4.3 Article

New fossil endocarps of Sambucus (Adoxaceae) from the upper Pliocene in SW China

期刊

REVIEW OF PALAEOBOTANY AND PALYNOLOGY
卷 171, 期 -, 页码 152-163

出版社

ELSEVIER
DOI: 10.1016/j.revpalbo.2011.11.008

关键词

Sambucus; Adoxaceae; Upper Pliocene; Sanying Formation; Yunnan; Southwest China

资金

  1. National Natural Science Foundation of China, NNSFC [41030212, 30970206]
  2. National Basic Research Program of China, 973 Program [2012CB821901]
  3. US NSF [EAR-0746105]
  4. U.S. DOE [DE-AC02-06CH11357]
  5. Division Of Earth Sciences
  6. Directorate For Geosciences [746105] Funding Source: National Science Foundation

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A new species of fossil endocarp is described from the Sanying Formation of the upper Pliocene at Fudong Village, Lanping County of northwestern Yunnan Province, Southwest China. The endocarps are elliptic, ovate or oblong elliptic, 2.1-2.5 mm long and 1.2-1.7 mm wide. The dorsal face is convex and the ventral is concave or more flattened. The endocarp surface is loosely, transversely or sinuously furrowed and ridged, forming a reticulate and alveolate pattern on the ridges, and the inner wall of the surface cells on the ridges is flaky and scaly. They are morphologically compared with selected extant genera of Adoxaceae and Caprifoliaceae. The interspecific comparisons show diagnostic differences of the fossil endocarps from the selected modern species and other fossil taxa, supporting their recognition as a new species: Sambucus alveolatisemina Huang, Liu et Zhou, sp. nov. Previous records of the reliable Sambucus fossils were from mid-high latitude regions in Europe, northeastern Asia and northern North America. Therefore, it is interesting to note that S. alveolatisemina represents a fossil record from a low latitude region. Sambucus apparently has existed at low latitudes in China at least since the upper Pliocene. A review of other Sambucus fossil occurrences indicates that plants of this genus have been living at higher latitudes in the geological past than they are at present. (C) 2011 Elsevier B.V. All rights reserved.

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