Surface soil phytolith assemblages in different vegetational zones of the Nilgiri Biogeographical Region, Western Ghats, India: implications for palaeoclimatic interpretation

IF 2.7 2区 地球科学 Q2 GEOGRAPHY, PHYSICAL
Gayathri Rajendiran , Vivek Pandi , Vishnu Shreekara Bhat , Nidhi Vastrad , K. Anupama , Doris Barboni
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Abstract

In the present study, we analyzed surface soil phytolith assemblages from 70 sites across seven vegetation types spanning an altitudinal range of 300–2400 m in the Nilgiri Biogeographic Region (NBR), Western Ghats, India. A total of 29 morphotypes were identified, dominated by BILOBATE, SADDLE, RONDEL, ELONGATE, BLOCKY, and POLYHEDRAL forms. Lowland seasonally-dry tropical forests (STDFs) were characterized by high proportions of C4 grass indicators, mid-elevation moist and wet forests exhibited mixed C3-C4 signatures, while upper montane forests and grasslands contained phytolith assemblages indicating relative grass dominance, although absolute grass cover was underestimated and woody signals overrepresented. Discriminant analysis achieved a moderate classification accuracy of ∼55 %, indicating a possible overlap between vegetation types and transitional communities. Principal Component Analysis indicated that elevation and mean annual precipitation as primary controls on phytolith composition. Morphometric analysis of BILOBATE phytoliths revealed decreasing dimensions (length and shank length) with elevation and strong positive correlations with mean annual temperature, highlighting temperature as a key driver of silica deposition. Overall, this first phytolith-based vegetation study in the NBR establishes a modern reference framework for interpreting the fossil record. Our findings demonstrate both the potential and limitations of phytolith assemblages and morphometrics for reconstructing past vegetation and climate in NBR and similar tropical montane ecosystems.
印度西高止山脉Nilgiri生物地理区不同植被带表层土壤植物岩组合:古气候解释的意义
在本研究中,我们分析了印度西高止山脉Nilgiri生物地理区(NBR)在300-2400 m的海拔范围内跨越7种植被类型的70个站点的表层土壤植物岩组合。共鉴定出29种形态,以双叶形、鞍形、圆形、长形、块状和多面体形态为主。低海拔季节性干燥热带森林(stdf)具有较高比例的C4草信号,中高海拔潮湿和潮湿森林表现出混合的C3-C4信号,而高山森林和草地含有植物岩组合,表明相对禾草优势,尽管绝对草覆盖被低估,木质信号被过度代表。判别分析获得了约55%的中等分类精度,表明植被类型和过渡群落之间可能存在重叠。主成分分析表明,海拔高度和年平均降水量是影响植物体组成的主要因素。BILOBATE植物岩的形态测量分析显示,长度和柄长随海拔升高而减小,且与年平均温度呈正相关,表明温度是硅沉积的关键驱动因素。总的来说,这是NBR中第一个基于植物岩的植被研究,为解释化石记录建立了一个现代参考框架。我们的研究结果显示了植物岩组合和形态计量学在重建NBR和类似热带山地生态系统过去植被和气候方面的潜力和局限性。
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来源期刊
CiteScore
5.90
自引率
10.00%
发文量
398
审稿时长
3.8 months
期刊介绍: Palaeogeography, Palaeoclimatology, Palaeoecology is an international medium for the publication of high quality and multidisciplinary, original studies and comprehensive reviews in the field of palaeo-environmental geology. The journal aims at bringing together data with global implications from research in the many different disciplines involved in palaeo-environmental investigations. By cutting across the boundaries of established sciences, it provides an interdisciplinary forum where issues of general interest can be discussed.
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