UVA1 is skin deep: molecular and clinical implications

Angela Tewari *a, Mette M. L. Grage b, Graham I. Harrison a, Robert Sarkany a and Antony R. Young a
aKing's College London (KCL), King's College London School of Medicine, Division of Genetics and Molecular Medicine, St John's Institute of Dermatology, London, UK. E-mail: angela.tewari@kcl.ac.uk
bDanish Meteorological Institute, Lyngbyvej 100-2100, Copenhagen, Denmark

Received 28th September 2012 , Accepted 21st November 2012

First published on 22nd November 2012


Long wavelength UVA1 (340–400 nm) is the main component of terrestrial UVR and is increasingly used in skin phototherapy. Its damage to critical biomolecules such as DNA has been widely attributed to its ability to generate reactive oxygen species (ROS) via other chromophores. However recent studies in vitro and in vivo have shown that UVA1 has a specific ability to generate cyclobutane pyrimidine dimers (CPD), especially thymine dimers (T<>T), and that this is probably due to direct absorption of UVR. The CPD has been implicated in many aspects of skin cancer. Measuring UVB-induced CPD in the epidermis and dermis in vivo shows that, as expected, the skin attenuates UVB. In contrast, our data show that this is not the case with UVA1: in fact there is more damage with increased skin depth. This suggests that the basal layer, which contains keratinocyte stem cells and melanocytes, is more vulnerable to the carcinogenic effects of UVA1 than would be predicted by mouse models. These data support the continuing trend for better UVA1 protection by sunscreens.

Erythema as a biological measure of exposure to solar UVR

Ultraviolet radiation (UVR) is electromagnetic radiation spanning 100–400 nm and is officially divided into UVC (100–280 nm), UVB (280–315 nm) and UVA (315–400 nm), with UVA being sub-classified into UVA2 (315–340 nm) and UVA1 (340–400 nm). However, a UVB–UVA cutoff at 320 nm is widely used in photodermatology. Since stratospheric ozone absorbs all UVR below ∼295 nm, terrestrial sunlight contains only UVB (5–10% of total UVR) and UVA (90–95% of total UVR), the latter being primarily UVA1 (∼75%). The precise ratio of UVB to UVA varies with the solar zenith angle that is determined by latitude, season and time of day. This is demonstrated by Fig. 1a, which shows the monthly variation of UVA and UVB irradiance at Chilton, UK (51.6°N), in which a radiative transfer model (SMARTS)1 generated the data taking total ozone into account.2 Similarly, Fig. 1b shows the daily variation of UVA and UVB taken in mid-summer (21st June) and mid-winter (21st December) at the same location.
Variation of UVB and UVA irradiance at Chilton, UK (a) monthly at noon on the 21st day of each month (b) daily at summer and winter solstices. These data have been modeled taking total ozone into account.2
Fig. 1 Variation of UVB and UVA irradiance at Chilton, UK (a) monthly at noon on the 21st day of each month (b) daily at summer and winter solstices. These data have been modeled taking total ozone into account.2

Erythema is widely used as a clinical measure of UVR exposure. Thus, the data in Fig. 1a and 1b have been weighted with the CIE erythema action spectrum3 to produce erythemally effective energy (EEE) as shown in Fig. 2a and 2b respectively. Fig. 2a shows that in mid-summer, UVA at temperate latitudes contributes about 25% of EEE of solar UVR. However, this decreases either side of this period such that the ratio is approximately 50[thin space (1/6-em)]:[thin space (1/6-em)]50 from December through to January. Fig. 2b shows that UVA contributes to a maximum of about 25% of EEE at noon in mid-summer, but that in mid-winter the relative contributions of UVB and UVA to erythema are independent of time of day, i.e. erythemal exposure is achieved equally by UVB and UVA. In this context, it must be remembered that considerable molecular and cellular damage can be done in human skin in vivo by single and repeated sub-erythemal exposure,4 irrespective of spectrum. Furthermore, suppression of the skin's immune function can occur with about 25% of the minimal erythema dose (MED).5

Variation of UVB and UVA EEE at Chilton, UK (a) monthly at noon on the 21st day of each month (b) daily at summer and winter solstices. These data are based on the data in Fig. 1.
Fig. 2 Variation of UVB and UVA EEE at Chilton, UK (a) monthly at noon on the 21st day of each month (b) daily at summer and winter solstices. These data are based on the data in Fig. 1.

The standard erythema dose (SED)6 is increasingly used as a measure of human exposure, especially in epidemiological studies. Unlike the MED, the SED is independent of individual UVR sensitivity. During mid-summer in Chilton at midday it would take approximately 9.5 minutes to receive a full UVR spectrum SED (unpublished data) which is approximately 1/3 of a minimal erythema dose (MED) in a skin type I/II person.7 It would take approximately 4 times longer to get an SED from the UVA component alone. These data show considerable potential exposure to UVA whether determined by physical or erythemal exposure parameters.

UVR and skin cancer

There has been a dramatic increase in incidence of skin cancers in Europe and the USA, especially malignant melanoma (MM), in the past 25 years.8,9 This has increased the urgency of identifying and protecting against the causative factors of which UVR has emerged as the most important. This conclusion has resulted from classic epidemiology and more recently, by molecular epidemiology that identifies UVR-specific mutations in skin cancers. The focus has been largely on UVB because of a combination of action spectrum data from a mouse model of squamous cell carcinoma (SCC)10,11 and the well-established finding that UVB readily induces the production of DNA photoproducts (see section below) associated with skin cancer.12–14 However, a combination of factors has arisen in recent years that implies that UVA plays a more significant role than was previously thought. First, epidemiological data have shown that MM shows a better latitude correlation with UVA than with UVB15,16 and that the use of artificial tanning devices (which mainly emit UVA) increases the risk of skin cancer, especially MM.17 UVA artificial tanning devices are widely used,18 especially by the young, and use under the age of 35 confers the greatest risk.19 Second, it has become increasingly clear that UVA1 is not photochemically or biologically inactive, and that UVA1 is a potent inducer of reactive oxygen species (ROS),20 which are thought to play a role in skin cancer.21,22 The question of whether UVA1 is a significant carcinogen has become more important as exposure of the human population to UVA has significantly increased. Until relatively recently, sunscreens were primarily UVB absorbing products that enabled prolonged sunbathing without much protection against UVA, paradoxically increasing exposure to UVA in sunbathers.23,24 This can occur to the extent that erythema from repeated sub-erythemal exposure can be caused by UVA.25 Finally UVA1 phototherapy has been developed in the last 20 years and is used to treat a variety of dermatological diseases26 with comparable efficacy to other types of phototherapy (TLO1 or narrowband UVB) for some conditions. Although the action spectrum for induction of SCC in mice is predominantly in the UVB waveband, the action spectrum for induction of MM in mammalian skin is still unknown. Mechanistically, the proven mutagenicity and carcinogenicity of UVB has led to the dogma that UVB is the only significant cause of skin cancer.

The rest of this review will focus on what is currently known about UVA1 photodamage of DNA, the significance of this damage in terms of mutagenicity and carcinogenicity, and the clinical and public health implications of these new findings.

UVR-induced DNA damage

DNA is susceptible to modification by UVR which may result in mutation if not successfully repaired. There are many different types of DNA photolesions, which show wavelength dependence in their formation. Some are formed by the direct absorption of UVR and others are formed indirectly as described below.

(i) Di-pyrimidine photolesions

UVR is absorbed by skin chromophores27 and DNA pyrimidine bases are primarily chromophores for UVB (thymine, cytosine and the minor 5 methylcytosine),28 but also weakly absorb UVA. The direct excitation of these nucleobases by UVB in an oxygen independent manner induces two main classes of photolesions in the DNA of skin fibroblasts and keratinocytes.29 These are cyclobutane pyrimidine dimers (CPD) and 6-4 pyrimidine pyrimidone adducts (6-4PP) (which make up 65% and 35% of the UVB induced DNA lesions respectively.30,31 The CPD arises by linkage of two adjacent pyrimidine bases of which the T<>T type is the most common.32

Until recently the presence of CPD-induced “fingerprint” mutations (e.g. C→T) in skin cancers was taken as a priori evidence for a causal role for UVB, even though it has been known for some time that UVA, including UVA1, induces CPD in human skin in vivo.33,34 More recent studies have confirmed that UVA1 induces CPD in vitro, ex vivo and in vivo32,35 but not 6-4PP,32,35 these being predominantly (but not exclusively) T<>T at frequencies comparable to or exceeding that of oxidative damage to DNA (see below) but at several orders of magnitude lower efficiency than UVB. The dogma that C→T mutations are only caused by UVB has been recently challenged.36

Distribution of UVB and UVA1-induced CPD in human skin in vivo. Fig. 3 shows the distribution of CPD and 6-4PP in the epidermis and dermis when biopsies were taken immediately after erythemally equivalent does of UVA1 (Fig. 3a) and monochromatic UVB at 300 nm (Fig. 3b); the latter wavelength was chosen because it approximately corresponds to the peak for the action spectra for both erythema and CPD.33Fig. 3b shows that both types of UVB-induced-damage are attenuated with increasing skin depth, as would be expected because of the presence of UVB absorbing chromophores in the skin. In contrast, Fig. 3a shows a significant increase in CPD with skin depth with UVA1 and no evidence for 6-4PP. These figures show that UVB and UVA1 can cause significant DNA damage to dermal cells; such damage has been largely neglected in the past, especially with UVB. Assessments of the epidermis showed that UVA1 induces at least twice as much DNA damage in the basal layer than the upper epidermis.35 Thus, the extent of CPD damage varies with spectrum and epidermal location.
(a) Linear regression for UVA1-induced CPD (p = 0.0006 for slope) and 6-4PP (p = 0.56 for slope) in the epidermis and dermis in vivo immediately after a 3MED exposure. More CPD appear to be induced as depth increases through the epidermis and dermis. Note the lack of UVA1 induced 6-4PP. (b) Linear regression for UVB (300 nm)-induced CPD (p = <0.0001 for slope) and 6-4PP (p = 0.0006 for slope) in the epidermis and dermis in vivo immediately after a 3MED exposure.
Fig. 3 (a) Linear regression for UVA1-induced CPD (p = 0.0006 for slope) and 6-4PP (p = 0.56 for slope) in the epidermis and dermis in vivo immediately after a 3MED exposure. More CPD appear to be induced as depth increases through the epidermis and dermis. Note the lack of UVA1 induced 6-4PP. (b) Linear regression for UVB (300 nm)-induced CPD (p = <0.0001 for slope) and 6-4PP (p = 0.0006 for slope) in the epidermis and dermis in vivo immediately after a 3MED exposure.

UVA1 is less well absorbed by the upper layers of the epidermis than UVB and hence can penetrate deeper into tissue, but the reasons for the “reverse attenuation” with UVA1 are not known. One possibility is that UVA1 photons are preferentially scattered by the epidermis and dermis, in a forward or backward direction, rather than absorbed by chromophores.37,38 Back scattering results in remittance (a type of “reflection”), which provides additional opportunity for chromophore absorption during the return pathway. Dermal remittance increases between 300 and 400 nm.37 Thus, it is possible that the higher number of UVA1-induced CPD seen in the basal layer is due to dermal back scatter (e.g., from collagen), as well as epidermal forward scatter.39

Although we have only measured CPD and 6-4PP, these can be used as a surrogate for UVR penetration into skin and can inform about the possibility of generating other types of DNA and bio-molecule damage. Overall, our data demonstrate that the basal layer, which contains melanocytes and proliferating keratinocytes, is especially sensitive to UVA1 induced DNA damage, and they challenge the paradigm that UVB is the only important spectral region for skin cancer. This is supported by studies on engineered human skin show that, in contrast to UVB, UVA-induced mutations were mainly located in the basal layer.40

The photochemical mechanisms of UVA1 CPD induction. The photochemical mechanisms, by which UVA1 selectively induces CPD, especially T<>T, and not 6-4PP (see Fig. 3a) in vivo, remains unknown. UVA activation of some photosensitizers such as fluoroquinolones41 and carprofen42 can induce CPD in vitro, suggesting that unidentified endogenous photosensitizers in human skin in vivo may have a role in the induction of CPD by UVA1, possibly via photosensitizer mediated triplet energy transfer.43,44 More recently a direct UVR absorption photochemical reaction45,46 has been proposed from in vitro studies. For example, double-stranded base sequences (e.g., dA.dT) increase UVA absorption compared with the same monomeric molecules.46

(ii) Oxidative damage

DNA damage also occurs indirectly through the formation of ROS.44,47 These are generated by the absorption of UVA by non-DNA endogenous chromophores (photosensitizers) such as porphyrins, flavins and NADH/NADPH44,48 which can be excited to a triplet state. Damage can occur via a type 1 photosensitization reaction which can cause DNA strand breaks by the generation of superoxide anions, hydrogen peroxide and hydroxyl radicals, the latter being very reactive with all DNA bases.47 There are also type 2 photosensitization reactions where energy is transferred to molecular oxygen giving rise to singlet O2 (1O2). This species specifically reacts with guanine residues49 producing 8-oxo-7,8-dihydro-2′deoxyguanosine (8oxodG) and is thought to be important in UVA induced cell death.50 Few studies have reported the detection of UVR-induced oxidative damage to DNA in vivo, but this has been reported in mice51 and in human skin.22,52 8oxodG has also been reported in urine after the exposure of human skin to UVA.53

When UVB (300 nm) and UVA1 doses are given to produce comparable levels of erythema in human skin (1MED ∼ 30 mJ cm−2 and ∼50 J cm−2 respectively), UVA1 induces 3–4 fold fewer T<>T than UVB implying other non-DNA chromophores have an important role in UVA1 erythema, and it is possible that this is mediated via oxidative damage to DNA. Unlike UVB erythema, UVA erythema is oxygen dependent,54 implying a role for ROS in UVA erythema. Different mechanisms for UVB and UVA1 erythema are supported by a lack of correlation between UVB and UVA1 induced MED on the same individuals (Fig. 4). A detailed laser action spectrum for human erythema showed a peak at 300 nm but also identified a minor UVA1 peak (at approximately 360 nm)55 which also suggests that more than one chromophore is important (Fig. 5).

Lack of relationship between a given individual's UVB and UVA1 MED (n = 22 with some data points overlapping). jp = just perceptible.
Fig. 4 Lack of relationship between a given individual's UVB and UVA1 MED (n = 22 with some data points overlapping). jp = just perceptible.

Erythema action spectrum55 showing small peak at approximately 360 nm (raw data obtained from the late Dr Anders) normalized at 300 nm with the CIE action spectrum.3
Fig. 5 Erythema action spectrum55 showing small peak at approximately 360 nm (raw data obtained from the late Dr Anders) normalized at 300 nm with the CIE action spectrum.3

Consequences of UVR induced DNA damage in human skin

(i) Non-genetic

The action spectra for CPD and erythema (inflammation) are similar (especially between 280–340 nm) suggesting that DNA is a chromophore for erythema33 which is also supported in studies in the marsupial Monodelphis domestica in which the MED was reduced by a factor of approximately four after enhanced CPD repair induced by UVA activation of endogenous photolyase which is not present in placental mammals.56 In other words the CPD triggers inflammation of the skin. Inflammation plays a role in many types of cancer57,58 by fostering tumour progression, and UVR-induced erythema is a risk factor for MM and possibly BCC.59 Persistent erythema is also found in xeroderma pigmentosum patients who are unable to repair CPD and who are also 2000–10[thin space (1/6-em)]000 times more likely to present with melanomas and non-melanoma type skin cancers.12,60

Apart from erythema, the CPD has been shown to trigger pro-inflammatory cytokine release and immunosuppression that are thought to play a role in skin cancer.61,62 We have recently shown that 3 SED, irrespective of spectrum (including UVA1), is predictive of the suppression of the sensitization phase of the contact hypersensitivity (CHS) response, which is regarded as a model for the immunological events in non-melanoma skin cancer (manuscript in preparation). In conclusion, there is considerable evidence that DNA damage, especially the CPD, causes inflammation/immunosuppression that may play a role in skin cancer. Recently published work also suggested that erythema is predictive of photoageing induced by matrix metalloproteinase 1 (MMP1) via the CPD.63

Oxidative damage and immunosuppression

The CPD and urocanic acid have been identified as possible chromophores for UVR-induced immunosuppression.64,65 However several studies in the mouse66,67 have shown that antioxidants can inhibit UVR-induced immunosuppression, which suggests other possibly UVA absorbing chromophores. In addition, antioxidants have been shown to inhibit mouse photocarcinogenesis.68,69 However, there is no direct evidence that oxidative damage to DNA is a trigger for UVA-induced immunosuppression.

(ii) Genetic

Di-pyrimidine lesions. Di-pyrimidine lesions containing a cytosine are thought to lead to a C→T transition (C:G to A:T transition) which are commonly found in UVR induced skin cancer (SCC, basal cell carcinoma (BCC)),14 and the majority of mutations in a melanoma cell line70 but rarely in non-UVR-induced internal cancers. Thus cytosine-containing photoproducts are thought to be more mutagenic. C→T transitions can be induced by both CPD and 6-4PP. However in mammalian cells, 6-4PP are repaired quickly71,72 whilst the CPD is believed to be the major mutagenic lesion owing to its high level of induction, slow repair by nucleotide excision repair (NER) and efficient replication bypass.73 Transgenic mouse studies have shown that the CPD is much more important for non-melanoma skin cancer than the 6-4PP.74

Faithful NER of CPD is crucial for the prevention of skin cancer. One study on ex vivo skin suggested poorer repair of UVA1-induced CPD compared with those induced by UVB32 but our data did not support this when the epidermis was assessed in total.35 However, a subsequent analysis of repair in the basal layer alone suggests that repair of UVA induced CPD is less efficient than that with UVB (unpublished). UVA can induce a G2/S block in melanocytes and melanoma cells suggesting that the DNA damage induced by UVA can have potent effects as they may not be easily repaired at the basal epidermis.75 Recent work76,77 suggests that UVB initiates melanoma and that both UVB and UVA are involved in the progression of the disease.

ROS-induced lesions. 8oxodG can induce G→T transversions which are potentially mutagenic,78,79 but because ROS-mediated base damage is low compared to direct damage and because this type of damage is rapidly repaired80 the importance of these lesions in skin carcinogenesis is less clear.32,43,81

Oxidative damage to DNA results in what have been termed “UVA fingerprint mutations” via G:C→A:T transversions which have been detected in human SCC and actinic keratosis, especially in the basal layer.22 These were found to be more prominent than C→T, transitions21 but p53 gene mutations do not contain UVA specific T and G transversions implying that although UVA causes oxidative DNA damage, such lesions may not contribute to the generation of p53 mutations.82 Also, the UVA mutation spectrum in mammalian cells does not exhibit a predominance of G:C→T:A transversions83 which, combined with the lack of increase in mutation rate in cells deficient in repair of 8oxodG,84 suggests that other lesions are involved in UVA mutagenesis. New work in mice85 examined UVB and UVA induced DNA damage and their contribution to melanoma. UVB induced melanoma was independent of melanin, but UVA-induced melanoma required melanin. UVA, but not UVB, induced oxidative DNA damage in melanocytes of pigmented mice. These data support other work that suggests that melanocytes are particularly sensitive to UVA.86

Clinical implications of UVA1 DNA photodamage in the skin

As discussed earlier, potential exposure to solar UVA1 is substantial, even in temperate UK climates. Further south, on a summer's day in the south of France the maximum ambient daily UVR dose is ∼22MED and the maximum UVA dose is ∼137 J cm−2,23 of which the majority is UVA1. The accumulation of high UVA1 doses also occurs during the treatment of dermatological skin disorders such as morphea87,88 and atopic eczema89 where on average patients receive cumulative doses of approximately 900 J cm−2 UVA1 (for example 50 J cm−2 3 times a week for 6–8 weeks) and some conditions such as atopic eczema of the hands or cutaneous T-cell lymphoma receiving single doses of up to 100 J cm−2 UVA1.90 The long-term consequences of such exposures are not known. We have shown that repeated daily exposure to sub-erythemal doses of solar simulated radiation (SSR) results in an accumulation of CPD4,25 probably because repair of this lesion is relatively slow. To the best of our knowledge, the effects of repeated UVA1 sub-erythemal exposure on CPD has not been studied.

A recent study91 demonstrated that uncontrolled activation of a major mediator of the Hedgehog pathway signalling can lead to the development of nodular BCC from hair follicle stem cells and superficial BCC-like tumours from the basal cell compartment of the epidermis. Such cells may also thus be vulnerable to UVA1 because of its skin penetration properties.

Increasing recognition of the possible long-term harmful effects of solar UVA exposure and development of better UVA sunscreens is now required by regulatory bodies in Europe and the USA.23 Recent government regulation in the UK and other countries and prohibits the use of sunbeds for those under 18 years of age.


Our data, and those of others, show that the basal epidermis of human skin is especially vulnerable to UVA1-induced CPD, and ROS-induced mutations and therefore suggests that the carcinogenic potential of this spectral region, which is the major UVR component of sunlight, may be much greater than has been estimated for SCC in the albino mouse, which has a very thin epidermis and unlikely to show much evidence of differential UVA1 induced damage in the epidermis.

The UVA1 sensitive basal layer is the location of proliferating keratinocytes and melanocytes. The action spectrum for MM in mammalian skin is unknown, but there are epidemiological data to suggest a greater role for UVA for MM compared to non-melanoma skin cancer, furthermore recent mouse data suggest that melanocyte DNA is especially sensitive to oxidative damage.85 Overall, the data support the use of broad-spectrum sunscreen protection.


The research was funded/supported by the National Institute for Health Research (NIHR) Biomedical Research Centre based at Guy's and St Thomas’ NHS Foundation Trust and King's College London. The views expressed are those of the authors and not necessarily those of the NHS, the NIHR or the Department of Health. Angela Tewari was awarded a medical research council (MRC)/British skin foundation (BSF)/British association of dermatology (BAD) clinical training fellowship during which the above research was completed. This research has also received funding from the European Community's Seventh Framework Programme (FP7/2007–2013) under grant agreement n° 227020.


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