Regional vegetation and climate changes during the last 13 kyr from a marine pollen record in Seno Reloncavi, southern Chile

被引:11
|
作者
Montade, Vincent [1 ,2 ]
Nebout, Nathalie Combourieu [1 ]
Chapron, Emmanuel [3 ,4 ,5 ]
Mulsow, Sandor [6 ]
Abarzua, Ana M. [7 ]
Debret, Maxime [3 ,4 ,5 ,8 ,9 ]
Foucher, Anthony [3 ,4 ,5 ,10 ]
Desmet, Marc [10 ]
Winiarski, Thierry [11 ]
Kissel, Catherine [12 ]
机构
[1] UMR 8212 CNRS UVSQ CEA, LSCE, F-91191 Gif Sur Yvette, France
[2] UMR 226 IRD CNRS UMII, ISE M, F-34095 Montpellier, France
[3] Univ Orleans, ISTO, UMR 7327, F-45071 Orleans, France
[4] ISTO, UMR 7327, CNRS INSU, F-45071 Orleans, France
[5] Bur Rech Geol & Minieres, ISTO, UMR 7327, F-45060 Orleans, France
[6] Univ Austral Chile, Inst Geociencias, Valdivia, Chile
[7] Univ Austral Chile, Inst Ciencias Ambientales & Evolutivas, Valdivia, Chile
[8] Ecole Normale Super, LMD, F-7531 Paris, France
[9] Ecole Normale Super, CERES ERTI IPSL, UMR 8539, F-7531 Paris, France
[10] Univ Tours, Fac Sci & Tech, Lab GeHCO, EA 6293, F-37200 Tours, France
[11] Univ Lyon, LEHN IPE, ENTPE, UMR 5023, F-68518 Vaulx En Velin, France
[12] UMR 8212 CNRS UVSQ CEA, LSCE, F-91198 Gif Sur Yvette, France
关键词
Patagonia; palaeoenvironment; Holocene; rainforest; pollen; marine core; SEA-SURFACE TEMPERATURE; GRANDE-DE-CHILOE; LAKE DISTRICT; ISLA-GRANDE; ABRUPT VEGETATION; LATE-PLEISTOCENE; VARIABILITY; SEDIMENTS; LLANQUIHUE; PATTERNS;
D O I
10.1016/j.revpalbo.2012.04.005
中图分类号
Q94 [植物学];
学科分类号
071001 ;
摘要
A marine pollen record from Seno Reloncavi (southern Chile, 41 degrees S) illustrates temperate rainforest changes during the last 13 cal kyr BP. Our study shows the end of the last Termination at similar to 11.5-12 cal kyr BP coincident with the expansion of Weinmannia, illustrating disturbance and warming conditions, at the expense of cold-resistant conifers (Fitzroya-Pilgerodendron and Podocarpus). Warming conditions are strengthened at 10.7 cal kyr BP by the increase of heliophytic taxa (Eucryphia-Caldcluvia) characteristic of the Valdivian rainforest. These heliophytic taxa reach their maximum expansion between 9.6 and 7.4 cal kyr BP and point to warm and dry conditions during the Holocene Climatic Optimum. After 7.4 cal kyr BP, vegetation changes indicate variable climate conditions superimposed on a cooling trend associated with an increase in precipitation after similar to 6-5 cal kyr BP, shown by the expansion of the cold-resistant conifers. During the late Holocene, after 2.8 cal kyr BP, the continuous expansion of cold-resistant conifers marks an increase of cool and wet conditions. The comparison between marine and terrestrial pollen records highlights the similar trends and timing of vegetation changes which allows to complete the regional pattern of vegetation changes around Seno Reloncavi. In comparison with the terrestrial pollen records, this marine pollen record provides a more regional signal of vegetation/climate changes and clearly demonstrates the sensitivity of marine pollen records to past vegetation and climate change. 2012 Elsevier B.V. All rights reserved.
引用
收藏
页码:11 / 21
页数:11
相关论文
共 50 条
  • [21] Vegetation response to climate change on Jeju Island, South Korea, during the last deglaciation based on pollen record
    Chung, Chull-Hwan
    GEOSCIENCES JOURNAL, 2007, 11 (02) : 147 - 155
  • [22] Pollen record of climate change during the last deglaciation from the eastern Tibetan Plateau
    Shi, Wei
    Jiang, Hanchao
    Mao, Xue
    Xu, Hongyan
    PLOS ONE, 2020, 15 (05):
  • [23] Vegetation and climate changes during the Late Pleistocene to Holocene inferred from pollen record in Jinju area, South Korea
    Chull-Hwan Chung
    Hyoun Soo Lim
    Ho II Yoon
    Geosciences Journal, 2006, 10 : 423 - 431
  • [24] Vegetation and climate changes during the Late Pleistocene to Holocene inferred from pollen record in Jinju area, South Korea
    Chung, Chull-Hwan
    Lim, Hyoun Soo
    Yoon, Ho Il
    GEOSCIENCES JOURNAL, 2006, 10 (04) : 423 - 431
  • [25] The vegetation and climate history of the last glacial cycle in a new pollen record from Lake Fimon (southern Alpine foreland, N-Italy)
    Pini, R.
    Ravazzi, C.
    Reimer, P. J.
    QUATERNARY SCIENCE REVIEWS, 2010, 29 (23-24) : 3115 - 3137
  • [26] A detailed pollen record of vegetation and climate changes in Central China during the past 16 000 years
    Zhu, Cheng
    Ma, Chunmei
    Yu, Shi-Yong
    Tang, Lingyu
    Zhang, Wenqing
    Lu, Xuefeng
    BOREAS, 2010, 39 (01) : 69 - 76
  • [27] Vegetation and climate changes during the last 8660 cal. a BP in central Mongolia, based on a high-resolution pollen record from Lake Ugii Nuur
    Wang Wei
    Ma YuZhen
    Feng ZhaoDong
    Meng HongWei
    Sang YanLi
    Zhai XinWei
    CHINESE SCIENCE BULLETIN, 2009, 54 (09): : 1579 - 1589
  • [28] VEGETATION AND CLIMATE CHANGES IN CENTRAL ASIA DURING OVER THE LAST 28,000 YRS: A HIGH-RESOLUTION POLLEN RECORD FROM VALIKHANOV SECTION, KAZAKHSTAN
    Huang, Changqing
    Liu, Kam-Biu
    Feng, Zhaodong
    Ran, Ming
    2011 3RD INTERNATIONAL CONFERENCE ON COMPUTER TECHNOLOGY AND DEVELOPMENT (ICCTD 2011), VOL 1, 2012, : 787 - 791
  • [29] Vegetation and climate changes during the last two glacial-interglacial cycles in the western Mediterranean: A new long pollen record from Padul (southern Iberian Peninsula) (vol 205, pg 86, 2019)
    Camuera, Jon
    Jimenez-Moreno, Gonzalo
    Ramos-Roman, Maria J.
    Garcia-Alix, Antonio
    Toney, Jaime L.
    Anderson, R. Scott
    Jimenez-Espejo, Francisco
    Bright, Jordon
    Webster, Cole
    Yanes, Yurena
    Carrion, Jose S.
    QUATERNARY SCIENCE REVIEWS, 2019, 207 : 161 - 162