1. Sequence I is Holocene softy sediment.

2. This saphire deposit is occurred in the Holocene alluvium.

3. Dodos are flightless birds from the late Holocene.

4. The sea level changes of Holocene in Shanghai region are discussed in this paper based on the spore - pollen and microfossil analysis of Zhaoxiang core.

5. This article has a brief review on Holocene climate changes in Mongolia.

6. There is important for recover history of the Holocene Volcanic and conclude environment of crater.

7. The duration of Holocene Optimum defined as a postglacial interval of the most equable climate with warm temperatures and abundant rainfall has not been beyond debate.

8. The Holocene intermediate stage was associated with a normal marine environment, with increased oceanic sediments and a warmer and moist climate, indicating a good marine ecological environment.

9. Many studies have shown that the Holocene basement stratum in Shanghai region consists of hard clay with upper dark-green and lower yellowish-brown layer.

10. The group will investigate coastal processes and assess these in the context of late Quaternary and Holocene conditions.

11. Es Safa contains numerous vents that have been active during the holocene epoch (beginning approximately 12, 000 years ago).

12. The semi-buried pluvial-alluvial terrace in front of the mountain and the Holocene pluvial-alluvial fan compose sloping plain in front of the mountain.

13. The stone tools in later period is mainly microlithics, The main geological time of cultural layers falls between late Pleistocene and early Holocene Epoch.

14. The process of paleogeographic evolution in this area is from land of pleistocene epoch to ingression of holocene epoch, then to littoral circumstances of today.

15. There are disputes on transgression and high sea level in academe since holocene.

16. It is shown from the analysis results of grain size data that the sediments from the northern Okinawa Trough are mixture of terrigenous materials and volcanic ash during the Holocene epoch.

17. Two species of rhinoceros, Didermocerus sumatrensis and Rhinoceros sondaicus, had been certainly confirmed being alive in China in Holocene epoch.

18. Data from the Antarctic temperature record show that the warming of the past 50 years has taken global temperature back to approximately the peak of the current interglacial (the Holocene).

19. The priciple of cyclic sedimentation applies to deposits dating from earliest Paleozoic time to the Holocene.

20. So , the old sand body is a result of the middle-late Holocene continental-oceanic interaction.

21. The fault has been mainly in stick slip from Subei to Arkesai, and in creep slip from Bage Valley to Changma Dam since Holocene Epoch.

22. The speed of uplift became slow, and the period of stability became long from Neopleistocene to Holocene epoch . There were descending movement on the uplift background in Holocene epoch.

23. East China Sea floor investigation and core data have showed that Holocene basement consists of yellow-brown or dark-green hard clay of 0.1-2m in thickness, buried beneath the soft Holocene deposits.

24. Sequence I can be distinguished from the northwest slope to trough basin and is Holocene softy sediments.

25. Through the analysis of 84 samples collected from the core B-3GC in the northern Okinawa Trough, a high resolution dinoflagellate cyst record of the Holocene has been obtained.

26. The eastern part of the western Henan province is covered with eolian loess and alluvial or diluvial loess. The Holocene and Late Pleistocene loess have low to moderate collapsibility.

27. The loesslike-palaeosoil series is one of the main bases for researching environment evolution of Holocene Epoch.

28. Wuguan marine erosion physiognomy has important geognosy significance in the study of structural movement and the changes in sea level in period of Holocene Epoch.

28. try its best to gather and build good sentences.

29. Therefore, the area is typical to study the environmental change of China , even of the globe since Quaternary Period, especially since the Holocene Epoch.

30. The shallow layer nature gas at the extrance of Hangzhou Gulf mainly existed in the stratums between Holocene epoch and Pleistocene epoch of the 4th Era.

31. In the early Holocene Epoch, the climate turned warm. Water collected in the low-lying lands and freshwater lakes formed.

32. These materials reveal that Holocene paleosol around Xi′an formed during Megathermal is luvic cinnamon soil developing in warm and humid climate but not developing in subarid climate.

33. In an editorial published in May, the respected publication argued that the Holocene could simply be renamed the Anthropocene.

34. The Yumen fault has been active since the Early Pleistocene to the present day, so it is an active fault during the Holocene Epoch and a causative fault of the Yumen earthquake.

35. On the influence of land cover on early Holocene climate in northern latitudes.

36. Rather than placing us still in the Holocene, a peculiarly stable era that began only around 10,000 years ago, the geologists say we are already living in the Anthropocene: the age of man.