ライフサイエンスコーパス: Carboniferous

1 various insect lineages in the Devonian and Carboniferous.

2 y complete dearth of material from the Early Carboniferous.

3 cular plants and forests in the Devonian and Carboniferous.

4 d in angiosperms had already diverged by the Carboniferous.

5 le/Late Devonian boundary, and in the latest Carboniferous.

6 Devonian and continuing through to the late Carboniferous.

7 f a high atmospheric O(2) content during the Carboniferous (300 million years ago), a time when insec

8 arth history was punctuated during the Permo-Carboniferous [300-250 million years (Myr) ago] by the l

9 Quantitative calibration of Late Carboniferous (330-300 Myr ago) and Permian (270-260 Myr

10 By the Late Carboniferous a diversity of flying lineages is known, m

11 itumen clast in a glacial diamictite of late Carboniferous age (c. 303 Ma) from eastern Oman.

12 CO(2) impoverished atmospheres of the Permo-Carboniferous and Cenozoic glaciations.

13 n between these two states begins during the Carboniferous and concludes approximately around the Tri

14 was formed from plant debris during the late Carboniferous and early Permian periods.

15 ncreased, hyperoxia, as occurred during late Carboniferous and early Permian, may have facilitated th

16 ous groups of temnospondyl amphibians of the Carboniferous and Permian periods, including the dissoro

17 with wingspans as large as 70 cm, ruled the Carboniferous and Permian skies.

18 d of arborsecent lycopsids of the equatorial Carboniferous and Permian swamp communities.

19 ula: see text]150 and 700 ppm for the latest Carboniferous and very low values of 100 [Formula: see t

20 ricomycetes may have been present before the Carboniferous, and lignin degradation was likely never r

21 aphy to describe two new harvestmen from the Carboniferous ( approximately 305 Myr) of France.

22 arked rise to approximately 35% in the Permo-Carboniferous, around 300 million years before present,

23 some 15 million years later at the Devonian-Carboniferous boundary (359 Ma).

24 ation among ray-fins centred on the Devonian-Carboniferous boundary.

25 Furthermore, a large proportion of Carboniferous coal horizons are dominated by unlignified

26 s called coal balls [2], which formed in the Carboniferous coal swamp forests over 300 million years

27 p to 50 m in height, were the tallest in the Carboniferous coal swamp forests.

28 cological change, quantitative counts of 847 Carboniferous-Cretaceous collections from the Paleobiolo

29 Middle Carboniferous deposition occurred in a shelf environment

30 he feet of later, more terrestrially adapted Carboniferous forms.

31 Low CO(2) levels during the Permo-Carboniferous glaciation are in agreement with glaciolog

32 The Upper Carboniferous Hamilton Formation (300 Myr) in Kansas, US

33 Here we report a Carboniferous harvestman species, Hastocularis argusgen.

34 ing from Early Ordovician (Late Tremadoc) to Carboniferous, have proved no less enigmatic.

35 rvals that sum to 300 Myr (Middle Ordovician-Carboniferous; Late Jurassic-Paleogene).

36 moradiensis gen. et sp. nov., as relicts of Carboniferous lineages that diverged 40-90 million years

37 High oxygen concentrations during the Carboniferous may have alleviated these physical constra

38 , a large soft-bodied organism from the late Carboniferous Mazon Creek biota (approximately 309-307 m

39 ium is an iconic soft-bodied fossil from the Carboniferous Mazon Creek Lagerstatte (Illinois, USA).

40 he wings of archaic Odonatoidea from the mid-Carboniferous of Argentina show features analogous to "s

41 f Jaekelocarpus oklahomensis, from the Upper Carboniferous of Oklahoma, USA, which, being externally

42 cial information from the wing pad joints of Carboniferous palaeodictyopteran insect nymphs using cla

43 strial carbon cycle model forced with a late Carboniferous paleoclimate simulation to evaluate the ef

44 Donbas segment (Ukraine) exposes the middle Carboniferous part of the basin's stratigraphy.

45 al-fired steam ships), and lead derived from Carboniferous Pb-Zn mineralization (mining activities).

46 in Earth's history occurred during the Late Carboniferous (Pennsylvanian) and Permian Periods (ca. 3

47 currence of insect herbivory during the Late Carboniferous (Pennsylvanian) has been questioned, we pr

48 Aggregated pairs dominated from the Carboniferous period (307 million years ago) to the earl

49 ere broadly similar to today during the Late Carboniferous period (314-300 Myr ago), when carbon diox

50 A new articulated specimen from the Carboniferous period (about 335 Myr bp) of Indiana revea

51 The Carboniferous Period of the Paleozoic is so named for ma

52 million years ago), but decreased during the Carboniferous period to concentrations similar to that o

53 Devonian and subsequently diversified in the Carboniferous period, they possessed substantially highe

54 mpression fossils and in coal balls from the Carboniferous period.

55 organic carbon burial around the end of the Carboniferous period.

56 from the Devonian period and mid-late Early Carboniferous period.

57 y placed in the group Mitrata (Ordovician to Carboniferous periods, 530-280 million years ago), by co

58 e and following the reverse polarity Kiaman (Carboniferous-Permian) and Moyero (Ordovician) superchro

59 re the sensitivity of the climate around the Carboniferous/Permian boundary to changes in Earth's orb

60 Studies of nearest living relatives of key Carboniferous plants suggest that their physiologies and

61 This integrated approach indicates that key Carboniferous plants were capable of growth and transpir

62 d as main event that triggered the huge post-Carboniferous radiation of hemipterans, and facilitated

63 ecular divergence time estimates, supporting Carboniferous rather than Devonian diversification for e

64 at a rise in pO(2) from 21 to 35% during the Carboniferous reduced global terrestrial primary product

65 undary, indicating a prolonged response to a Carboniferous rise in O2.

66 From this analysis, we deduce that a Permo-Carboniferous rise in pO(2) was unlikely to have exerted

67 A Carboniferous root apex reiterates the importance of the

68 have found Class I (polylabdanoid) amber in Carboniferous sediments dating to approximately 320 mill

69 ly growing root meristem from permineralized Carboniferous soil with detail of the stem cells and dif

70 This suggests that the middle Carboniferous stratigraphy of the Dniepr-Donets basin to

71 vity and magnetic maps indicate that the pre-Carboniferous Tasmanides in southeastern Australia may h

72 ave hitherto separated Late Devonian and mid-Carboniferous tetrapod faunas.

73 1347 1348 1348 References 1348 The Carboniferous, the time of Earth's penultimate icehouse

74 have colonized fresh water in Pangaea during Carboniferous times.

75 Echinoderms from the Cambrian and from the Carboniferous to the Triassic indicate a seawater Mg/Ca

76 ring the early evolution of Amniota from the Carboniferous to the Triassic, subjecting a new supertre

77 ppian temporal gap ranging from the earliest Carboniferous (Tournaisian and early Visean) to the mid-

78 impression of a flying insect from the Late Carboniferous Wamsutta Formation of Massachusetts, repre