Holocene

Among the topics are the cave at the end of the world: Cueva del Medio and the early colonization of southern South America, early human occupation in the southeastern plains of South America, mobility and human dispersion during the peopling of northwest South America between the late Pleistocene and the early Holocene, Mexican prehistory and Chiquihuite Cave (northern Zacatecas): studying Pleistocene human occupation as an exercise of skepticism, the end of an era: early Holocene Paleoindian caribou hunting in a Great Lakes glacial refugium, and where tides of genes perpetually ebb and flow: what DNA evidence says about the peopling of the Americas.

Dry erosional-denudational valleys, as well as denudational basins, are most often the subject of research concerning the evolution of the terrain relief in the late Vistulian and Holocene. In recent decades, dry valleys have been studied mainly in terms of morpholithology, morphogenetics and morphodynamics (e.g.

The eastern and western limb formations are Early Eocene Shaheed Ghat (shale), Drug (rubbly limestone), Baska (gypsum and shale) of Chamalang (Ghazij) Group and Middle Eocene Habib Rahi Limestone, Domanda shale, Pirkoh marl/limestone and Drazinda shale of Kahan Group, Oligocene Chitarwata (ferruginous sandstone, conglomerate and shale), Miocene Vihowa (red muds and sandstone) and Litra (greenish grey sandstone with some red muds) and Pliocene Chaudhwan (alternated sandstone and maroon muds) of Vihowa Group and Pleistocene Dada (conglomerate) and Holocene Sakhi Sarwar (clays, sandstone and conglomerates) of Sakhi Sarwar Group.

Scientists call this geologic epoch the Holocene. Our entire history of civilisation fits within it.

According to Meilan Solly of the Smithsonian, the earth is "currently situated in the Phanerozoic Eon, Cenozoic Era, Quaternary Period, Holocene Epoch and Meghalayan Age."

Modern humans, born into one climate era, called the Holocene, have crossed the border into another, the Anthropocene.

Summary: Modern humans, born into one climate era, called the Holocene, have crossed the border into another, the Anthropocene.

To get their results, the researchers looked at three of the best-documented warm periods, the Holocene thermal maximum (5000-9000 years ago), the last interglacial (129,000-116,000 years ago) and the mid-Pliocene warm period (3.3-3 million years ago).

A team of eight researchers from the Zoological Society of London (ZSL) published a paper in Science magazine, titled "New genus of extinct Holocene gibbon associated with humans in Imperial China," on June 22 introducing Junzi imperialis, or imperial gibbons, explaining the importance of the find.

The Holocene has lasted almost 12,000 years; it will not end in one.

Mid-Late Holocene Population Trends, Culture Change, and Marine Resource Intensification in Western Alaska.