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Late Miocene palaeoflora and palaeoclimate of Lincang (China)

B2FIND2026-04-29 收录

晚中新世古气候重建

古植物季风演化

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https://b2find.eudat.eu/dataset/436cacbf-299c-53b8-9c65-2210ac23abf6 数据链接链接失效反馈

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The Miocene Lincang leaf assemblage is used in this paper as proxy data to reconstruct the palaeoclimate of southwestern Yunnan (SW China) and the evolution of monsoon...

应用场景：

晚中新世古气候重建

Pikermian动物群演化

End-member modelling of grain-size distribution; Optimal number of significant end-members (Suppl. Data 1) Palaeomagnetic directions (Suppl. Data 2)

NIAID Data Ecosystem30

Revised stable isotope analysis for the late Pliocene composite section from different Holes of ODP SIte 138-846

稳定同位素地层学

晚中新世古气候重建

Stable isotopic values obtained for the mid to late Pliocene section of Site 138-846. Values are a composite of data previously reported by Shackleton et al. ( Shackleton N, Hall, M.A. and Pate, D.. P

PANGAEA2020-01-01 更新00

accurate orbital calibration from a deep-sea perspective

天文年代学

晚中新世古气候重建

Accurate age control of the late Tortonian to early Messinian (8.3-6.0 Ma) is essential to ascertain the origin of benthic foraminiferal d18O trends and the late Miocene carbon isotope shift (LMCIS),

PANGAEA00

Stable isotope ratios of benthic and planktonic foraminifera from Late Miocen...

晚中新世古气候重建

有孔虫稳定同位素

Tropical Indian Ocean planktonic and benthic foraminifera have 13C/12C ratios which change abruptly within Magnetic Epoch 6 about 6.2 million years ago. All species analyzed in...

B2FIND10

Age estimates of ODP Hole 175-1085A bio-and paleomagnetic events (Table 1)@en

晚中新世古气候重建

地中海盐度危机

High-resolution benthic oxygen isotope and XRF (Fe and Ca) records from Site 1085 drilled in the Mid-Cape basin (ODP Leg 175) are used to investigate global climate changes during the Late Miocene in

DataONE2026-02-15 更新00

Late Miocene palaeoflora and palaeoclimate of Lincang (China)

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