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Mangrove shoreline responses to Holocene environmental change, Makassar Strait, Indonesia
Yulianto E.a,d, Sukapti W.S.b, Rahardjo A.T.c, Noeradi D.c, Siregar D.A.b, Suparan P.b, Hirakawa K.d
a Research Center for Geotechnology, Indonesian Inst. Sci. Jl. S., Indonesia
b Laboratory of Quaternary Geology, Geol. R. D. Ctr. Jl. Dr. D., Indonesia
c Department of Geology, Bandung Inst. Technol. Jl. G., Indonesia
d Laboratory of Geoecology, Grad. Sch. of Environ. Earth Science, Hokkaido Univ., Kita 10 Nishi 5, S., Japan
[vc_row][vc_column][vc_row_inner][vc_column_inner][vc_separator css=”.vc_custom_1624529070653{padding-top: 30px !important;padding-bottom: 30px !important;}”][/vc_column_inner][/vc_row_inner][vc_row_inner layout=”boxed”][vc_column_inner width=”3/4″ css=”.vc_custom_1624695412187{border-right-width: 1px !important;border-right-color: #dddddd !important;border-right-style: solid !important;border-radius: 1px !important;}”][vc_empty_space][megatron_heading title=”Abstract” size=”size-sm” text_align=”text-left”][vc_column_text]Pollen and radiocarbon analyses have been used to study environmental and mangrove dynamics at two near-coastal sites at Batulicin, South Kalimantan and Pare-Pare, South Sulawesi, Indonesia. These two sites are separated by the Makassar Strait. The results indicate that mangroves developed at Batulicin in the mid-Holocene following sea-level stabilization. Although mangroves might have degraded to some extent due to a high rate of sea level rise prior to the mid-Holocene peak, they persisted to the present time at Batulicin. In contrast, mangrove development commenced at Pare-Pare in the early Holocene following Holocene transgression. Their development was abruptly halted in the mid-Holocene. Deposition at the site since the mid Holocene has been supra-tidal terrestrial (fluvial/floodplain), this may have been facilitated by a minor sea-level regression. Briefly, Holocene environmental and mangrove dynamics at Batulicin are: shallow marine-lower half intertidal zone/mid-tide mangroves forest-upper half intertidal zone/high-tide mangroves, while at Pare-Pare site are: terrestrial/fluvial environment-intertidal zone/mangroves-fluvial environment. © 2004 Elsevier B.V. All rights reserved.[/vc_column_text][vc_empty_space][vc_separator css=”.vc_custom_1624528584150{padding-top: 25px !important;padding-bottom: 25px !important;}”][vc_empty_space][megatron_heading title=”Author keywords” size=”size-sm” text_align=”text-left”][vc_column_text][/vc_column_text][vc_empty_space][vc_separator css=”.vc_custom_1624528584150{padding-top: 25px !important;padding-bottom: 25px !important;}”][vc_empty_space][megatron_heading title=”Indexed keywords” size=”size-sm” text_align=”text-left”][vc_column_text]Holocene,Indonesia,Makassar Strait,mangrove,palynology[/vc_column_text][vc_empty_space][vc_separator css=”.vc_custom_1624528584150{padding-top: 25px !important;padding-bottom: 25px !important;}”][vc_empty_space][megatron_heading title=”Funding details” size=”size-sm” text_align=”text-left”][vc_column_text][/vc_column_text][vc_empty_space][vc_separator css=”.vc_custom_1624528584150{padding-top: 25px !important;padding-bottom: 25px !important;}”][vc_empty_space][megatron_heading title=”DOI” size=”size-sm” text_align=”text-left”][vc_column_text]https://doi.org/10.1016/j.revpalbo.2004.03.009[/vc_column_text][/vc_column_inner][vc_column_inner width=”1/4″][vc_column_text]Widget Plumx[/vc_column_text][/vc_column_inner][/vc_row_inner][/vc_column][/vc_row][vc_row][vc_column][vc_separator css=”.vc_custom_1624528584150{padding-top: 25px !important;padding-bottom: 25px !important;}”][/vc_column][/vc_row]