ^1 2 3 4 5 6 {{cite journal|last1=Hirsch|first1=Karl|last2=Kihm|first2=Allen|last3=Zelenitsky|first3=Darla|title=New Eggshell of Ratite Morphotype with Predation Marks from the Eocene of Colorado|journal=Journal of Vertebrate Paleontology|date=1997|volume=17|issue=2|pages=360–369|jstor=4523812|doi=10.1080/02724634.1997.10010980}} 2. ^{{cite journal |last1=Tanaka |first1=Kohei |last2=Zelenitsky |first2=Darla |last3=Saegusa |first3=Haruo |last4=Ikeda |first4=Tadahiro |last5=DeBuhr |first5=Christopher |last6=Therrien |first6=François |title=Dinosaur eggshell assemblage from Japan reveals unknown diversity of small theropods|journal=Cretaceous Research |date=2016 |volume=57 |pages=350–363 |doi=10.1016/j.cretres.2015.06.002}} 3. ^{{cite journal|last1=Bibi|first1=Faysal|last2=Shabel|first2=Alan|last3=Kraatz|first3=Brian|last4=Stidham|first4=Thomas|title=New fossil ratite (Aves: Palaeognathae) eggshell discoveries from the Late Miocene Baynunah Formation of the United Arab Emirates, Arabian Peninsula.|journal=Palaeontologia Electronica|date=2006|volume=9|issue=1|page=2A}} 3 : Bird breeding|Fossil parataxa described in 1997|Paleogene birds of North America |
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