Analysis of Herbaceous Plant Succession and Dispersal Mechanisms in Deglaciated Terrain on Mt. Yulong, China

Table 1

Changes of the terminus of Glacier-BS1 since the little ice age (data sources [24, 33]).

Period	Elevation of Glacier End, m	Advance (+) and retreat (−), m
Little ice age (17–19th centuries)	3800	+
—	3900	−214
—	4000	−350
1957	4535	−1250
1982	4100	+800
1997	4200	−150
1998	4150	+
2002	4250	−100
2011	4365	−