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A proxy server is a server that sits between a client and a web server and represents itself to each end as being the other.
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Proxy comparison in ancient peat sediments: pollen, macrofossil and plant DNA
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The pollen, macrofossil and the trn L sequences are available through the Dryad repository doi We compared DNA, pollen and macrofossil data obtained from Weichselian interstadial age more than 40 kyr and Holocene maximum age cal yr BP peat sediments from northern Europe and used them to reconstruct contemporary floristic compositions at two sites. The majority of the samples provided plant DNA sequences of good quality with success amplification rates depending on age.
At both sites, pollen analysis detected the largest 54 and DNA the lowest 10 number of taxa, but five of the DNA taxa were not detected by pollen and macrofossils.
In the study of past climates ” paleoclimatology ” , climate proxies are preserved physical characteristics of the past that stand in for direct meteorological measurements  and enable scientists to reconstruct the climatic conditions over a longer fraction of the Earth’s history. Reliable global records of climate only began in the s, and proxies provide the only means for scientists to determine climatic patterns before record-keeping began.
A large number of climate proxies have been studied from a variety of geologic contexts. Examples of proxies include stable isotope measurements from ice cores , growth rates in tree rings , species composition of sub-fossil pollen in lake sediment or foraminifera in ocean sediments, temperature profiles of boreholes , and stable isotopes and mineralogy of corals and carbonate speleothems.
In each case, the proxy indicator has been influenced by a particular seasonal climate parameter e. Interpretation of climate proxies requires a range of ancillary studies, including calibration of the sensitivity of the proxy to climate and cross-verification among proxy indicators. Proxies can be combined to produce temperature reconstructions longer than the instrumental temperature record and can inform discussions of global warming and climate history.
The geographic distribution of proxy records, just like the instrumental record, is not at all uniform, with more records in the northern hemisphere. In science, it is sometimes necessary to study a variable which cannot be measured directly. This can be done by “proxy methods,” in which a variable which correlates with the variable of interest is measured, and then used to infer the value of the variable of interest. Proxy methods are of particular use in the study of the past climate, beyond times when direct measurements of temperatures are available.
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Not a MyNAP member yet? Register for a free account to start saving and receiving special member only perks. Establishing a baseline of natural climate variability over decade-to-century time scales requires a perspective that can be obtained only from a better knowledge of past variability, particularly that which precedes the pre-industrial era. Information revealing these past climate conditions is contained in historical records and “proxy” indicators.
The historical records of climate other than systematic weather observations, which began in the late s , while invaluable because of their scope and often uniquely relevant perspective, are usually limited to the last several hundred years see Chapter 2. The proxy indicators represent any piece of evidence that can be used to infer climate. Typically, proxy evidence includes the characteristics and constituent compositions of annual layers in polar ice caps, trees, and corals; material stored in ocean and lake sediments including biological, chemical, and mineral constituents ; records of lake levels; and certain historical documents.
Such proxy indicators can provide a wealth of information on past atmospheric compositions, tropospheric aerosol loads, volcanic eruptions, air and sea temperatures, precipitation and drought patterns, ocean chemistry and productivity, sea-level changes, former ice-sheet extent and thickness, and variations in solar activity—among other things.
These records are particularly appropriate for detecting three manifestations of climate variability:. Periodic or near-periodic variations the latter are those that become evident only after examination of considerable data through which a clear statistical signal stubbornly emerges ;. Large and pronounced climate signals, such as severe and sustained droughts, drastically altered precipitation patterns, anomalously warm or cold periods, or floods; and.
Gradual trends, infrequent shifts, or other characteristics of natural variability that are difficult to recognize without the benefit of a long, continuous or near-continuous record. Because the bulk of these proxy indicators are recorded naturally, their time span is potentially unlimited; their resolution and accuracy are limited only by the fidelity of the recorder itself.
These “natural archives” are simply there for the taking—awaiting discovery, recovery, means of extraction, and interpretation.