Faster access than browser!
40 relations: Allerød oscillation, Antarctica, Archaeology, Atlantic (period), Bølling oscillation, Blytt–Sernander system, Boreal (age), British Isles, Bronze Age, Climatology, Core sample, Dendrochronology, Flandrian interglacial, Geography, Geology, Harry Godwin, Holocene, Iron Age, Johannes Iversen, Last glacial period, Lennart von Post, Mesolithic, Neolithic, Older Dryas, Oldest Dryas, Oxygen isotope ratio cycle, Palynology, Park Tundra, Peat, Pleistocene, Pollen core, Radiocarbon dating, Scandinavia, Sweden, Tundra, Upper Paleolithic, Varve, World War I, World War II, Younger Dryas.
Allerød oscillation
The Allerød oscillation (Allerødtiden) was a warm and moist global interstadial that occurred c.13,900 to 12,900 BP, nearly at the end of the last glacial period.
New!!: Pollen zone and Allerød oscillation · See more »
Antarctica
Antarctica is Earth's southernmost continent.
New!!: Pollen zone and Antarctica · See more »
Archaeology
Archaeology, or archeology, is the study of humanactivity through the recovery and analysis of material culture.
New!!: Pollen zone and Archaeology · See more »
Atlantic (period)
The Atlantic in palaeoclimatology was the warmest and moistest Blytt-Sernander period, pollen zone and chronozone of Holocene northern Europe.
New!!: Pollen zone and Atlantic (period) · See more »
Bølling oscillation
The Bølling oscillation, also Bølling interstadial, was a cool temperate climatic interstadial between the glacial Oldest Dryas and Older Dryas stadials, between 14,700 and 14,100 BP, near to the end of the last glacial period.
New!!: Pollen zone and Bølling oscillation · See more »
Blytt–Sernander system
The Blytt-Sernander classification, or sequence, is a series of north European climatic periods or phases based on the study of Danish peat bogs by Axel Blytt (1876) and Rutger Sernander (1908).
New!!: Pollen zone and Blytt–Sernander system · See more »
Boreal (age)
In paleoclimatology of the Holocene, the Boreal was the first of the Blytt-Sernander sequence of north European climatic phases that were originally based on the study of Danish peat bogs, named for Axel Blytt and Rutger Sernander, who first established the sequence.
New!!: Pollen zone and Boreal (age) · See more »
British Isles
The British Isles are a group of islands off the north-western coast of continental Europe that consist of the islands of Great Britain, Ireland, the Isle of Man and over six thousand smaller isles.
New!!: Pollen zone and British Isles · See more »
Bronze Age
The Bronze Age is a historical period characterized by the use of bronze, and in some areas proto-writing, and other early features of urban civilization.
New!!: Pollen zone and Bronze Age · See more »
Climatology
Climatology (from Greek κλίμα, klima, "place, zone"; and -λογία, -logia) or climate science is the scientific study of climate, scientifically defined as weather conditions averaged over a period of time.
New!!: Pollen zone and Climatology · See more »
Core sample
A core sample is a cylindrical section of (usually) a naturally occurring substance.
New!!: Pollen zone and Core sample · See more »
Dendrochronology
Dendrochronology (or tree-ring dating) is the scientific method of dating tree rings (also called growth rings) to the exact year they were formed in order to analyze atmospheric conditions during different periods in history.
New!!: Pollen zone and Dendrochronology · See more »
Flandrian interglacial
The Flandrian interglacial or stage is the name given by geologists and archaeologists in the British Isles to the first, and so far only, stage of the Holocene epoch (the present geological period), covering the period from around 12,000 years ago, at the end of the last glacial period to the present day.
New!!: Pollen zone and Flandrian interglacial · See more »
Geography
Geography (from Greek γεωγραφία, geographia, literally "earth description") is a field of science devoted to the study of the lands, the features, the inhabitants, and the phenomena of Earth.
New!!: Pollen zone and Geography · See more »
Geology
Geology (from the Ancient Greek γῆ, gē, i.e. "earth" and -λoγία, -logia, i.e. "study of, discourse") is an earth science concerned with the solid Earth, the rocks of which it is composed, and the processes by which they change over time.
New!!: Pollen zone and Geology · See more »
Harry Godwin
Sir Harry Godwin, FRS (9 May 1901 – 12 August 1985) was a prominent English botanist and ecologist of the 20th century.
New!!: Pollen zone and Harry Godwin · See more »
Holocene
The Holocene is the current geological epoch.
New!!: Pollen zone and Holocene · See more »
Iron Age
The Iron Age is the final epoch of the three-age system, preceded by the Stone Age (Neolithic) and the Bronze Age.
New!!: Pollen zone and Iron Age · See more »
Johannes Iversen
Johannes Iversen (December 12, 1904 – October 17, 1972) was a Danish palaeoecologist and plant ecologist.
New!!: Pollen zone and Johannes Iversen · See more »
Last glacial period
The last glacial period occurred from the end of the Eemian interglacial to the end of the Younger Dryas, encompassing the period years ago.
New!!: Pollen zone and Last glacial period · See more »
Lennart von Post
Ernst Jakob Lennart von Post (16June 188411January 1951) was a Swedish naturalist and geologist.
New!!: Pollen zone and Lennart von Post · See more »
Mesolithic
In Old World archaeology, Mesolithic (Greek: μέσος, mesos "middle"; λίθος, lithos "stone") is the period between the Upper Paleolithic and the Neolithic.
New!!: Pollen zone and Mesolithic · See more »
Neolithic
The Neolithic was a period in the development of human technology, beginning about 10,200 BC, according to the ASPRO chronology, in some parts of Western Asia, and later in other parts of the world and ending between 4500 and 2000 BC.
New!!: Pollen zone and Neolithic · See more »
Older Dryas
The Older Dryas was a stadial (cold) period between the Bølling and Allerød interstadials (warmer phases), about 14,000 years Before Present), towards the end of the Pleistocene. Its date is not well defined, with estimates varying by 400 years, but its duration is agreed to have been around 200 years. The gradual warming since the Last Glacial Maximum (27,000 to 24,000 years BP) has been interrupted by two cold spells: the Older Dryas and the Younger Dryas (c.
New!!: Pollen zone and Older Dryas · See more »
Oldest Dryas
The Oldest Dryas was a climatic period, which occurred during the coldest stadial after the Weichselian glaciation in north Europe.
New!!: Pollen zone and Oldest Dryas · See more »
Oxygen isotope ratio cycle
Oxygen isotope ratio cycles are cyclical variations in the ratio of the abundance of oxygen with an atomic mass of 18 to the abundance of oxygen with an atomic mass of 16 present in some substances, such as polar ice or calcite in ocean core samples, measured with the isotope fractionation.
New!!: Pollen zone and Oxygen isotope ratio cycle · See more »
Palynology
Palynology is the "study of dust" (from palunō, "strew, sprinkle" and -logy) or "particles that are strewn".
New!!: Pollen zone and Palynology · See more »
Park Tundra
Park tundra was a plant community that occurred in northwestern Europe after the last ice age ended.
New!!: Pollen zone and Park Tundra · See more »
Peat
Peat, also called turf, is an accumulation of partially decayed vegetation or organic matter that is unique to natural areas called peatlands, bogs, mires, moors, or muskegs.
New!!: Pollen zone and Peat · See more »
Pleistocene
The Pleistocene (often colloquially referred to as the Ice Age) is the geological epoch which lasted from about 2,588,000 to 11,700 years ago, spanning the world's most recent period of repeated glaciations.
New!!: Pollen zone and Pleistocene · See more »
Pollen core
A pollen core is a core sample of a medium containing a stratigraphic sequence of pollen.
New!!: Pollen zone and Pollen core · See more »
Radiocarbon dating
Radiocarbon dating (also referred to as carbon dating or carbon-14 dating) is a method for determining the age of an object containing organic material by using the properties of radiocarbon, a radioactive isotope of carbon.
New!!: Pollen zone and Radiocarbon dating · See more »
Scandinavia
Scandinavia is a region in Northern Europe, with strong historical, cultural and linguistic ties.
New!!: Pollen zone and Scandinavia · See more »
Sweden
Sweden (Sverige), officially the Kingdom of Sweden (Swedish), is a Scandinavian country in Northern Europe.
New!!: Pollen zone and Sweden · See more »
Tundra
In physical geography, tundra is a type of biome where the tree growth is hindered by low temperatures and short growing seasons.
New!!: Pollen zone and Tundra · See more »
Upper Paleolithic
The Upper Paleolithic (or Upper Palaeolithic, Late Stone Age) is the third and last subdivision of the Paleolithic or Old Stone Age.
New!!: Pollen zone and Upper Paleolithic · See more »
Varve
A varve is an annual layer of sediment or sedimentary rock.
New!!: Pollen zone and Varve · See more »
World War I
World War I (often abbreviated as WWI or WW1), also known as the First World War, the Great War, or the War to End All Wars, was a global war originating in Europe that lasted from 28 July 1914 to 11 November 1918.
New!!: Pollen zone and World War I · See more »
World War II
World War II (often abbreviated to WWII or WW2), also known as the Second World War, was a global war that lasted from 1939 to 1945, although conflicts reflecting the ideological clash between what would become the Allied and Axis blocs began earlier.
New!!: Pollen zone and World War II · See more »
Younger Dryas
The Younger Dryas (c. 12,900 to c. 11,700 years BP) was a return to glacial conditions which temporarily reversed the gradual climatic warming after the Last Glacial Maximum started receding around 20,000 BP.
New!!: Pollen zone and Younger Dryas · See more »
References
[1] https://en.wikipedia.org/wiki/Pollen_zone
