Invited research articleWarfare dendrochronology: Trees witness the deployment of the German battleship Tirpitz in Norway
Introduction
Warfare is a central and unique feature of Homo sapiens L. and has been part of human cultures and civilizations for thousands of years (Machlis et al., 2011; Francis and Krishnamurthy, 2014). Obviously, war leads to tragedies for societies and human suffering, but also poses a great threat to the environment and most living organisms (Farina, 2011). The fact that war leads to undesirable environmental impacts, including the (un)intentional destruction and degradation of natural resources, such as forests, crops and water resources, has long been recognized (Hupy, 2008; Machlis and Hanson, 2008; Reuveny et al., 2010; Hanson, 2011; Francis and Krishnamurthy, 2014). Ecological consequences can be generated during all three stages of war — preparation of war, war (violent conflict), and post-war activities (Machlis and Hanson, 2008) — and environmental damage is generally accepted as unavoidable collateral damage (Marler, 2013).
War has affected forests for millennia (McNeill, 2004). Roman accounts describe massive forest fires set by Germanic barbarian tribes to confuse and frighten their enemies, but the Romans themselves also used fire as a weapon in what is now France and Germany (Hupy, 2008). The era of modern chemical weapons in World War I (WWI) and the associated effects on forests reached a new level beyond simple burning. The Battles of Verdun and Ypres at the Western Front devastated forests in France and Belgium through stationary combative activities (Freedman, 1995; McNeill, 2004; Hupy, 2008). Names for some regions as “place à gaz” (gas place), “Forêt de Guerre” (War Forest) or “Zones Rouge” (Red Zones) still bear witness to the heavy and persistent environmental destructions. Even though explosion of ordnance itself had likely destroyed the forest, chemical warfare agents additionally contaminated these battlefields. These agents includes chlorine, phosgene/diphosgene, arsenicals and lachrymator, mostly contained in artillery shells (Thieme, 1998; Bausinger and Preuß, 2005; Bausinger et al., 2007; Prestidge, 2013). During the Greek Civil War in the late 1940s, napalm was used to burn down the forests in the Pindus Mountains of northern Greece, which served as refuge for rebel forces (McNeill, 2003, 2004). More recently, the Second Indochina War represents one of the most prominent and obvious forest devastations ever conducted by humans. With the application of chemical anti-plant herbicide and defoliation chemicals, including Agent Orange, ∼22,000 km2 of Vietnamese forests (23% of all forested area in the country) were intentionally destroyed (Orians and Pfeiffer, 1970; McNeill, 2004; Westing, 2012 and references therein).
Scientific studies on the environmental impact of warfare on forests are still scarce, however, especially for WWI and World War II (WWII). Historical writings provide some assessments, but these documents focus on the environmental factors influencing battles rather than the effects of war on the environment (Hupy, 2008). Photographs, paintings, or first-person accounts that allow an appreciation of the intensity of forest devastation also enable assessment of the ecological effects of warfare (e.g. Parsons, 1919, also see Freedman (1995) for other examples). Studies using proxy archives to evaluate military related forest devastation are rare, except a stalagmite from Northern Italy, which indicates deforestation coinciding with pre-WWI military activities (Borsato et al., 2007). An archive that scholars have not used yet to identify the impacts of military conflicts on forest ecosystems are tree rings. Only one study used dendrochronology to identify the wood supply for trenches at the above mentioned Western Front during WWI (Haneca et al., 2018). Trees record environmental changes and impacts in high temporal resolution (Fritts, 1976), offering tree-ring research the potential to steadily expand its application areas (Büntgen, 2019). Tree-ring width is a parameter representing the tree’s vitality (Dobbertin, 2005), thus it enables assessment of damage through environmental disturbance. This paper introduces the general approach of ‘warfare dendrochronology’, which should be defined, as a previously unrecognized tool to evaluate the effects of warfare on local environments and forests specifically.
In this case, the theatre of war is the Kåfjord in northern Norway. There, the Tirpitz, the largest battleship in the Kriegsmarine (German navy from 1935 to 1945), was moored for several months during the latter stages of WWII in 1943 and 1944 (Fig. 1). The ship loomed as a constant threat to Allied shipping and, as a consequence, was the target of several Soviet and British efforts to sink the giant battleship. In this article, we first provide detail on the ship and its history, as well as the strategy employed by the Kriegsmarine to use ‘artificial smoke’ to conceal the ship’s location. Then, we detail our study of more than 200 trees at the surroundings of the Kåfjord (Fig. 1b). We addressed the following research questions: (1) How did the Tirpitz battles affect local forests? (2) What was the spatial impact and duration of those effects? (3) Did they have different effects on the two main tree species pine and birch? We report how we applied dendrochronological techniques to assess biological damages due to this smoke, which is still visible in the trees 70 years later.
Section snippets
The battleship Tirpitz and its attacks and defence in northern Norway
Two thousand tons heavier than her sister ship the Bismarck, the Tirpitz was the largest ship in the Kriegsmarine during WWII. Commissioned on February 25, 1941 in Wilhelmshaven, Germany, the Tirpitz had a length of 251 m, a crew compliment of 2,500, and displaced 53,500 tons fully loaded (Koop and Schmolke, 1990). Shortly after its completion, Germany invaded the Soviet Union and the Tirpitz was appointed flagship of a temporary Baltic Fleet tasked with limiting Soviet naval operations out of
Tree-ring material from the Kåfjord, Norway
During the summers of 2016 and 2017, we collected tree-ring specimens from forests close to the Kåfjord in northern Norway, near the harbour used by the Tirpitz. Five Scots pine (Pinus sylvestris L.) stands with increasing distance to the anchor point of the Tirpitz (maximum ∼7.5 km away) and one downy birch (Betula pubescens Ehrh.) stand directly at the Tirpitz’s anchor point were sampled at the Kåfjord (Fig. 1, Table 1). We collected two 5 mm diameter increment cores per tree at breast height
Effects of smoke screens on trees in northern Norway
Before the 1940s, pine trees at almost all sites near the Kåfjord featured a small number of missing rings (with at most two trees failing to form a ring in the same calendar year) (Fig. 3a). These data show that missing rings are in a way a common feature of P. sylvestris. In general, missing rings are caused by a local lack of cambial activity, meaning an interruption of new cell production, due to extremely unfavourable growth conditions (Leuschner and Schweingruber, 1996). Therefore, the
Summary and conclusions: tree rings in “warfare ecology”
Analysis of more than 200 trees collected in 2016 and 2017 from forests surrounding the Kåfjord in northern Norway permit answers to the research questions posed in this paper. (1) The artificial smoke used to hide the Tirpitz from aerial attacks caused widespread defoliation resulting in a strong and unusual growth decline in 1945. (2) This damage extended up to 4 km away from the Tirpitz and, in the most extreme case, tree growth was interrupted for up to 9 years. Overall, growth decline was
Declaration of interest
None.
Acknowledgements
We thank Markus Kochbeck, Philip Bergforth, Ben Lehmann, Bianca Müller, Johannes Neumann and Marcus Schwarz for help with laboratory work and several geography students from the Johannes Gutenberg University Mainz who supported fieldwork during the North Scandinavia Excursions in summer 2016 and 2017. We also thank the forest owner Finnmarkseiendom for sampling permission as well as historian Arvid Petterson, Lakselv, for proving the first lead towards Tirpitz and artificial smoke in Kåfjord.
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