Twilight of the gods? The 'dust veil event' of AD 536 in critical perspective.
'Then it was destroyed by the volcano'
Over the last ten years or so, questions of human-environmental interaction, and particularly the cultural impact of natural disasters, have developed a growing prominence in archaeological research. In their ancient reflection of contemporary social concerns, it is not difficult to understand why these issues have been debated with renewed urgency, and also found their way into popular science writing on the past (Fagan 2000, 2004; Diamond 2005). Natural cause and social effect have been directly linked: for example, in a chain of argument dating back to Fouques work of 1879 (1998), seismic calamity and volcanic eruptions volcanic eruptions
discharging of fumes, dust and lava from volcanoes. They have damaging potential in addition to those of being physically overpowering by the lava flow or the ash or dust fallout. were once regularly blamed for bringing about the 'end' of the Minoan and Mycenaean civilisations, and for generally disrupting the Bronze Age Bronze Age, period in the development of technology when metals were first used regularly in the manufacture of tools and weapons. Pure copper and bronze, an alloy of copper and tin, were used indiscriminately at first; this early period is sometimes called the societies of the region. The proponents of widespread social collapse through long-term environmental dislocation have attracted considerable critique within the archaeological community (e.g. Tainter 2008; Inglis & Pryor 2009; McAnany & Yoffee 2010), emphasising notions of resilience, the potential for ancient civilisations to recover (or not) after substantial environmental impacts. Debatable over-estimates of cultural dissolution following natural disasters have also tended to push the very real consequences of such catastrophes towards the academic fringe, what one might call the 'then it was destroyed by the volcano' school of history (Pomeroy 2008). Several recent collections have emphasised that communities once thought to have been eliminated by natural disasters, or which would once have been assumed to have succumbed, in fact achieve renewed stability relatively soon (e.g. Torrence & Grattan 2002; Grattan & Torrence 2007, with particular reference to the Americas). Accordingly, a more nuanced perspective is now the norm (for recent works on the Aegean see Friedrich 2009; Warburton 2009; Knappett et al. 2011).
Alongside the science-based study of environmental catastrophe, a new emphasis on so-called 'geomythology' has emerged, exploring how understandings of such events may have been articulated through stories of gods, supernatural powers and the cosmos (the term was coined by Vitaliano in 1968; see also Piccardi & Masse 2007). The concept of geomythology has clear problems, inherent in its central attempt to link the hard science of environmental cause and effect with the humanities-based study of oral tradition and epic literature (e.g. Baillie 1998; contra Buckland et al. 1997). These include the serious risk of circular argument and 'confirmation bias' (Rundkvist 2011). The addition of archaeology to the mix provides further complications through an attempt to assess social response articulated in material culture. However, the limitations of certain case studies are no reason to reject all the others, and with sensible caution the principle remains both logical and viable in its historical utility.
Conscious of these debates, we here examine a specific event of this kind, the so-called 'dust veil' of AD 536, and critically explore its interpretation from a range of interdisciplinary perspectives. By way of explanatory example, we then present a number of new conclusions about its impact and possible geomythological legacy within a single region--in some ways the least-studied of the many areas affected--namely Scandinavia.
The dust veil event of AD 536: textual scholarship and the environmental sciences
The first observations of what scientists later termed the 'dust veil' appear in a number of Late Antique sources dating to the same time (Arjava 2006). The most detailed and dramatic description comes from the Roman official Cassiodorus, writing outside Ravenna, in whose Variae we read of "something coming at us from the stars" that produces a "blue-coloured sun", dims the full moon and results in "a summer without heat ... perpetual frost ... unnatural drought". The crops wither in the fields, nothing grows and all the while "the rays of the stars have been darkened". With almost scientific observation he records some kind of opacity apparently very high in the stratosphere, narrating how "things in mid-space dominate out sight" and describing how a cloudy mist "condensed by some sort of mixture.., permits neither the natural colours, nor the heat of the heavenly bodies to penetrate". Most significantly, "this has not happened in the momentary loss of an eclipse, but has assuredly been going on equally through almost the entire year" (all quotes from Barnish 1992: 179-80). Similar descriptions of a prolonged celestial darkness, unseasonal chili and failed harvests are found in the securely-dated and independently-created works of Procopius, Zachariah of Mytilene, John the Lydian and John of Ephesus John of Ephesus (ĕf`əsəs), c.505–c.585, Syrian Monophysite historian, bishop of Ephesus. He became a leader of the Monophysites (see Monophysitism), and Byzantine Emperor Justinian, whose favor he enjoyed, set him over the (Arjava 2006). Again, they all relate how the sun was so obscured over the Mediterranean and the Near East that it hardly cast a shadow from the beginning of AD 536 to the end of summer AD 537. Even Mesopotamia experienced frost and snow in the summer of AD 536.
A powerful confirmation of the effects of the dust veil can be found in a series of fossil tree-rings that indicate how the summers in the northern hemisphere, from Siberia in the east all the way to the western United States Noun 1. western United States - the region of the United States lying to the west of the Mississippi River
Santa Fe Trail - a trail that extends from Missouri to New Mexico; an important route for settlers moving west in the 19th century , were unusually cold from AD 536-545, in places even until AD 550. In eastern Siberia Eastern Siberia is a part of Siberia that incorporates the territory located between the Yenisei River in the west and the Pacific Ocean divides in the east. Its area is equal to 7.2 million sq. km. and northern Sweden the average summer temperature has been estimated to have dropped by 3--4 degrees centigrade centigrade /cen·ti·grade/ (sen´ti-grad) having 100 gradations (steps or degrees); see under scale.
Celsius. , a dramatic worsening of the climate. However, this data also seems to indicate that there were in fact two clearly separate periods of severe climatic downturn, the first in AD 536 and the second in AD 540-542, with fewer cold periods in between (the tree-ring data is debated in Briffa et al. 1990, 1992; Baillie 1994, 1995: 84-93, 1999, 2008, 2010; d'Arrigo et al. 2001a, 2001b; Grudd et al. 2002; Grudd 2006; Salzer & Hughes 2007).
Whether or not its effects endured or were repeated, for as long as 15 years, all sectors of the research community agree today that in AD 536 something drastic occurred to affect the global environment, reflected in so many proxies as to leave no doubt that it was a widespread catastrophic event. Its consequences varied geographically in their severity and longevity, and also in the degree to which they have left a mark in the textual and archaeological record The archaeological record is a term used in archaeology to denote all archaeological evidence, including the physical remains of past human activities which archaeologists seek out and record in an attempt to analyze and reconstruct the past. .
What caused the AD 536 event?
In the early 1980s the American geoscientists Stothers and Rampino began to search the Classical sources for descriptions of volcanic eruptions, in order to compare them with data from the natural sciences (Stothers & Rampino 1983; Stothers 1984). Over the next decade these accounts were then linked with information on the ice-cold summers that occurred in China, amongst other places, during the years AD 536-538, which caused widespread ruined harvests and starvation (Rampino et al. 1988; Baillie 1994, 1999; Gunn 2000). Stothers and Rampino felt able to make connections with a significant layer of sulphuric acid sulphuric acid: see sulfuric acid. in the Greenland ice from around the year AD 540, which they suggested derived from a violent volcanic eruption some years earlier (Stothers & Rampino 1983; Stothers 1999). Later investigations of major deposits of sulphates in the ice of both Antarctica and Greenland seemed to confirm this presence of sulphuric Sul`phu´ric
a. 1. Of or pertaining to sulphur; as, a sulphuric smell s>.
2. (Chem.) Derived from, or containing, sulphur; specifically, designating those compounds in which the element has a higher aerosols, which were argued to have come most plausibly from a volcanic super-eruption that probably occurred in the tropics tropics, also called tropical zone or torrid zone, all the land and water of the earth situated between the Tropic of Cancer at lat. 23 1-2°N and the Tropic of Capricorn at lat. 23 1-2°S. , still circulating in the stratosphere over the entire globe for several years after AD 536 (Traufetter et al. 2004; Larsen et al. 2008). This would have resulted in much of the sun's warmth being reflected upwards, with a consequent serious cooling of the earth's surface. Over the last three decades various candidates for the volcano have been proposed, including sites in Papua New Guinea Papua New Guinea (păp`ə, –y (Stothers 1984) and Java (Keys 1999). Recent work by Dull et al. (2010) suggests a link with a massive eruption in EI Salvador, pyroclastic py·ro·clas·tic
Composed chiefly of rock fragments of volcanic origin.
Composed chiefly of rock fragments of explosive origin, especially those associated with explosive volcanic flows from which have been shown to have killed trees in AD 535.
The original supposition of a 'nuclear winter' enduring over several years caused by a single massive eruption is now thought increasingly unlikely by volcanologists (Grattan, J. pers. comm.). Volcanic dust falls from the stratosphere relatively quickly and the volume of water vapour also limits the quantity of sulphur that can be oxidised into an aerosol, the latter being the most powerful mechanism for climate change. However, even allowing for the full range of academic debate, the causative options are not numerous: the dust veil must have resulted either from one or more volcanic eruptions of unusual magnitude; from one or more extraterrestrial impacts, involving whole or fragmentary comets and/or meteorites; or from some combination of these. The latter possibility is important, because the 'event' usually discussed in the singular may in fact have represented the cumulative effects of several events occurring within a short space of time, perhaps in different places. This is particularly relevant to the medium-term impact, and what seems to have happened to the climate in various parts of the world for several years after AD 536.
However, while the location and nature of the event(s) remain unclear, the existence of extreme weather phenomena in and after AD 536 is unquestionable. Our primary purpose in this paper is to examine the issue from the perspective of the humanities. Put simply, the reasons for the solar darkness of AD 536 do not necessarily need to matter more to students of its consequences than they did to those actually experiencing them. At a human level, if your harvests have failed and your family faces starvation then you have other priorities than knowing precisely why the summer has turned to winter (though as time goes on you may begin to invent reasons, or adopt those given you by others). Arguments put forward by the advocates of volcanoes, comets and asteroids have their own contested validity, but do not substantially affect archaeological and textual research into how the people of the mid sixth century reacted to whatever it was that had happened. This is our subject here, and one we offer as a critical counterpoint to the polarised environmental discussion of the AD 536 event(s).
The archaeology of the Fimbulwinter
The consequences of the dust veil as they can be read through dendochronology strongly imply a pattern of intermittently colder summers and a shorter growing season growing season, period during which plant growth takes place. In temperate climates the growing season is limited by seasonal changes in temperature and is defined as the period between the last killing frost of spring and the first killing frost of autumn, at which , colder winters, increased humidity and stormier weather. But cold winters as such have never been a difficulty for low-tech agrarian societies in the northern hemisphere. The overbearing problem has been cold summers. It has long been known that large areas of agricultural land in northern and central Europe Central Europe is the region lying between the variously and vaguely defined areas of Eastern and Western Europe. In addition, Northern, Southern and Southeastern Europe may variously delimit or overlap into Central Europe. returned to forest during the middle and later sixth century, the so-called 'Migration Period Crisis', but the data has not been previously placed into a larger environmental context. In many regions four to seven generations would pass before the cultural landscape returned to its former dimensions (Welinder 1975; Andersen & Berglund 1994; Berglund et al. 1996; Behre et al. 1996; Vervruggen et al. 1996; Bork et al. 1998; Berglund 2003). It is hard to avoid interpreting this general and surprisingly sudden woodland advance as the expression of a dramatic agricultural decline, which would surely have caused a similarly marked reduction in population with long-term effects.
Of necessity in a brief paper of this kind, much of the supporting data must be generalised, but by way of example we can take one detailed regional study. In eastern central Sweden during the AD 500s, the majority of villages were abandoned, with new settlements later founded in drastically reduced numbers on slightly higher ground nearby. This constituted the greatest change in settlement patterns in Sweden for 6000 years. The complete data for Uppland province, some 86 sites, have recently been brought together from a trawl trawl - To sift through large volumes of data (e.g. Usenet postings, FTP archives, or the Jargon File) looking for something of interest. of the grey literature as part of the massive excavation project for the new E4 motorway north of Uppsala, now published in six volumes. In an overview of the settlement evidence from all periods, Hans Gothberg notes (2007: 440) that the total number of occupied sites across the province falls by a staggering 75 per cent during the sixth century. This is all the more striking when the data is displayed visually (Figures 1 & 2) and it is clear that the agrarian economy was actually expanding in the centuries prior to the collapse, which appears to have happened suddenly. In many cases, the settlements abandoned at this time had been in continuous use for more than 1000 years.
As a comparison to the settlement data, Daniel Lowenborg (2010: paper V, and in press) has looked at graves in Vastmanland province, adjacent to Uppland in the central part of the country, and found an identical pattern. Figure 3 shows the dated periods of use for every excavated prehistoric cemetery in Vastmanland, a total of 65 sites. With only five exceptions, all the grave-fields that had been in continuous use since the pre-Roman Iron Age (and some began even earlier) were abandoned during the sixth century. We do not have more precise dating than this in most instances, but again it is clear how a millennium or more of tradition came to an end across the province. This may have been either a sudden or a gradual process, but in any event it occurred over a period of less than 100 years. As these burial grounds went out of use, a range of entirely new cemeteries were founded in previously unoccupied locations, and it is these that developed through the Vendel and Viking periods until--and in some cases beyond--the adoption of Christianity. Moving in from the macro-scale of provinces, one can also trace the same cycle of contraction and dislocation at individual sites. A good example is Torun Zachrisson's 2011 archaeological review of the royal power centre at Gamla Uppsala Gamla Uppsala ("Old Uppsala") is a parish and a village outside Uppsala in Sweden. It had 16,231 inhabitants in 1991.
As early as the 3rd century AD and the 4th century AD and onwards, it was an important religious, economic and political centre. , where she notes that the climate catastrophe coincides with the transformation of the agrarian landscape as exactly as our current dating allows (Zachrisson 2011: 146).
The same phenomenon is demonstrated all across central Sweden by Renck (2008), with clear parallels elsewhere in the northern provinces of Halsingland and Medelpad, and even as far south as Smaland near the Danish border. This picture is also replicated consistently over the rest of Scandinavia for which we have data. As confirmation of population decline, the period immediately following these events in Sweden and Norway has generally produced very few indications of settlements, graves, material culture, iron production and fortifications, by comparison with the periods both before and after (see Graslund 2004, 2008 for all these regions). In several areas of southern Norway the number of known burial finds after AD 536-545 are 90-95 per cent fewer than in the period before (Solberg 2000: 180-82, 197-98).
The situation is, if anything, even worse on the small Baltic island societies of Oland and Gotland. Over 1300 Iron Age house foundations have been recorded on Oland, all apparently abandoned in the sixth century (Stenberger 1933; Fallgren 2006), while on Gotland at least 1900 similar deserted structures have been documented (Carlsson 1979). A handful of village sites have been excavated in their entirety, bringing the picture into sharper focus. One such is Vallhagar in eastern Gotland (Stenberger 1955; Figure 4), a prosperous community that came to a violent end in a single event in the mid sixth century when the village was burned, with bodies still left lying in some of the houses. Similar destruction seems to have swept over the Oland ring-forts and many other sites, with an increase in fortified fortified (fôrt´fīd),
adj containing additives more potent than the principal ingredient. refuges at the same time (Herschend 2009 gives a good overview of these social processes).
[FIGURE 1 OMITTED]
Ruined harvests and grazing for two years in a row, combined with several cold summers and shorter growing seasons for a further decade, would have led unavoidably to serious famine in archaic agricultural societies. It seems reasonable to suggest that the populations of Scandinavia in the mid sixth century may have been halved. As if this were not enough misery, the climate disaster may have unleashed the Justinian pandemic pandemic /pan·dem·ic/ (pan-dem´ik)
1. a widespread epidemic of a disease.
2. widely epidemic.
Epidemic over a wide geographic area.
n. that reached Western Europe Western Europe
The countries of western Europe, especially those that are allied with the United States and Canada in the North Atlantic Treaty Organization (established 1949 and usually known as NATO). in AD 541, with drastic effects on the peoples of the southern and central continent (Little 2006; Rosen 2006: 201-203). It should also be noted that DNA DNA: see nucleic acid.
or deoxyribonucleic acid
One of two types of nucleic acid (the other is RNA); a complex organic compound found in all living cells and many viruses. It is the chemical substance of genes. from the plague bacillus bacillus (bəsĭl`əs), any rod-shaped bacterium or, more particularly, a rod-shaped bacterium of the genus Bacillus. Some bacterium in the genus cause disease, for example B. Yersinia pestis Yersinia pes·tis
A bacterium that causes plague and is transmitted from rats to humans by the rat flea Xenopsylla cheopis. Also called Pasteurella pestis. has now been identified in contemporary skeletal material from southern Germany and France (Wiechmann & Grube 2005; Drancourt et al. 2007).
[FIGURE 2 OMITTED]
On this broad canvas of social unrest and sharp agrarian decline, Lowenborg (2010, in press) uses Klein's 2007 work on the opportunities generated by crises to discuss how some sectors of Swedish society may have taken advantage of a demographic disaster. It may be that the events of the mid sixth century were critical for the development of the strikingly different political economies of the later Iron Age, manifested in new types of monumentalised cemeteries and settlements, in new locations, and thus formed one catalyst for the long social trajectory that ultimately resulted in the Viking diaspora and the transformation of the North.
[FIGURE 3 OMITTED]
[FIGURE 4 OMITTED]
The Danish archaeologist Morten Axboe was the first in Scandinavia to consider the possible impact of the AD 536 event(s) in relation to the 'Migration Period Crisis'. In several papers, and especially in a chapter of his doctoral dissertation, he outlined a suggestion that the large numbers of 'sacrificial' gold deposits in Scandinavia from the sixth century may be connected with the solar disaster; he also made a link with the Norse myth of the Fimbulwinter (Axboe 1999, 2001a, 200lb, 2004, 2005, 2007: ch. 9). At the time, Axboe was a lone voice on this subject in the North, and his work was both brave and challenging, but the link between the bracteate finds and the dust veil event is now being taken up regularly. One example is Kent Andersson's work (2011: 94-107) on the Soderby hoard from Uppland province, Sweden, which appears to date from this time. Here, the bracteate images, usually interpreted as representing the gods, have been defaced and mutilated, as if their power was rejected for some reason.
Following the publication of the new environmental data noted above, one of us (BG) has recently taken this Fimbulwinter connection further to argue that the information from the Late Antique textual sources has a detailed counterpart in these Norse traditions of the Ragnarok--the final battle at the end of the worlds (Graslund 2008, 2009; see also Hultgard 2004), and that this may reflect the archaeological material from the mid sixth century. We can now examine these claims in more depth.
The evidence of Old Norse poetry Old Norse poetry encompasses a range of verse forms written in Old Norse, during the period from the 8th century (see Eggjum stone) to as late as the far end of the 13th century.
The exact date of composition for the corpus of mythological poetry that forms our current foundation for pre-Christian Norse beliefs has long been debated. In the shape that we currently have them, it seems that the earliest poems were finally put into order around the turn of the first millennium AD, before being committed to vellum vellum: see parchment. some 150-200 years later. That said, it is equally clear that they are merely the end result of centuries of addition and reworking, and that they contain numerous elements that go back to at least the fifth century. Among the narratives that thus emerge are several stories of Migration Period warriors both in Scandinavia and beyond (Attila was particularly popular), all known and confirmed from other contemporary sources. In other poems, such as Voluspa ('The Seeress's Prophecy'), it has long been argued that almost all the material culture described is of pre-Viking, sixth-century date (first proposed in Nerman 1958, 1963). The notion that these poems might preserve some memory of an event like the AD 536 disaster is therefore entirely consistent with the current interpretations of these texts.
Gylfaginning ('The Tricking of Gylfi') forms a major component of Snorri Sturluson's Edda, an early thirteenth-century Icelandic text that not only served as a kind of handbook for medieval poets but also forms one of our main sources on Norse mythology. In section 51 of the text is a brief account of traditions relating to relating to relate prep → concernant
relating to relate prep → bezüglich +gen, mit Bezug auf +acc the fimbulvetr, the 'great' or 'mighty' winter that serves as a forewarning of the Ragnarok, the destruction of all the worlds and their inhabitants, even the gods themselves. It is told how the mythical king Gylfi visits the AEsir gods and enters a hall where three men are seated. He asks them what they know about the Ragnarok. One of them answers:
First of all that a winter will come called Fimbulwinter. Then snow will drift from all directions. There will then be great frosts and keen winds. The sun will do no good. There will be three of these winters together and no summer between (Faulkes 1987: 52-53).
In strophes 39-40 and 54 of Voluspa it is indicated that the Ragnarok begins when the children of the wolf Fenrir carry off the moon, attack the sun and paint the home of the gods red with their blood. It also says that the sun's rays are dark and the stars are no longer visible in the following (i.e. at least two) summers, and that the weather is out of balance. This is in agreement not only with Gylfaginning (and other Norse mythological texts) but also with the Classical sources.
Note that these are clear descriptions of specific weather conditions, including their appearance, duration and precise effects--very far from the generic end-of-the-world stories found in many mythologies, accounts of severe but nonetheless rather vague destruction. The core of the Norse stories can be confidently dated to the later Iron Age (c. AD 5501000), and as noted above there are many circumstantial references that support a mid sixth century context for the material culture that they describe.
It is probable that sudden changes observed in the iconography of stone monuments also relate to the sixth-century event. The Gotland picture stones are monumental grave markers and memorials carved with symbols and figurative images that are often linked to the cycles of Norse mythology (Lindqvist 1941-42). During the fifth and early sixth centuries the stones commonly feature a large whirling disc as the primary image, interpreted as the sun on the basis of many centuries of Scandinavian parallels going back to the Bronze Age, and seen as evidence of a long-held prehistoric solar cult (Kaul 2004; Figure 5). In the sixth century the whirling disc disappears completely, and is replaced by symbols that seem to relate more directly to the stories of gods and heroes that we know from the Viking Age
There is nothing to suggest any textual collusion between the Northern myths and the Late Antique sources, and that the textual, vulcanological, dendrochronological, palaeobotanical and archaeological source categories are independent of one another further reduces the possibility of circular argument. If we follow Zachariah of Mytilene and see the darkening of the sun beginning in early March of the year AD 536, and place its approximate end in September AD 537, we have a period of 18-19 months when the sun was powerfully misted over and winter weather prevailed during the European summer. Whatever was in the stratosphere was almost certainly of variable thickness and longevity in different areas and latitudes. If it thinned out slowly, it cannot have been easy for the people of the time to say when exactly the sun returned to normal. In northern latitudes with naturally weaker sunlight, the clouded sun was probably experienced for rather longer than in the south.
Serious, if intermittent, reductions in summer temperatures for as long as 10-15 years must have reduced evaporation and probably increased rainfall (Buntgen et al. 2011). At this time the water levels rose in Swedish lakes and watercourses, and in many bogs, which indicates a higher water table and increased humidity. At the same time the water temperature fell in the North Atlantic (Jansen & Koc 2000). These conditions are matched by John the Lydian's description of extremely humid conditions in Europe (Arjava 2006). In eastern central Sweden the majority of villages of this period lay on the clay soils near wetlands and watercourses, before moving as we have seen in the mid sixth century to higher and drier ground nearby. The catalyst for this may have been problems with rising groundwater, overflowing rivers and the damage to timber buildings arising from damp and mould that spread with the humidity.
Such a lengthy catastrophe must naturally have generated suspicion of the gods' ability to control the environment, and suggested that they were destined for the same unfortunate fate as mortals. Whatever its cause(s), the abnormally long dust veil of AD 536-537, with its blood-red sunsets, ice-cold summers, chill winters and serious famine must have been experienced as a frightening foretaste fore·taste
1. An advance token or warning.
2. A slight taste or sample in anticipation of something to come.
tr.v. of the world's ending. But when this did not happen and the sun actually returned, perhaps the terrifying memory was instead woven into an imagined image of a coming destruction, the Ragnarok, which long thereafter held sway over the Northern peoples as their own version of Apocalypse. The final scenes of the Ragnarok myth, when sun, earth, gods and humans are resurrected in a paradisiacal milieu, can be interpreted as a reflex of the happy moment when warmth returned after the Fimbulwinter, and a new, hopeful time of light opened up for those who had survived.
There is one final but compelling piece of evidence. As we have seen, in Voluspa we find the term Ragnarok used for the battle at the end of the worlds, but Snorri's Edda has the alternative form ragnarokkr. Early scholars of Old Norse Old Norse
1. The North Germanic languages until the middle of the 14th century.
a. Old Icelandic.
b. Old Norwegian.
Noun 1. interpreted this to mean 'twilight of the gods', hence Wagner's famous Gotterdammerung that the tales inspired (Mullenhoff 1873). This reading was dismissed by later research, and modern textual scholars usually interpret the Ragnarok to refer to the 'end' of the gods (Holtsmark 1968). However, as Bernhardsson (2007) has recently shown, the is in risk is a neutral wa-stem, suggesting the substantive rok(k) or rek(k), 'darkness', and the strong associated verb rok(k)va, rek(k)va with no other meaning than 'darken'. The old reading of the gods' 'twilight' or 'darkness' is thereby not only now again shown to be more likely, but in fact forms a perfect literal description of the long eclipse that not even the highest powers were able to avert.
[FIGURE 5 OMITTED]
The traditions of the sun and moon's disappearance in the Fimbulwinter and Ragnarok have generally been interpreted as purely mystical in nature. But when they are relocated in a broader context of natural history and archaeology, and re-read in the light of Late Antique sources, their obscurities are removed. Instead, what appears is actually a remarkably clear and consistent image.
In the above discussion, we are not arguing that the late Iron Age cultures of the North were 'destroyed by the volcano' (or the comet, or the asteroid, singular or plural). In avoiding such exaggerated simplifications, it is nonetheless important to observe that the dust veil really happened and does seem to have had a very considerable socio-cultural impact. In the present paper we have noted some of the archaeological markers for the damage within just one specific region, Scandinavia. With its lower margins of agricultural resilience, the North can also serve as a useful laboratory of the more drastic effects that really can follow environmental impact. The social effects of the episode can also be seen in the period of recovery. In the Scandinavian late Iron Age, we can clearly observe new structures of power with an increased focus on elite ownership of land. This may perhaps have been provoked by the fact that, in the middle of the sixth century, large areas of agricultural soil were suddenly left without obvious occupants.
We believe that several categories of independent data combine to suggest that the Old Norse traditions of the Fimbulwinter and Ragnarok may collectively remember terrifying experiences of starvation and collapse as a result of extreme weather phenomena during the years AD 536-550.
The terrible Fimbulwinter must have lived long in Northern folk memory Folk memories is a term sometimes used to describe stories, folklore or myths about past events that have passed orally from generation to generation. The events described by the memories may date back tens, hundreds, or even thousands of years and often have a local significance. , and been retold re·told
Past tense and past participle of retell. , sung and embellished with mystical interpretation. When a tradition like this is based on a completely mutual external experience, where there was no doubt in people's mind as to what happened, it would have long been impossible to embroider em·broi·der
v. em·broi·dered, em·broi·der·ing, em·broi·ders
1. To ornament with needlework: embroider a pillow cover.
2. the story in an unrealistic manner. Only when explaining why the sun, moon and stars disappeared and at last returned was there room for the poetic fantasy of myth.
For their discussion and assistance, we would like to thank Anders Andren, Morten Axboe, Bjorn Berglund, Francois-Xavier Dillmann, Bjorn Gunnarson, Hans Gothberg, Frands Herschend, Anders Hultgard, Daniel Lowenborg, Heimir Palsson, Linda Qvistrom, Olof Sundqvist, Henrik Williams and Torun Zachrisson. We are also grateful to Mike Baillie Not to be confused with Mike Baillie, drummer of The Skids
Dr Mike Baillie is a Professor Emeritus of Palaeoecology in the School of Archaeology and Palaeoecology at Queen's University of Belfast in Northern Ireland. , John Grattan and two anonymous referees for their comments to an earlier version of this paper.
ANDERSEN, S.T. & B.E. BERGLUND. 1994. Maps for terrestrial non-tree pollen (NAP) percentages in north and central Europe 1800 and 1450 yr BP. Palaoklimaforschung 12: 119-134.
ANDERSSON, K. 2011. Guldalder. Uppsala: Balderson.
ANDREN, A. 2012. Fragments of world-views. Archaeological studies of Old Norse cosmology. Lund: Nordic Academic Press.
ARJAVA, A., 2006. The mystery cloud of the year 536 CE in the Mediterranean sources. Dumbarton Oaks Papers Dumbarton Oaks Papers (DOP) is an academic journal founded in 1941 for the publication of articles relating to civilizations of the late antique, early medieval, and Byzantine periods. 2005: 73-94.
D'ARRIGO, R., G. JACOBY, D. FRANK, N. PEDERSON, E. COOK, B. BUCKLEY, B. NACHIN, R. MIJIDDORJ & C. DUGARJAV. 200la. 1738 years of Mongolian temperature variability inferred from a tree-ring width chronology of Siberian pine The Siberian Pine (Pinus sibirica; family Pinaceae) is a species of pine tree that occurs in Siberia from 58°E in the Ural Mountains east to 126°E in the Stanovoy Khrebet mountains in southern Sakha Republic, and from Igarka at 68°N in the lower Yenisei valley, south . Geophysical Research Letters Geophysical Research Letters is a publication of the American Geophysical Union. GRL is the organization's only letters journal. Since its introduction in 1974, GRL has published only short research letters, typically 3-5 pages long, which focus on a specific discipline or 28(3): 543-46.
D'ARRIGO, R., D. FRANK, G. JACOBY & N. PEDERSON. 2001 b. Spatial response to major volcanic events in or about AD 536, 934 and 1258: frost rings and other dendrochronological evidence from Mongolia and northern Siberia. Climatic Change Climatic Change is a journal published by Springer. Climatic Change is dedicated to the totality of the problem of climatic variability and change - its descriptions, causes, implications and interactions among these. 49: 239-46.
AXBOE, M. 1999. The year 536 and the Scandinavian gold hoards. Medieval Archaeology The study of humankind through its material culture, specialising in the period of the European Middle Ages. At its broadest, the period stretches from the 5th to the 16th century CE and refers to post-Roman but pre modern remains. 43: 186-88.
--2001a. Aret 536. Skalk 4: 28-32.
--2001b. Amulet amulet (ăm`yəlĭt), object or formula that credulity and superstition have endowed with the power of warding off harmful influences. pendants and a darkened sun, in B. Magnus (ed.) Roman gold and the development of the early Germanic kingdoms: 119-136. Stockholm: Royal Academy of Letters, History and Antiquities.
--2004. Die Goldbrakteaten der Volkerwanderungszeit: Herstellungsprobleme und Chronologie. Berlin: de Gruyter.
--2005. Guld og guder, in T. Capelle & C. Fischer (ed.) Ragnarok: Odins verden: 41-56. Silkeborg: Silkeborg Museum.
--2007. Brakteatstudier. Copenhagen: Royal Society of Northern Antiquaries.
BAILLIE, M.G.L. 1994. Dendrochronology dendrochronology: see dating.
Method of scientific dating based on the analysis of tree rings. Because the width of annular rings varies with climatic conditions, laboratory analysis of timber core samples allows scientists to raises questions about the nature of the AD 536 dust-veil event. The Holocene 4/94: 212-17.
--1995. A slice through Verb 1. slice through - move through a body or an object with a slicing motion; "His hand sliced through the air"
go, locomote, move, travel - change location; move, travel, or proceed, also metaphorically; "How fast does your new car go?"; "We time. Dendochronology and precision dating. London: Batsford.
--1998. Bronze Age myths expose archaeological shortcomings? A reply to Buckland et al. 1997. Antiquity 72: 425-27.
--1999. Exodus to Arthur. Catastrophic encounters with comets, London: Batsford.
--2008. Proposed re-dating of the European ice core chronology by seven years prior to the 7th century AD. Geophysical Research Letters 35: L15813. doi: 10.1029/2008GLO GLO Global
GLO General Land Office
GLO Greek Life Office
GLO General Learner Outcomes
GLO GLO Lounge Orlando
GLO Good Looking Organisation Ltd. (music production)
GLO Get the Lead Out
GLO Gospel Literature Outreach 34755.
--2010. Volcanoes, ice-cores and tree-rings: one story or two? Antiquity 84:202-215.
BARNISH, S.J.B. (ed. & tr.) 1992. The Variae of Magnus Aurelius Cassiodorus Senator. Liverpool: Liverpool University Press.
BEHRE, K.-E., A. BRANDE, H. KUSTER & M. ROSCH. 1996. Germany, in B.E. Berglund, J.B. Birks & M. Ralska-Jasiewiczowv (ed.) Palaeoecological events during the last 15 000 years: 507-551. Chichester: Wiley.
BERGLUND, B.E. 2003. Human impact and climate changes--synchronous events and a causal link? Quaternary quaternary /qua·ter·nary/ (kwah´ter-nar?e)
1. fourth in order.
2. containing four elements or groups.
1. Consisting of four; in fours. International 105/1: 7-12.
BERGLUND, B.E., J.B. BIRKS & M. RALSKAJASIEWICZOWV (ed.). 1996. Palaeoecological events during the last 15 000 years. Chichester: Wiley.
BERNHARDSSON, H. 2007. Old Icelandic Old Icelandic
Icelandic from the middle of the 12th to the middle of the 16th century.
Noun 1. Old Icelandic - the extinct dialect of Old Norse that was spoken in Iceland up until about 1600 ragnarok and ragnarokkr, in A.J. Nussbaum (ed.) Verba docenti. Studies in historical and Indo-European linguistics presented to Jay H. Jasanoff by students, colleagues, and friends: 25-38. Ann Arbor Ann Arbor, city (1990 pop. 109,592), seat of Washtenaw co., S Mich., on the Huron River; inc. 1851. It is a research and educational center, with a large number of government and industrial research and development firms, many in high-technology fields such as (MI): Beech Stave Press.
BORK, H.R., H. BORK, C. DALCHOW, B. FAUST, H.P. PION & T. SCHATZ. 1998. Landschaftsentwicklung in Mitteleuropa. Wirkungen des Menschen auf Landsehaften. Gotha: Klett Perthes.
BRIFFA, K.R., T. BARTHOLIN, D. ECKSTEIN, P.D. JONES, W. KARLEN, F.H. SCHWEINGRUBER & P. ZETTERBERG. 1990. A 1400-hundred tree-ring record of summer temperatures in Fennoscandia. Nature 346: 434-39.
BRIFFA, K.R., P.D. JONES, T. BARTHOLIN, D. ECKSTEIN, F.H. SCHWEINGRUBER, W. KARLEN, P. ZETTERBERG & M. ERONEN. 1992. Fennoscandian summers from AD 500: temperature changes on short and long time scales. Climatic Dynamics 7: 111-19.
BUCKLAND, P., A.J. DUGMORE & K.J. EDWARDS. 1997. Bronze Age myths? Volcanic activity and human response in the Mediterranean and North Atlantic regions. Antiquity 71: 581-93.
BUNTGEN, U., W. TEGEL, K. NICOLUSSI, M. McCoRMICK, D. FRANK, V. TROUET, J.O. KAPLAN, F. HERZIG, K-U. HEUSSNER, H. WANNER, J. LUTERBACHER & J. ESPER. 2011. 2500 years of European climate variability and human susceptibility. Science doi: 10.1126/science.1197175.
CARLSSON, D. 1979. Kuhurlandskapets utveckling pa Gotland: en studie av jordbruks- och bebyggelseforandringar under jarnaldern. Stockholm: Stockholm University Stockholm University (Stockholms universitet) is a state university in Stockholm, Sweden. It has about 37,000 students studying at four faculties. History
In 1878, the university college Stockholm högskola .
DIAMOND, J. 2005. Collapse: how societies choose to fail or survive. London: Allen Lane.
DRANCOURT, M., M. SIGNOLI, L.V. DANG, B. BIZOT, V. ROUX Roux , Pierre Paul Émile 1853-1933.
French bacteriologist. His work with the diphtheria bacillus led to the development of antitoxins to neutralize pathogenic toxins. , S. TZORTIS & D. RAOULT. 2007. Yersinia pestis orientalis in remains of ancient plague patients. Emerging infectious diseases. Available at: http://www.cdc.gov/EID/content/13/2/332.htm (accessed 23 Jan 2012).
DULL, R., J.R. SOUTHON, S. KUTTEROLF, A. FREUNDT, D. WAHL & P. SHEETS. 2010. Did the TBJ TBJ Trial by Jury
TBJ Toronto Blue Jays (Major League baseball team)
TBJ Terrain Bounce Jamming
TBJ Turbulent Bounded Jet Ilopango eruption cause the AD 536 event? American Geophysical Union Fall Meeting Abstracts. Bibcode 2010AGUFM.V13C2370D.
FAGAN, B. 2000. The Little Ice Age: how climate made history 1300-1850. New York New York, state, United States
New York, Middle Atlantic state of the United States. It is bordered by Vermont, Massachusetts, Connecticut, and the Atlantic Ocean (E), New Jersey and Pennsylvania (S), Lakes Erie and Ontario and the Canadian province of : Basic Books.
--2004. The long summer: how climate changed civilization. New York: Basic Books.
FALLGREN, J.-H. 2006. Kontinuitet och forandring: bebyggelse och samhalle pa Oland, 200-1300 eKr. Uppsala: Uppsala University Uppsala University (Swedish Uppsala universitet) is a public university in Uppsala, Sweden, 64 kilometres (40 miles) north-northwest of Stockholm. Founded in 1477, it claims to be the oldest university in Scandinavia, outdating the University of Copenhagen Press.
FAULKES, A. (tr.) 1987. Snorri Sturluson Snorri Sturluson or Sturleson (snôr`rē stür`lüsôn, –lĕsôn) , Edda: Prologue and Gylfaginning. Oxford: Oxford University Press.
FOUQUE, F. 1998 . Santorini and its eruptions. Baltimore (MD): Johns Hopkins University Johns Hopkins University, mainly at Baltimore, Md. Johns Hopkins in 1867 had a group of his associates incorporated as the trustees of a university and a hospital, endowing each with $3.5 million. Daniel C. Press.
FRIEDRICH, W.L. 2009. Santorini: volcano, natural history, mythology. Aarhus: Aarhus University Press.
GOTHBERG, H. 2007. Mer an bara hus och gardar, in H. Gothberg (ed.) Hus och bebyggelse i Uppland (Arkeologi E4 i Uppland--studier 3): 403-447. Uppsala: Uppland Museum.
GRASLUND, B. 2004. Aldre ortnamn och forntida bebyggelse. Ortnamnssallskapet i Uppsala Arsskrift 2004: 11-38.
--2008. Fimbulvintern, Ragnarok och klimatkrisen ar 536-537 e.Kr. Saga och Sea 2007: 93-123.
--2009. Ekki ny'tf solar. Nar himlen fargades rod av gudarnas blod, in A. Ney, H. Williams & F. Charpentier Ljungqvist (ed.) A austrvega. Saga and East Scandinavia. Preprint pre·print
Something printed and often distributed in partial or preliminary form in advance of official publication: a preprint of a scientific article.
tr.v. papers of the 14th International saga Conference, Uppsala, 9th-15th August 2009: 318-26. Uppsala: Uppsala University.
GRATTAN, J. & R. TORRENCE (ed.). 2007. Living under the shadow: the cultural impacts of volcanic eruptions. Walnut Creek Walnut Creek, residential city (1990 pop. 60,569), Contra Costa co., W Calif., in the San Francisco Bay area; inc. 1914. It is the trade and shipping center of an extensive agricultural area where walnuts are among the major product. (CA): Left Coast Press.
GRUDD, H. 2006. Tree rings as sensitive proxies of past climate change. Stockholm: Stockholm University.
GRUDD, H., K. BRIFFA, W. KARLEN, T. BARTHOLIN, P.D. JONES & B. KROMER. 2002. A 7400-year tree-ring chronology in northern Swedish Lapland: natural climatic variability expressed on annual to millennial timescales. The Holocene 12(6); 657-65.
GUNN, J.D. (ed.) 2000. The years without summer. Tracing AD 536 and its aftermath (British Archaeolaogical Reports International Series 872). Oxford: Archaeopress.
HERSCHEND, F. 2009. The Early Iron Age in south Scandinavia: social order in settlement and landscape. Uppsala: Uppsala University Press.
HOLTSMARK, A. 1968. Ragnarok. Kulturhistorisk Lexikon for Nordisk Medletid 13: 650-51.
HULTGARD, A. 2004. Fimbulvintern--ett mytmotiv och dess tolkning. Saga och Sed 2003: 51-69.
INGLIS, R.H. & J.E. PRYOR (ed.). 2009. Beyond determinism? Engagement and response in human-environment interactions. Archaeological Review from Cambridge 24(2).
JANSEN, E. & N. KOC. 2000. Century to decadal scale records of Norwegian sea Norwegian Sea, part of the Atlantic Ocean, NW of Norway, between the Greenland Sea and the North Sea. It is separated from the Atlantic by a submarine ridge linking Iceland and the Faeroe Islands, and from the Arctic by the Jan Mayer Ridge. surface temperature variations of the past two millennia. PAGES Newsletter 8(1): 13-14.
KAUL, F. 2004. Bronzealderens religion: studier af den nordiske bronzealders ikonografi. Copenhagen: der Kongelige Nordiske Oldskriftselskab.
KEYS, D. 1999. Catastrophe: an investigation into the origins of the modern world. London: Century.
KLEIN, N. 2007. The shock doctrine: the rise of disaster capitalism. London: Allen Lane.
KNAPPETT, C., R. RIVERS & T. EVANS. 2011. The Theran eruption and Minoan palatial pa·la·tial
1. Of or suitable for a palace: palatial furnishings.
2. Of the nature of a palace, as in spaciousness or ornateness: a palatial yacht. collapse: new interpretations gained from modelling the maritime network. Antiquity 85: 1008-1023.
LARSEN, L.B., B.M. VINTHER, K.R. BRIFFA, T.M. MELVIN, H.B. CLAUSEN, P.D. JONES, M.L. SIGGARD-ANDERSEN, C.U. HAMMER, M. ERONEN, H. GRUDD, B.E. GUNNARSSON, R.M. HANTEMIROV, M.M. NAURZBAEV & K. NICOLUASSI. 2008. New ice core evidence for a volcanic cause of the AD 536 dust-veil. Geophysical Research Letters 35: doi: 10.1029/2007GL032450.
LINDQVIST, S. 1941-42. Gotlands Bildsteine. Stockholm: Wahlstrom & Wikstrand.
LITTLE, L.K. (ed.) 2006. Plague and the end of Antiquity: the pandemic of 541-750. Cambridge: Cambridge University Press Cambridge University Press (known colloquially as CUP) is a publisher given a Royal Charter by Henry VIII in 1534, and one of the two privileged presses (the other being Oxford University Press). .
LOWENBORG, D. 2010. Excavating the digital landscape: GIS analyses of social relations in central Sweden in the 1st millennium AD. Uppsala: University of Uppsala Press.
--In press. An Iron Age shock doctrine. The 536-7 AD event as a trigger of large-scale social change in the Malaren valley area. Journal of Archaeology and Ancient History.
MCANANY, P. & N. YOFFEE (ed.). 2010. Questioning collapse: human resilience, ecological vulnerability and the aftermath of empire. Cambridge: Cambridge University Press.
MULLENHOFF, K. 1873. Um Ragnarockr. Zeitschrift fur deutsches Altertum 16.
NERMAN, B. 1958. Hur gammal ar Voluspa? Arkiv for Nordisk Filologi 73(1-2): 1-4.
--1963. Voluspa 61:3 gullnor tofflor. Arkiv for Nordisk Filologi 78(1-4): 122-25.
PICCARDI, L. & B. MASSE (ed.). 2007. Myth and geology Geomythology is the study of alleged referencees to geological events in mythology. The term was coined in 1968 by Dorothy Vitaliano, a geologist at Indiana University. . London: Geological Society.
POMEROY, A.J. 2008. 'Then it was destroyed by the volcano'. The ancient world in film and on television. London: Duckworth.
RAMPINO, M.R., S. SELF & R.B. STOTHERS. 1988. Volcanic winters. Annual Review of Earth and Planetary Sciences 16: 73-99.
RENCK, A.M. 2008. Erovrad mark--erovrat slaktskap, in M. Olausson (ed.) Hem till Jarlabanke: jord, makt och evigt liv i ostra Malardalen under jarnalder och medeltid: 91-111. Lund: Historiska Media,
ROSEN, W. 2006. Justinian's flea: plague, empire and the birth of Europe. London: Pimlico.
RUNDKVIST, M. 2011. Myths and meteorites. Minerva 22(2): 14-16.
SALZER, M.W. & M.K. HUGHES. 2007. Bristlecone pine tree rings and volcanic eruptions over the last 5000 yr. Quaternary Research 67: 57-68.
SOLBERG, B. 2000. Jernalderen i Norge. ca. 500 f Kr.1030 e. Kr. Oslo: Cappelen Forlag.
STENBERGER, M. 1933. Oland under aldre jarnaldern: en bebyggelsehistorisk undersokning. Stockholm: Kungl. Vitterhets-, historie- och antikvitetsakademien.
--1955. Vallhagar: a Migration Period settlement on Gotland, Sweden. Copenhagen: Munksgaard.
STOTHERS, R.B. 1984. Mystery cloud of AD 536. Nature 307: 344-45.
--1999. Volcanic dry fogs, climate cooling, and plague pandemics in Europe and the Middle East. Climate Change 42(4): 713-23.
STOTHERS, R.B. & M.R. RAMPINO. 1983. Volcanic eruptions in the Mediterranean before AD 630 from written and archaeological sources. Journal of Geophysical Research Journal of Geophysical Research is a publication of the American Geophysical Union. JGR was formerly titled Terrestrial Magnetism from its founding by the AGU's president Louis A. 88: 6357-71.
TAINTER, J.A. 2008. Collapse, sustainability, and the environment: how authors choose to fail or succeed. Reviews in Anthropology 37(4): 342-71.
TORRENCE, R. & J. GRATTAN (ed.). 2002. Natural disasters and cultural change. London & New York: Routledge.
TRAUFETTER, F., H. OERTER, H. FISCHER, R. WELLER & H. MILLER. 2004. Spatio-temporal variability in volcanic sulphate deposition over the past 2 kyr in snow pits and firn cores from Amundsenisen, Antartica. Journal of Glaciology glaciology
Scientific discipline concerned with all aspects of ice on landmasses. It deals with the structure and properties of glacier ice, its formation and distribution, the dynamics of ice flow, and the interactions of ice accumulations with climate. 50: 137-46.
VERVRUGGEN, C., L. DENYS & P. KIDEN. 1996. Belgium, in B.E. Berglund, J.B. Birks & M. Ralska-Jasiewiczowv (ed.) Palaeoecological events during the last 15 000 years: 553-74. Chichester: Wiley.
VITALIANO, D. 1968. Geomythology: the impact of geological events on history and legend with special reference to Atlantis. Journal of the Folklore Institute 1: 5-30.
WARBURTON, D.A. (ed.) 2009. Time's up! Dating the Minoan eruption of Santorini. Aarhus: Aarhus University Press.
WELINDER, S. 1975. Prehistoric agriculture in eastern middle Sweden. Lund: Gleerup.
WIECHMANN, I. & G. GRUBE. 2005. Detection of Yersinia pestis DNA in two early medieval skeleton finds from Aschheim (Upper Bavaria, 6th century AD). American Journal of Physical anthropology 126: 48-55.
ZACHRISSON, T. 2011. Property and honour--social change in central Sweden, 200-700 AD mirrored in the area around Old Uppsala, in L. Boye Boye may refer to:
- Anker Boye (born 1950), Danish politician
- Jan Boye (born 1962), Danish politician
- Karin Boye (1900-1941), Swedish poet and novelist
- Mame Madior Boye (born 1940), former Prime Minister of Senegal
Received: 18 July 2011; Accepted: 1 November 2011; Revised: 13 December 2011
Bo Graslund (1) & Neil Price (2)
(1) Department of Archaeology and Ancient History, University of Uppsala, Box 626, SE-751 26 Uppsala, Sweden (Email: email@example.com)
(2) Department of Archaeology, University of Aberdeen The University of Aberdeen is an ancient university founded in 1495, in Old Aberdeen, Scotland and a world-renowned centre for teaching and research. It is the fifth oldest university in the United Kingdom and the wider English-speaking world. , St Mary's, Elphinstone Road, Aberdeen AB24 3UF, UK (Email: neiLprice@abdn.ac.uk); and Rock Art Research Institute, University of the Witwatersrand Due to the 1959 Extension of University Education Act the school was only allowed to register a small number of black students for most of the apartheid era, even though several notable black anti-apartheid leaders graduated from the university. , Johannesburg, South Africa
|Printer friendly Cite/link Email Feedback|
|Author:||Graslund, Bo; Price, Neil|
|Date:||Jun 1, 2012|
|Previous Article:||Megalithic monumentality in Africa: from graves to stone circles at Wanar, Senegal.|
|Next Article:||Roads to recovery: an investigation of early medieval agrarian strategies in Byzantine Italy in and around the eighth century.|