Nd isotope signature of Holocene Baltic Mn/Fe precipitates as monitor of climate change during the Little Ice Age

• Published in: Geochimica et cosmochimica acta Vol. 69; no. 9; pp. 2253 - 2263
• Main Authors: Bock, B., Liebetrau, V., Eisenhauer, A., Frei, R., Leipe, T.
• Format: Journal Article
• Language: English
• Published: Elsevier Ltd 01.05.2005
• Subjects: Marine; ANE, North Sea; ANE, Baltic Sea; AN, North Atlantic, North Atlantic Oscillation
• ISSN: 0016-7037; 1872-9533
• DOI: 10.1016/j.gca.2004.11.016

Neodymium (Nd) isotope profiles were analyzed on two Baltic Mn/Fe precipitates (99/2 and TL1) from shallow water (20 m) of the Mecklenburg Bay. The age range of these Mn/Fe precipitates determined by 226Ra ex/Ba dating reaches from recent growth back to ∼4300 and 1000 yr BP, respectively. Over this time range, the Nd isotope composition varies from ε Nd (0) = −13.1 to −17.5 in the selected Baltic precipitates indicating substantial changes in the Nd isotope composition of the Baltic Sea. The lowest ε Nd values were recorded during the time interval of the Little Ice Age (LIA, AD ∼1350 to 1850). These minimum values indicate either an increase of the input of less radiogenic Nd from Scandinavian Archean-Proterozoic sources (ε Nd about −22) to the Baltic Sea or a decrease of the input of more radiogenic Nd from continental European sources (ε Nd about −12) and/or North Sea water (ε Nd about −10). Variations of both, erosive continental input and North Sea inflow may indicate a direct response of the Nd isotope signal in the Baltic Sea to climate changes during the LIA and be related to cyclic shifts in the atmospheric circulation triggered by the North Atlantic Oscillation (NAO). Another aspect that possibly influenced the input of trace elements and Nd isotopes into the Baltic Sea is the population development in the circum Baltic area during the LIA. The lowest ε Nd values also correspond to the medieval demographic crises that led to a significant decrease of agricultural activity and farmland. The reduction of soil erosion and enhanced regrowth of natural vegetation may have changed the amount and proportions of dissolved and suspended particulate matter transported into the Baltic Sea by rivers which in turn may have resulted in a change of the Nd isotope composition of Baltic Sea water.