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Note: A negative Delta-R will make the date older (typically presuming freshwater dilution from the global marine average).

Sample reports below show the difference between a radiocarbon date of 1000 /-30 BP with a Delta R of 0 /-0 (i.e.

with just the global marine reservoir correction) and a 1000 /-30BP radiocarbon date with a Delta R of 222 /-35 and the global marine reservoir correction included.

Freshwater systems running through limestone or fed by old water from springs can lead to falsely old ages in carbonate AMS dates.

A Delta±R correction is applied to the sample that has already been corrected with the global marine reservoir correction.

The value that is provided by the client is subtracted or added to this already corrected age (depending if it is a Delta R or Delta–R value).

Radiocarbon formed in the atmosphere is dissolved in oceans in the form of carbon dioxide and contemporaneously assimilated by plants through photosynthesis and enters food chains.

This is how terrestrial organisms take in carbon 14 in their systems.

Deep waters in oceans get carbon 14 from mixing with the surface waters as well as from the radioactive decay already occurring at their levels.

global marine reservoir correction) is applied automatically for all marine carbonates.

This automatic correction means the radiocarbon date gets more recent in time due to the fact that it takes 200-500 years for present-day carbon dioxide in the atmosphere to be incorporated and distributed (equilibrated) through the ocean water column.

The mixing of deep waters upward with surface waters—in a phenomenon known as upwelling—is latitude dependent and occurs predominantly in the equatorial region.

Coastline shape, local climate and wind, trade winds, and ocean bottom topography also affect upwelling. Mangerud, global variation in marine radiocarbon reservoir effect evident in shell carbonates are due to the incomplete mixing of upwelling water of “old” inorganic carbonates from the deep ocean where long residence times of more than 1,000 years cause depletion of carbon 14 activity through radioactive decay, resulting in very old apparent carbon 14 age.

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