Layered intrusion and Prothrombin time: Difference between pages

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The '''prothrombin time''' ('''PT''') and its derived measures of '''prothrombin ratio''' ('''PR''') and '''international normalized ratio''' ('''INR''') are measures of the ''extrinsic pathway'' of [[coagulation]]. They are used to determine the clotting tendency of blood, in the measure of [[warfarin]] dosage, liver damage, and [[vitamin K]] status. The [[reference range]] for prothrombin time is usually around 12–15 seconds; the normal range for the INR is 0.8–1.2. PT measures factors [[thrombin|II]], V, VII, X and [[fibrinogen]]. It is used in conjunction with the [[partial thromboplastin time|activated partial thromboplastin time]] (aPTT) which measures the ''intrinsic pathway''.
'''Ultramafic to mafic layered intrusions''' are found in typically ancient [[craton]]s and are rare but worldwide in distribution. The intrusive complexes exhibit evidence of [[Fractional crystallization (geology)|fractional crystallization]] and crystal segregation by settling or floating of minerals from a melt.


==Laboratory measurement==
Ideally the stratigraphic sequence of an ultramafic-mafic [[intrusive]] complexe consists of [[ultramafic]] [[peridotite]]s and [[pyroxenite]]s with associated [[chromitite]] layers toward the base with more [[mafic]] [[norite]]s, [[gabbro]]s and [[anorthosite]]s in the upper layers. Some include [[diorite]] and [[granophyre]] near the top of the bodies. Orebodies of [[platinum group]] elements, [[chromite]], [[magnetite]] and [[ilmenite]] are often associated with these rare intrusions.
===Methodology===
The prothrombin time is most commonly measured using [[blood plasma]]. Blood is drawn into a [[test tube]] containing liquid [[citrate]], which acts as an anticoagulant by binding the calcium in a sample. The blood is mixed, then centrifuged to separate blood cells from plasma. In [[newborn]]s, whole blood is used.{{Fact|date=May 2008}}


The plasma is analyzed by a [[medical technologist]] on an automated instrument at 37°C, which takes a sample of the plasma. An excess of calcium is added (thereby reversing the effects of citrate), which enables the blood to clot again. For an accurate measurement the proportion of blood to citrate needs to be fixed; many laboratories will not perform the assay if the tube is underfilled and contains a relatively high concentration of citrate. This is because [[Vacutainer]] test tubes generally contain a powdered anticoagulant to prevent blood from clotting. For the prothrombin time test the appropriate sample is the blue top tube, or citrate tube, which is a liquid anticoagulant. Just as adding solvent to any solution will dilute it, adding liquid anticoagulant to blood will dilute it. This dilution will cause a falsely long prothrombin time. So, all analysis takes this dilution into account by multiplying the result by 1.1 to account for the dilution. If a tube is underfilled or overfilled with blood, the standardized dilution of 1.1 is no longer valid.
==Intrusive behavior and setting==
Mafic-ultramafic layered intrusions occur at all levels within the crust, from depths in excess of 50km to depths of as little as 1.5 to 5km. The depth at which an intrusion is formed is dependent on several factors:
* Density of the melt. Magmas with high magnesium and iron contents are denser and are therefore less likely to be able to reach the surface.
* Interfaces within the crust. Typically, a horizontal detachment zone, a dense, impermeable layer or even a lithological interface may provide a horizontal plane of weakness which the ascending magma will exploit, forming a [[sill]] or [[lopolith]].
* Temperature and viscosity. As an ascending magma rises and cools, it becomes thicker and more viscous. This then restricts the magma from rising further because more energy is required to push it upwards. Conversely, thicker magma is also more efficient at forcing apart the wall rocks, creating volume which the magma may fill.


[[Tissue factor]] (also known as ''factor III'' or ''thromboplastin'') is added, and the time the sample takes to clot is measured optically. Some laboratories use a mechanical measurement, which eliminates interferences from lipemic and icteric samples.
==Intrusive Mechanisms==
It is difficult to precisely determine what causes large ultramaficmafic intrusives to be emplaced within the crust, but there are two main hypotheses: '''''plume magmatism''''' and '''''rift upwelling'''''.


The prothrombin ratio is the prothrombin time for a patient, divided by the result for control plasma.
===Plume Magmatism===
The plume magmatism theory is based on observations that most [[large igneous province]]s include both hypabyssal and surficial manifestations of voluminous mafic magmatism within the same temporal period. For instance, in most [[Archaean]] cratons, greenstone belts correlate with voluminous dyke injection as well as usually some form of larger intrusive episodes into the crust. This is particularly true of a series of ultramafic-mafic layered intrusions in the [[Yilgarn craton|Yilgarn Craton]] of ~2.8 Ga and associated [[komatiite]] volcanism and widespread [[tholeiitic]] volcanism.


===International normalized ratio===
Plume magmatism is an effective mechanism for explaining the large volumes of magmatism required to inflate an intrusion to several kilometres thickness (up to and greater than 13 kilometres). Plumes also tend to create warping of the crust, weaken it thermally so that it is easier to intrude magma and create space to host the intrusions.
Because of differences between different batches and manufacturers of tissue factor (it is a biologically obtained product), the INR was devised to standardize the results.


Each manufacturer gives an ISI (International Sensitivity Index) for any tissue factor they make. The ISI value indicates how the particular batch of tissue factor compares to an internationally standardized sample. The ISI is usually between 1.0 and 1.4.
Plume magmatism is supported in some intrusions by geochemistry. In particular the [[Norilsk|Noril's-Talnakh]] intrusions are considered to be created by plume magmatism and other large intrusions have been suggested as created by mantle plumes.


The INR is the ratio of a patient's prothrombin time to a normal (control) sample, raised to the power of the ISI value for the control sample used.
However, the story is not so simple, because most ultramafic-mafic layered intrusions also correlate with craton margins, perhaps because they are exhumed more efficiently in cratonic margins because of faulting and subsequent orogeny.


:<math>
===Rift magmatism===
\text{INR}= \left(\frac{\text{PT}_\text{test}}{\text{PT}_\text{normal}}\right)^\text{ISI}
The presence of large layered complexes in Greenland such as the [[Skaergaard intrusion]] which are not related to mantle plumes indicated other processes can form these intrusions. Here, the large magma volumes which are created by mid-ocean ridge spreading allow the accumlation of large volumes of cumulate rocks. Also, the problem of creating space for the intrusion is easily explained by the extensional tectonics in operation.
</math>


===Interpretation===
==Causes of layering==
The prothrombin time is the time it takes [[blood plasma|plasma]] to clot after addition of [[tissue factor]] (obtained from animals). This measures the quality of the ''extrinsic pathway'' (as well as the ''common pathway'') of [[coagulation]].
The causes of layering in large ultramafic intrusions include [[convection]], thermal diffusion, assimilation of wall rocks and [[Fractional crystallization (geology)|fractional crystallization]].


The speed of the ''extrinsic pathway'' is greatly affected by levels of [[factor VII]] in the body. Factor VII has a short [[half-life]] and its synthesis requires [[vitamin K]]. The prothrombin time can be prolonged as a result of deficiencies in vitamin K, which can be caused by [[warfarin]], [[malabsorption]], or lack of intestinal colonization by bacteria (such as in [[newborn]]s). In addition, poor factor VII synthesis (due to [[liver disease]]) or increased consumption (in [[disseminated intravascular coagulation]]) may prolong the PT.
The primary mechanism for forming cumulate layers is of course the accumulation of layers of mineral crystals on the floor or roof of the intrusion. Rarely, [[plagioclase]] is found in [[cumulate rocks|cumulate]] layers at the top of intrusions, having floated to the top of a much denser [[magma]]. Here it can form [[anorthosite]] layers.


A high INR level such as INR=5 indicates that there is a high chance of bleeding, whereas if the INR=0.5 then there is a high chance of having a clot. Normal range for a healthy person is 0.9–1.3, and for people on warfarin therapy, 2.0–3.0, although the target INR may be higher in particular situations, such as [[artificial heart valve|mechanical heart valves]].
Accumulation occurs as crystals are formed by fractional crystallisation and, if they are dense enough, precipitate out from the magma. In large enough and hot enough magma chambers, where vigorous convection currents form, pseudo-sedimentary structures such as [[flow banding]], [[graded bedding]], scour channels, foreset beds and other usually sedimentary features can be created by convection and settling processes. The [[Skaergaard intrusion]] in [[Greenland]] is a prime example of these quasi-sedimentary structures.


===Factors determining accuracy===
Whilst fractional crystallisation is the dominant process, it can be triggered in the magma body by assimilation of the wall rocks. This will tend to increase the silica content of the melt, which will eventually prompt a mineral to reach the liquidus for that magma composition. Note also that assimilation of wall rocks takes considerable thermal energy, so this process goes hand in hand with the natural cooling of the magma body. Often, assimilation can only be proven by detailed [[geochemistry]].
[[Lupus anticoagulant]], a circulating inhibitor predisposing for thrombosis, may skew PT results, depending on the assay used.<ref>Della Valle P, Crippa L, Garlando AM, Pattarini E, Safa O, Vigano D'Angelo S, D'Angelo A. Interference of lupus anticoagulants in prothrombin time assays: implications for selection of adequate methods to optimize the management of thrombosis in the antiphospholipid-antibody syndrome. ''Haematologica'' 1999;84:1065-74. PMID 10586206.</ref> Variations between various thromboplastin preparations have in the past led to decreased accuracy of INR readings, and a 2005 study suggested that despite international calibration efforts (by INR) there were still statistically significant differences between various kits,<ref>Horsti J, Uppa H, Vilpo JA. Poor agreement among prothrombin time international normalized ratio methods: comparison of seven commercial reagents. ''Clin Chem'' 2005;51:553-60. PMID 15665046.</ref> casting doubt on the long-term tenability of PT/INR as a measure for anticoagulant therapy.<ref name=Jackson>Jackson CM, Esnouf MP. Has the time arrived to replace the quick prothrombin time test for monitoring oral anticoagulant therapy? ''Clin Chem'' 2005;51:483-5. PMID 15738512.</ref>


==Statistics==
Often, cumulate layers are polyminerallic, forming [[gabbro]], [[norite]] and other rock types. The terminology of cumulate rocks, however, is usually used to describe the individual layers as, for instance ''pyroxene-plagioclase cumulates''.
An estimated 800 million PT/INR assays are performed annually worldwide.<ref name=Jackson/>


==Near-patient testing==
Monominerallic cumulate layers are common. These may be economically important, for instance magnetite and ilmenite layers are known to form [[titanium]], [[vanadium]] deposits such as at [[Windimurra intrusion]] and hard-rock [[iron]] deposits (such as at [[Savage River, Tasmania]]). [[Chromite]] layers are associated with [[platinum]]-[[palladium]] group element ([[Platinum group|PGE]]) deposits, the most famous of these being the [[Merensky Reef]] in the [[Bushveld igneous complex|Bushveld Igneous Complex]].
In addition to the laboratory method outlined above, near-patient testing (NPT) or home INR monitoring is becoming increasingly common in some countries. In the [[United Kingdom]], for example, near-patient testing is used both by patients at home, and by some anticoagulation clinics (often hospital-based) as a fast and convenient alternative to the lab method. After a period of doubt about the accuracy of NPT results, a new generation of machines and reagents seems to be gaining acceptance for its ability to deliver results close in accuracy to those of the lab.<ref>Poller L, Keown M, Chauhan N, Van Den Besselaar AM, Tripodi A, Shiach C, Jespersen J; ECCA Steering Group Members. European Concerted Action on Anticoagulation. Correction of displayed international normalized ratio on two point-of-care test whole-blood prothrombin time monitors (CoaguChek Mini and TAS PT-NC) by independent international sensitivity index calibration. ''Br J Haematol'' 2003;122:944-9. PMID 12956765.</ref>


In a typical NPT setup a small table-top device is used; for example the [[Hoffmann-La Roche|Roche]] Coaguchek S, or the more recently (2005) introduced HemoSense INRatio. A drop of capillary blood is obtained with an automated finger-prick, which is almost painless. This drop is placed on a disposable test strip with which the machine has been prepared. The resulting INR comes up on the display a few seconds later. Similar testing methods are used by [[diabetes mellitus|diabetics]] on [[insulin]], and are easily taught and practiced.
The central section or upper sections of many large ultramafic intrusions are poorly layered, massive gabbro. This is because as the magma differentiates it reaches a composition favouring crystallisation of only two or three minerals; the magma may also have cooled by this stage sufficiently for the increasing [[viscosity]] of the magma to halt effective convection, or convection may stop or break up into inefficient small cells because the revervoir becomes too thin and flat.


Local policy determines whether the patient or a coagulation specialist (nurse, general practitioner or hospital doctor) interprets the result and determines the dose of medication. In Germany, patients may adjust the medication dose themselves,{{Fact|date=February 2007}} while in the UK and the USA this remains in the hands of a health care professional.
==Examples==
* [[Bushveld igneous complex]], [[South Africa]]
* [[Dufek intrusion]], [[Antarctica]]
* [[Duluth Complex]], northeastern [[Minnesota]]
* [[Giles complex]] intrusions central [[Australia]]
* [[Great Dyke]], [[Zimbabwe]]
* [[Kiglapait intrusion]], [[Labrador]]
* [[Lac des Iles igneous complex]], [[Ontario]]
* [[Muskox intrusion]], [[Canada]]
* [[Skaergaard intrusion]] of east [[Greenland]]
* [[Stillwater igneous complex]], southwestern [[Montana]]
* [[Windimurra intrusion]], [[West Australia]]


The advantages of the NPT approach are obvious: it is fast and convenient, usually less painful, and offers, in home use, the ability for patients to measure their own INRs when required. Among its problems are that quite a steady hand is needed to deliver the blood to the exact spot, that some patients find the finger-pricking difficult, and that the cost of the test strips must also be taken into account. In the UK these are available on prescription so that elderly and unwaged people will not pay for them and others will pay only a standard prescription charge, which at the moment represents only about 20% of the retail price of the strips. In the USA, NPT in the home is currently reimbursed by [[Medicare (United States)|Medicare]] for patients with mechanical heart valves, while private insurers may cover for other indications.
==See also==
* [[ultramafic|Definition of ultramafic]]
* [[List of rock types]]
* [[Igneous rocks]]
* [[Igneous differentiation|Fractional crystallization]]


There is some evidence to suggest that NPT may be less accurate for certain patients, for example those who have the [[lupus anticoagulant]].{{Fact|date=February 2007}}
==References==
* Blatt, Harvey and Robert J. Tracy, 1996, ''Petrology: Igneous, Sedimentary and Metamorphic,'' 2nd ed., pp. 123-132 & 194-197, Freeman, ISBN 0-7167-2438-3
* Ballhaus, C.G. & Glikson, A.Y., 1995, ''Petrology of layered mafic-ultramafic intrusions of the Giles Complex, western Musgrave Block, central Australia''. AGSO Journal, 16/1&2: 69-90.


===Guidelines for near-patient testing or home INR monitoring===
==External links==
International guidelines were published in 2005 to govern home monitoring of oral anticoagulation by the International Self-Monitoring Association for Oral Anticoagulation.<ref>{{cite journal| title=Guidelines for implementation of patient self-testing and patient self-management of oral anticoagulation. International consensus guidelines prepared by International Self-Monitoring Association for Oral Anticoagulation| author=Jack Ansell| journal=International Journal of Cardiology| date=10 March 2005| url= http://www.sciencedirect.com/science?_ob=ArticleURL&_udi=B6T16-4CVR7GB-2&_user=10&_coverDate=03%2F10%2F2005&_rdoc=1&_fmt=&_orig=search&_sort=d&view=c&_acct=C000050221&_version=1&_urlVersion=0&_userid=10&md5=31d380c38e3d5afdba3f7dbb04e8b5b7 }}</ref>
*[http://www.gsf.fi/explor/pgeweb/home.htm Overview of Finnish Layered Intrusions]
The international guidelines study stated, “The consensus agrees that patient self-testing and patient self-management are effective methods of monitoring oral anticoagulation therapy, providing outcomes at least as good as, and possibly better than, those achieved with an anticoagulation clinic. All patients must be appropriately selected and trained. Currently available self-testing/self-management devices give INR results which are comparable with those obtained in laboratory testing.”
*[http://www.igem.ru/igem/petr/int7.htm Overview of Monche Tundra Intrusion, Russia]

Medicare coverage for home testing of INR has been expanded in order to allow more people access to home testing of INR in the USA. The release on the 19th March 2008 said, “[t]he Centers for Medicare & Medicaid Services (CMS) expanded Medicare coverage for home blood testing of prothrombin time (PT) International Normalized Ratio (INR) to include beneficiaries who are using the drug warfarin, an anticoagulant (blood thinner) medication, for chronic atrial fibrillation or venous thromboembolism.” In addition, “[t]hose Medicare beneficiaries and their physicians managing conditions related to chronic atrial fibrillation or venous thromboembolism will benefit greatly through the use of the home test.”<ref>{{cite web | title= Medicare expands coverage for home blood testing of prothrombin time international normalized ratio| publisher= The [[Centers for Medicare and Medicaid Services]] | date= 19 March 2008| url= http://www.cms.hhs.gov/apps/media/press/release.asp?Counter=2987 }}</ref>

==History==
The prothrombin time was discovered by Dr Armand Quick and colleagues in 1935,<ref>Quick AJ, Stanley-Brown M, Bancroft FW. A study of the coagulation defect in hemophilia and in jaundice. ''Am J Med Sc 1935;190:501.</ref> and a second method was published by Dr Paul Owren<ref>Owren PA, Aas K. The control of dicumarol therapy and the quantitative determination of prothrombin and proconvertin. ''Scand J Clin Lab Invest'' 1951;3:201-8. PMID 14900966.</ref> (also called the "p and p" or "prothrombin and proconvertin" method). It aided in the identification of the [[anticoagulant]]s [[dicumarol]] and [[warfarin]],<ref>Campbell HA, Smith WK, Roberts WL, Link KP. Studies on the hemorrhagic sweet clover disease. II. The bioassay of hemorrhagic concentrates by following the prothrombin level in the plasma of rabbit blood. ''J Biol Chem'' 1941;138:1-20.</ref> and was used subsequently as a measure of activity for warfarin when used therapeutically.

The INR was introduced in the early 1980s when it turned out that there was a large degree of variation between the various prothrombin time assays, a discrepancy mainly due to problems with the purity of the thromboplastin (tissue factor) concentrate.<ref>Hirsh J, Bates SM. Clinical trials that have influenced the treatment of venous thromboembolism: a historical perspective. ''Ann Intern Med'' 2001;134:409-17. PMID 11242501.</ref> The INR became widely accepted worldwide, especially after endorsement by the [[World Health Organisation]].<ref>Expert Committee on Biological Standardization. Requirements for thromboplastins and plasma used to control oral anticoagulant therapy. ''World Health Organ Tech Rep Ser'' 1983;33:81-105.<!--Not indexed on PubMed--></ref>

==References==
{{Reflist|2}}


[[Category:Economic geology]]
[[Category:Blood tests]]
[[Category:Igneous rocks]]
[[Category:Petrology]]


[[de:Quickwert]]
[[it:Intrusioni mafiche stratificate]]
[[fr:Taux de prothrombine]]
[[fi:Kerrosintruusio]]
[[it:Tempo di protrombina]]
[[nl:International Normalized Ratio]]
[[ja:プロトロンビン時間]]
[[no:Internasjonalt normalisert ratio]]
[[pl:Czas protrombinowy]]
[[pt:Tempo de protrombina]]

Revision as of 03:17, 11 October 2008

The prothrombin time (PT) and its derived measures of prothrombin ratio (PR) and international normalized ratio (INR) are measures of the extrinsic pathway of coagulation. They are used to determine the clotting tendency of blood, in the measure of warfarin dosage, liver damage, and vitamin K status. The reference range for prothrombin time is usually around 12–15 seconds; the normal range for the INR is 0.8–1.2. PT measures factors II, V, VII, X and fibrinogen. It is used in conjunction with the activated partial thromboplastin time (aPTT) which measures the intrinsic pathway.

Laboratory measurement

Methodology

The prothrombin time is most commonly measured using blood plasma. Blood is drawn into a test tube containing liquid citrate, which acts as an anticoagulant by binding the calcium in a sample. The blood is mixed, then centrifuged to separate blood cells from plasma. In newborns, whole blood is used.[citation needed]

The plasma is analyzed by a medical technologist on an automated instrument at 37°C, which takes a sample of the plasma. An excess of calcium is added (thereby reversing the effects of citrate), which enables the blood to clot again. For an accurate measurement the proportion of blood to citrate needs to be fixed; many laboratories will not perform the assay if the tube is underfilled and contains a relatively high concentration of citrate. This is because Vacutainer test tubes generally contain a powdered anticoagulant to prevent blood from clotting. For the prothrombin time test the appropriate sample is the blue top tube, or citrate tube, which is a liquid anticoagulant. Just as adding solvent to any solution will dilute it, adding liquid anticoagulant to blood will dilute it. This dilution will cause a falsely long prothrombin time. So, all analysis takes this dilution into account by multiplying the result by 1.1 to account for the dilution. If a tube is underfilled or overfilled with blood, the standardized dilution of 1.1 is no longer valid.

Tissue factor (also known as factor III or thromboplastin) is added, and the time the sample takes to clot is measured optically. Some laboratories use a mechanical measurement, which eliminates interferences from lipemic and icteric samples.

The prothrombin ratio is the prothrombin time for a patient, divided by the result for control plasma.

International normalized ratio

Because of differences between different batches and manufacturers of tissue factor (it is a biologically obtained product), the INR was devised to standardize the results.

Each manufacturer gives an ISI (International Sensitivity Index) for any tissue factor they make. The ISI value indicates how the particular batch of tissue factor compares to an internationally standardized sample. The ISI is usually between 1.0 and 1.4.

The INR is the ratio of a patient's prothrombin time to a normal (control) sample, raised to the power of the ISI value for the control sample used.

Interpretation

The prothrombin time is the time it takes plasma to clot after addition of tissue factor (obtained from animals). This measures the quality of the extrinsic pathway (as well as the common pathway) of coagulation.

The speed of the extrinsic pathway is greatly affected by levels of factor VII in the body. Factor VII has a short half-life and its synthesis requires vitamin K. The prothrombin time can be prolonged as a result of deficiencies in vitamin K, which can be caused by warfarin, malabsorption, or lack of intestinal colonization by bacteria (such as in newborns). In addition, poor factor VII synthesis (due to liver disease) or increased consumption (in disseminated intravascular coagulation) may prolong the PT.

A high INR level such as INR=5 indicates that there is a high chance of bleeding, whereas if the INR=0.5 then there is a high chance of having a clot. Normal range for a healthy person is 0.9–1.3, and for people on warfarin therapy, 2.0–3.0, although the target INR may be higher in particular situations, such as mechanical heart valves.

Factors determining accuracy

Lupus anticoagulant, a circulating inhibitor predisposing for thrombosis, may skew PT results, depending on the assay used.[1] Variations between various thromboplastin preparations have in the past led to decreased accuracy of INR readings, and a 2005 study suggested that despite international calibration efforts (by INR) there were still statistically significant differences between various kits,[2] casting doubt on the long-term tenability of PT/INR as a measure for anticoagulant therapy.[3]

Statistics

An estimated 800 million PT/INR assays are performed annually worldwide.[3]

Near-patient testing

In addition to the laboratory method outlined above, near-patient testing (NPT) or home INR monitoring is becoming increasingly common in some countries. In the United Kingdom, for example, near-patient testing is used both by patients at home, and by some anticoagulation clinics (often hospital-based) as a fast and convenient alternative to the lab method. After a period of doubt about the accuracy of NPT results, a new generation of machines and reagents seems to be gaining acceptance for its ability to deliver results close in accuracy to those of the lab.[4]

In a typical NPT setup a small table-top device is used; for example the Roche Coaguchek S, or the more recently (2005) introduced HemoSense INRatio. A drop of capillary blood is obtained with an automated finger-prick, which is almost painless. This drop is placed on a disposable test strip with which the machine has been prepared. The resulting INR comes up on the display a few seconds later. Similar testing methods are used by diabetics on insulin, and are easily taught and practiced.

Local policy determines whether the patient or a coagulation specialist (nurse, general practitioner or hospital doctor) interprets the result and determines the dose of medication. In Germany, patients may adjust the medication dose themselves,[citation needed] while in the UK and the USA this remains in the hands of a health care professional.

The advantages of the NPT approach are obvious: it is fast and convenient, usually less painful, and offers, in home use, the ability for patients to measure their own INRs when required. Among its problems are that quite a steady hand is needed to deliver the blood to the exact spot, that some patients find the finger-pricking difficult, and that the cost of the test strips must also be taken into account. In the UK these are available on prescription so that elderly and unwaged people will not pay for them and others will pay only a standard prescription charge, which at the moment represents only about 20% of the retail price of the strips. In the USA, NPT in the home is currently reimbursed by Medicare for patients with mechanical heart valves, while private insurers may cover for other indications.

There is some evidence to suggest that NPT may be less accurate for certain patients, for example those who have the lupus anticoagulant.[citation needed]

Guidelines for near-patient testing or home INR monitoring

International guidelines were published in 2005 to govern home monitoring of oral anticoagulation by the International Self-Monitoring Association for Oral Anticoagulation.[5] The international guidelines study stated, “The consensus agrees that patient self-testing and patient self-management are effective methods of monitoring oral anticoagulation therapy, providing outcomes at least as good as, and possibly better than, those achieved with an anticoagulation clinic. All patients must be appropriately selected and trained. Currently available self-testing/self-management devices give INR results which are comparable with those obtained in laboratory testing.”

Medicare coverage for home testing of INR has been expanded in order to allow more people access to home testing of INR in the USA. The release on the 19th March 2008 said, “[t]he Centers for Medicare & Medicaid Services (CMS) expanded Medicare coverage for home blood testing of prothrombin time (PT) International Normalized Ratio (INR) to include beneficiaries who are using the drug warfarin, an anticoagulant (blood thinner) medication, for chronic atrial fibrillation or venous thromboembolism.” In addition, “[t]hose Medicare beneficiaries and their physicians managing conditions related to chronic atrial fibrillation or venous thromboembolism will benefit greatly through the use of the home test.”[6]

History

The prothrombin time was discovered by Dr Armand Quick and colleagues in 1935,[7] and a second method was published by Dr Paul Owren[8] (also called the "p and p" or "prothrombin and proconvertin" method). It aided in the identification of the anticoagulants dicumarol and warfarin,[9] and was used subsequently as a measure of activity for warfarin when used therapeutically.

The INR was introduced in the early 1980s when it turned out that there was a large degree of variation between the various prothrombin time assays, a discrepancy mainly due to problems with the purity of the thromboplastin (tissue factor) concentrate.[10] The INR became widely accepted worldwide, especially after endorsement by the World Health Organisation.[11]

References

  1. ^ Della Valle P, Crippa L, Garlando AM, Pattarini E, Safa O, Vigano D'Angelo S, D'Angelo A. Interference of lupus anticoagulants in prothrombin time assays: implications for selection of adequate methods to optimize the management of thrombosis in the antiphospholipid-antibody syndrome. Haematologica 1999;84:1065-74. PMID 10586206.
  2. ^ Horsti J, Uppa H, Vilpo JA. Poor agreement among prothrombin time international normalized ratio methods: comparison of seven commercial reagents. Clin Chem 2005;51:553-60. PMID 15665046.
  3. ^ a b Jackson CM, Esnouf MP. Has the time arrived to replace the quick prothrombin time test for monitoring oral anticoagulant therapy? Clin Chem 2005;51:483-5. PMID 15738512.
  4. ^ Poller L, Keown M, Chauhan N, Van Den Besselaar AM, Tripodi A, Shiach C, Jespersen J; ECCA Steering Group Members. European Concerted Action on Anticoagulation. Correction of displayed international normalized ratio on two point-of-care test whole-blood prothrombin time monitors (CoaguChek Mini and TAS PT-NC) by independent international sensitivity index calibration. Br J Haematol 2003;122:944-9. PMID 12956765.
  5. ^ Jack Ansell (10 March 2005). "Guidelines for implementation of patient self-testing and patient self-management of oral anticoagulation. International consensus guidelines prepared by International Self-Monitoring Association for Oral Anticoagulation". International Journal of Cardiology.
  6. ^ "Medicare expands coverage for home blood testing of prothrombin time international normalized ratio". The Centers for Medicare and Medicaid Services. 19 March 2008.
  7. ^ Quick AJ, Stanley-Brown M, Bancroft FW. A study of the coagulation defect in hemophilia and in jaundice. Am J Med Sc 1935;190:501.
  8. ^ Owren PA, Aas K. The control of dicumarol therapy and the quantitative determination of prothrombin and proconvertin. Scand J Clin Lab Invest 1951;3:201-8. PMID 14900966.
  9. ^ Campbell HA, Smith WK, Roberts WL, Link KP. Studies on the hemorrhagic sweet clover disease. II. The bioassay of hemorrhagic concentrates by following the prothrombin level in the plasma of rabbit blood. J Biol Chem 1941;138:1-20.
  10. ^ Hirsh J, Bates SM. Clinical trials that have influenced the treatment of venous thromboembolism: a historical perspective. Ann Intern Med 2001;134:409-17. PMID 11242501.
  11. ^ Expert Committee on Biological Standardization. Requirements for thromboplastins and plasma used to control oral anticoagulant therapy. World Health Organ Tech Rep Ser 1983;33:81-105.