In today's article, we are going to address the topic of Greenlandian, an issue that has generated great interest in today's society. Greenlandian is a topic that has been the subject of debate and controversy in recent times, and it is crucial to understand its importance and impact on our lives. Throughout this article, we will explore the various aspects related to Greenlandian, from its origin and history to its relevance today. In addition, we will discuss the different points of view and opinions that exist around Greenlandian, with the aim of offering a complete and enriching vision of this very relevant topic. Get ready to immerse yourself in the exciting world of Greenlandian and discover everything this issue has to offer!
Greenlandian | ||||||
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Chronology | ||||||
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Etymology | ||||||
Name formality | Formal | |||||
Name ratified | 14 June 2018 | |||||
Usage information | ||||||
Celestial body | Earth | |||||
Regional usage | Global (ICS) | |||||
Time scale(s) used | ICS Time Scale | |||||
Definition | ||||||
Chronological unit | Age | |||||
Stratigraphic unit | Stage | |||||
Time span formality | Formal | |||||
Lower boundary definition | End of the Younger Dryas stadial | |||||
Lower boundary GSSP | NGRIP2 ice core, Greenland 75°06′00″N 42°19′12″W / 75.1000°N 42.3200°W | |||||
Lower GSSP ratified | 14 June 2018 (as base of Greenlandian) | |||||
Upper boundary definition | 8.2 kiloyear event | |||||
Upper boundary GSSP | NGRIP1 ice core, Greenland 75°06′00″N 42°19′12″W / 75.1000°N 42.3200°W | |||||
Upper GSSP ratified | 14 June 2018 |
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In the geologic time scale, the Greenlandian is the earliest age or lowest stage of the Holocene Epoch or Series, part of the Quaternary. Beginning in 11,650 BP (9701 BCE or 300 HE) and ending with the 8.2-kiloyear event (c. 8200–8300 BP, 6200–6300 BCE, 3600–3700 HE), it is the earliest of three sub-divisions of the Holocene. It was officially ratified by the International Commission on Stratigraphy in June 2018 with the later Northgrippian and Meghalayan Ages/Stages. The lower boundary of the Greenlandian Age is the GSSP sample from the North Greenland Ice Core Project in central Greenland (75.1000°N 42.3200°W). The Greenlandian GSSP has been correlated with the end of Younger Dryas (from near-glacial to interglacial) and a "shift in deuterium excess values".