The Piram Island fossil mammals revisited: Implications for age and palaeoecology.

IF 2.1
Rajeev Patnaik, Suresh Srivastava, K Milankumar Sharma, Asgar Hossain, Advait M Jukar, Deepak Choudhary, Christopher C Gilbert, Ashok Sahni
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Abstract

Piram (Perim) Island of Kathiawar (Gujarat) is well known for its preserved wealth of fossil vertebrates since the early 18th century. Broadly, these vertebrates have been considered to be equivalent to the Dhok Pathan stage of the Middle Siwaliks (~9.8-3.5 Ma). Based on earlier finds and recent field work, we describe additional fossil mammals, including the first report of a rodent from these sediments. Also, we discuss the biostratigraphy and palaeoecology of Piram in the light of the latest available Siwalik mammalian biochronology and stable carbon and oxygen isotope analyses. We can now place these highly fossiliferous sediments at ~8.7 Ma based on the first occurrence (FO) of the hipparionine equid Sivalhippus perimensis and the last occurrence (LO) of the rodent Democricetodon fejfari. Our carbon isotopic data reveal that most of the mammals (bovids, proboscideans, rhinoceratids and giraffids) were dominantly C3 browsers and lived in tropical forests and wet to dry woodlands, whereas Sivalhippus perimensis had a wider range of diet and habitat, ranging from C3 browsing in the tropical forest and wet-dry woodland to mixed C3 and C4 feeding in water stressed wooded grassland. Further, the intra-tooth oxygen isotope values recovered from two high crowned Sivalhippus perimensis teeth reveal evidence of the existence of monsoon-like seasonality in the Late Miocene around the Kathiawar region of Gujarat. Overall, the carbon isotope data indicate co-existence of strict browsers, mixed feeders, and limited grazers in a mosaic of closed canopy forest, woodland and some grassland patches, while oxygen isotope data suggest environmental heterogeneity.

皮拉姆岛哺乳动物化石重访:对年龄和古生态学的影响。
皮拉姆(皮林)岛的Kathiawar(古吉拉特邦)是众所周知的保存丰富的脊椎动物化石自18世纪初。大体上,这些脊椎动物被认为相当于中siwalks的Dhok Pathan阶段(~9.8-3.5 Ma)。根据早期的发现和最近的野外工作,我们描述了更多的哺乳动物化石,包括这些沉积物中首次报告的啮齿动物。根据最新的Siwalik哺乳动物生物年代学和稳定的碳氧同位素分析,讨论了Piram的生物地层学和古生态学。根据第一次出现的河马科动物Sivalhippus periimensis和最后一次出现的啮齿类动物Democricetodon fejfari,我们现在可以将这些高度化石化的沉积物定位在~8.7 Ma。碳同位素数据表明,大多数哺乳动物(牛科动物、鼻科动物、犀牛科动物和长颈鹿)以C3食性为主,生活在热带森林和湿-干林地,而Sivalhippus perimensis的食性和栖息地范围更广,从热带森林和干湿林地的C3食性到缺水林地的C3和C4混合食性。此外,从两颗高冠Sivalhippus perimensis牙齿中恢复的齿内氧同位素值揭示了古吉拉特邦Kathiawar地区晚中新世存在季风样季节性的证据。总体而言,碳同位素数据表明,在封闭冠层林、林地和部分草地斑块的嵌合体中,严格食草动物、混合食草动物和有限食草动物共存,而氧同位素数据表明环境异质性。
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