![]() ![]() For example, Sir William Jones’s famous lecture in 1786, in which he calls attention to the similarities between Sanskrit (Old Indo-Aryan ) and the classical languages of Europe, such as Greek, Latin, and others, was instrumental in the development of Indo-European studies (Szemerényi, 1996: 4). The languages of South Asia have long played an important role in historical and contact linguistics. ![]() The study also confirms the results of other studies which suggest that different areas of grammar, such as nominal and verbal systems, may be affected to different degrees in language contact and that their respective rates of (re)complexification may also differ. The results suggest that 2,000–2,500 years ago eastern and western Indo-Aryan languages were spoken in very different sociolinguistic environments, with a high degree of ethnic and linguistic diversity in eastern India and a comparatively low level of diversity in the west. Based on assumptions made in sociolinguistic typology (e.g., Trudgill, 2011), which forms part of a larger research program investigating the effects of social factors on language structures, this study attempts to reconstruct various aspects of prehistoric society based on the structures of these two modern languages as typical representatives of eastern and western Indo-Aryan, respectively. We propose this accessible additional quantitative quality control during the final interpretation phase of establishing emergent reef sequence based LIG RSL indicators can assist in narrowing down the wide uncertainty surrounding inter-stadial ice sheet behaviors.īoyden, P., Stocchi, P., and Rovere, A.: Assessing Last Interglacial Greenland and Antarctic Ice Sheet melting through forward stratigraphic derived synthetic outcrops: test case from Southwestern Madagascar, EGU General Assembly 2022, Vienna, Austria, 23–, EGU22-8270,, 2022.The present study compares two Indo-Aryan languages, Sadri and Konkani, with respect to their morphological complexity. The resulting suite of synthetic reef sequences provides the ability to probabilistically test any number of melt scenarios against the sensitivity of the stratigraphic record. Each reef sequence has been subjected to distinct Greenland and Antarctica melt scenarios produced by a coupled ANICE-SELEN global isostatic adjustment model, matching previously hypothesized LIG sea level curves in the Indo-Pacific Basin. Stepping back from a conventional approach, in this study we generate a spectrum of synthetic Quaternary subtropical fringing reefs in southwestern Madagascar within the DIONISOS forward stratigraphic model environment. Unfortunately, this is often subjective, with significant reliance on field observations where missing facies and incomplete sequences can distort interpretations. ![]() In order to address this shortcoming, lithostratigraphic and geomorphologic traces are often used to place RSLs into a broader context. This in turn, limits ability to elucidate different commonly reported meter-scale sub-stadial sea level peak patterns and their associated uncertainties. Download final approach sub indo series#However, the often-limited sub-stadial temporal preservation of many Pleistocene reef sequences on stable coastlines restrict many reported RSLs to a series of distinct points in within the LIG. Along tropical coastal margins, LIG RSL observations are predominately based on exposed shallow coral reef sequences due to their relatively narrow indicative range and reliable U-series chronological constraints. In order to extract the RSL, a series of corrections for formational parameters and post-depositional processes need to be applied. In particular, significant effort has been made to better constrain ice sheet contributions to sea level rise through direct field observation of relative sea level (RSL) indicators. 128-116 ka, is widely considered a process analogue in understanding Earth’s systems in a future warmer climate. ![]()
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