अरनिया हिंदी उपयोग और उदाहरण

अरनियान वाली : यह स्‍थल, सिरसा के सिरसा भद्र रोड़ पर 8 किलोमीटर दक्षिण में स्थित है जहां चार एकड़ जमीन और दस फुट ऊंचा टीला स्थित है, यहां मध्‍ययुगीन अवधि से संबंधित टूटी हुई मिट्टी के बर्तन के टुकड़े प्राप्‍त किए गए है।

3. समता महाविद्यालय अरनिया, जन्दाहा।

""3. समता महाविद्यालय अरनिया, जन्दाहा।

अरनियाँ ख्वाजा राजू इगलास, अलीगढ़, उत्तर प्रदेश स्थित एक गाँव है।

अरनिया इसके अंग्रेजी अर्थ का उदाहरण

Porroglossum marniae Luer.

For example, the Egyptian cavern features decorations of [and The Carnian (less commonly, Karnian) is the lowermost stage of the Upper Triassic series (or earliest age of the Late Triassic epoch).

The Carnian is preceded by the Ladinian and is followed by the Norian.

Its boundaries are not characterized by major extinctions or biotic turnovers, but a climatic event (known as the Carnian Pluvial Event) occurred during the Carnian and seems to be associated with important extinctions or biotic radiations.

The Carnian was named in 1869 by Mojsisovics.

It is unclear if it was named after the Carnic Alps or after the Austrian region of Carinthia (Kärnten in German) or after the Carnia historical region in northwestern Italy.

The base of the Carnian stage is defined as the place in the stratigraphic record where the ammonite species Daxatina canadensis first appears.

The top of the Carnian (the base of the Norian) is at the bases of the ammonite biozones of Klamathites macrolobatus or Stikinoceras kerri and the conodont biozones of Metapolygnathus communisti or Metapolygnathus primitius.

There is no established, standard usage for the Carnian subdivisions, thus, while in some regional stratigraphies a two-substage subdivision is common:.

In the Tethys domain, the Carnian stage contains six ammonite biozones:.

The paleogeography of the Carnian was basically the same as for the rest of the Triassic.

This putative climatic event is called the "Carnian Pluvial Event", its age being between latest early Carnian (Julian) and the beginning of late Carnian (Tuvalian).

In the marine realm, the Carnian saw the first abundant occurrences of calcareous nanoplankton, a morphological group including the coccolithophores.

There are a few invertebrates which are typical and characteristic of the Carnian.

Among molluscs, the ammonoid genus Trachyceras is exclusive to the lower Carnian (i.