Cenomanianadj.

/ˌsiːnəʊˈmeɪnɪən/

/ˌsɛnəʊˈmeɪnɪən/

Etymology: < French cénomanien, < medieval Latin Cenomania , now Le Mans, France, < Latin Cenomani , an ancient Gallic tribe of northern Italy: see -ian suffix.

Geology.

Designating a subdivision of the Upper Cretaceous period, corresponding to the Lower Chalk and Upper Greensand of British geologists; of flora, etc., belonging to or found in these strata.

ΘΚΠ

the world > plants > by habitat or distribution > [adjective] > characteristic of particular region or period

southerneOE

African1578

Asiatic1670

American1678

Creole1758

Californian1785

subalpine1808

Antarctic1835

Adelaidean1847

Arctic1876

Atlantic1876

gerontogeous1880

Cenomanian1902

Lusitanian1907

pantropic1911

pantropical1913

native1920

1882 A. Geikie Text-bk. Geol. 829 The Cenomanian formation consists in Hanover of earthy limestones and marls.

1902 Encycl. Brit. XXXI. 434/2 The Cenomanian flora of central Europe.

1914 Brit. Mus.: Return 206 in Parl. Papers (H.C. 186) LXXI. 193 The Cenomanian Chalk Marl of Cambridge.

1960 L. D. Stamp Britain's Struct. & Scenery (ed. 5) xii. 138 A great marine transgression..referred to as the ‘Cenomanian Transgression’.

This entry has not yet been fully updated (first published 1933; most recently modified version published online September 2018).

单词	cenomanian
释义	Cenomanianadj. /ˌsiːnəʊˈmeɪnɪən//ˌsɛnəʊˈmeɪnɪən/ Etymology: < French cénomanien, < medieval Latin Cenomania , now Le Mans, France, < Latin Cenomani , an ancient Gallic tribe of northern Italy: see -ian suffix. Geology. Designating a subdivision of the Upper Cretaceous period, corresponding to the Lower Chalk and Upper Greensand of British geologists; of flora, etc., belonging to or found in these strata. ΘΚΠ the world > plants > by habitat or distribution > [adjective] > characteristic of particular region or period southerneOE African1578 Asiatic1670 American1678 Creole1758 Californian1785 subalpine1808 Antarctic1835 Adelaidean1847 Arctic1876 Atlantic1876 gerontogeous1880 Cenomanian1902 Lusitanian1907 pantropic1911 pantropical1913 native1920 1882 A. Geikie Text-bk. Geol. 829 The Cenomanian formation consists in Hanover of earthy limestones and marls. 1902 Encycl. Brit. XXXI. 434/2 The Cenomanian flora of central Europe. 1914 Brit. Mus.: Return 206 in Parl. Papers (H.C. 186) LXXI. 193 The Cenomanian Chalk Marl of Cambridge. 1960 L. D. Stamp Britain's Struct. & Scenery (ed. 5) xii. 138 A great marine transgression..referred to as the ‘Cenomanian Transgression’. This entry has not yet been fully updated (first published 1933; most recently modified version published online September 2018). < adj.1882
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