The potential of contribution of mangrove-derived organic matter in intertidal sediments as a proxy of mangrove development in the northern Beibu Gulf

Jun Zhang; Xianwei Meng; Peng Xia; Xiangqin Wang; Shan Gao

doi:10.1007/s13131-020-1640-y

Volume 39 Issue 12

Jan. 2021

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Jun Zhang, Xianwei Meng, Peng Xia, Xiangqin Wang, Shan Gao. The potential of contribution of mangrove-derived organic matter in intertidal sediments as a proxy of mangrove development in the northern Beibu Gulf[J]. Acta Oceanologica Sinica, 2020, 39(12): 21-29. doi: 10.1007/s13131-020-1640-y

Citation:

Jun Zhang, Xianwei Meng, Peng Xia, Xiangqin Wang, Shan Gao. The potential of contribution of mangrove-derived organic matter in intertidal sediments as a proxy of mangrove development in the northern Beibu Gulf[J]. Acta Oceanologica Sinica, 2020, 39(12): 21-29. doi: 10.1007/s13131-020-1640-y

Citation:

Jun Zhang, Xianwei Meng, Peng Xia, Xiangqin Wang, Shan Gao. The potential of contribution of mangrove-derived organic matter in intertidal sediments as a proxy of mangrove development in the northern Beibu Gulf[J]. Acta Oceanologica Sinica, 2020, 39(12): 21-29. doi: 10.1007/s13131-020-1640-y

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The potential of contribution of mangrove-derived organic matter in intertidal sediments as a proxy of mangrove development in the northern Beibu Gulf

doi: 10.1007/s13131-020-1640-y

Jun Zhang^{1, 2},
Xianwei Meng^{2, 3
,
,},
Peng Xia²,
Xiangqin Wang²,
Shan Gao²

1.
College of Marine Geosciences, Ocean University of China, Qingdao 266100, China
2.
Key Laboratory of Marine Geology and Metallogeny, Ministry of Natural Resources, Qingdao 266061, China
3.
Laboratory for Maine Geology, Pilot National Laboratory for Marine Science and Technology (Qingdao), Qingdao 266237, China

Funds: The National Natural Science Foundation of China under contract No. 41576061; the Basic Scientific Fund for National Public Research Institutes of China under contract No. 2017Q03.

More Information

Corresponding author: E-mail address: mxw@fio.org.cn (Meng Xianwei)
Received Date: 2019-07-05
Accepted Date: 2020-04-21
Rev Recd Date: 2019-09-20

Available Online: 2021-04-21

Publish Date: 2020-12-25

Abstract

Abstract

Located between terrestrial and marine ecosystems, mangrove forests are sensitive to changes in climate. The responses of mangrove ecosystems to climate change in the future can be understood by reconstructing past mangrove dynamics using proxies preserved in the intertidal sediments. Considering the complexity of the proxies commonly used, it is necessary to develop a relatively simple, inexpensive proxy. In this study, available chemical tracers (δ¹³C_org and C:N) of the four cores (YLW02, YLW03, O18, and Q37) from the intertidal zone of the northern Beibu Gulf (NBG) and a three-end-member (mangrove, sea grass, and suspended particulate matter) model was utilized to determine the contribution of mangrove-derived organic matter (CMOM) in carbonate-free sediments. Compared with the summed concentration of mangrove pollen (SCMP), a significant positive correlation between CMOM and SCMP is displayed. The calculated CMOM for an additional ²¹⁰Pb-dated sediment core from the Yingluo Bay, NBG (YLW01) clearly indicates a mangrove development going through degradation, flourishing, relative degradation, and relative flourishing, which are separately in correspondence with the lowest, highest, lower, and higher air temperature and rainfall in the time intervals of 1890–1918 AD, 1919–1956 AD, 1957–1990 AD, and 1991–2010 AD. This suggests that CMOM preserved in intertidal sediments has a potential to reconstruct historical mangrove development in high resolution, at the very least, along the coasts of the NBG.
- mangrove-derived organic matter (CMOM),
- carbonate-free sediments,
- mangrove development,
- mangrove pollen,
- potential proxy

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References(48)

References

[1]	Andrews J E, Greenaway A M, Dennis P F. 1998. Combined carbon isotope and C/N ratios as indicators of source and fate of organic matter in a poorly flushed, tropical estuary: Hunts Bay, Kingston Harbour, Jamaica. Estuarine, Coastal and Shelf Science, 46(5): 743–756. doi: 10.1006/ecss.1997.0305
[2]	Badeck F W, Tcherkez G, Nogués S, et al. 2005. Post-photosynthetic fractionation of stable carbon isotopes between plant organs—a widespread phenomenon. Rapid Communications in Mass Spectrometry, 19(11): 1381–1391. doi: 10.1002/rcm.1912
[3]	Bouillon S, Borges A V, Castañeda-Moya E, et al. 2008. Mangrove production and carbon sinks: a revision of global budget estimates. Global Biogeochemical Cycles, 22(2): GB2013
[4]	Bouillon S, Dahdouh-Guebas F, Rao A V V S, et al. 2003. Sources of organic carbon in mangrove sediments: variability and possible ecological implications. Hydrobiologia, 495(1): 33–39
[5]	Bouillon S, Moens T, Koedam N, et al. 2004. Variability in the origin of carbon substrates for bacterial communities in mangrove sediments. FEMS Microbiology Ecology, 49(2): 171–179. doi: 10.1016/j.femsec.2004.03.004
[6]	Calder J A, Parker P L. 1968. Stable carbon isotope ratios as indexes of petrochemical pollution of aquatic systems. Environment Science & Technology, 2: 535–539
[7]	Cifuentes L A, Coffin R B, Solorzano L, et al. 1996. Isotopic and elemental variations of carbon and nitrogen in a mangrove estuary. Estuarine, Coastal and Shelf Science, 43(6): 781–800. doi: 10.1006/ecss.1996.0103
[8]	Cordeiro P J M, Vilegas J H Y, Lancas F M. 1999. HRGC-MS analysis of terpenoids from maytenus ilicifolia and maytenus aquifolium (“Espinheira Santa”). Journal of the Brazilian Chemical Society, 10(6): 523–526. doi: 10.1590/S0103-50531999000600017
[9]	Dittmar T, Lara R J, Kattner G. 2001. River or mangrove? Tracing major organic matter sources in tropical Brazilian coastal waters. Marine Chemistry, 73(3–4): 253–271. doi: 10.1016/S0304-4203(00)00110-9
[10]	Ellison J C. 1993. Mangrove retreat with rising sea-level, Bermuda. Estuarine, Coastal and Shelf Science, 37(1): 75–87. doi: 10.1006/ecss.1993.1042
[11]	Ellison J C. 2008. Long-term retrospection on mangrove development using sediment cores and pollen analysis: A review. Aquatic Botany, 89(2): 93–104. doi: 10.1016/j.aquabot.2008.02.007
[12]	Fan Hangqing, Qiu Guanglong, Shi Yajun, et al. 2011. Studies on Physiological Ecology of Seagrasses in Subtropical China (in Chinese). Beijing: Science Press, 202
[13]	Gillman E, Ellison J, Coleman R. 2007. Assessment of mangrove response to projected relative sea-level rise and recent historical reconstruction of shoreline position. Environmental Monitoring & Assessment, 124(1): 105–130
[14]	Goñi M A, Ruttenberg K C, Eglinton T I. 1997. Sources and contribution of terrigenous organic carbon to surface sediments in the Gulf of Mexico. Nature, 389(6648): 275–278. doi: 10.1038/38477
[15]	Gonneea M E, Paytan A, Herrera-Silveira J A. 2004. Tracing organic matter sources and carbon burial in mangrove sediments over the past 160 years. Estuarine, Coastal and Shelf Science, 61(2): 211–227. doi: 10.1016/j.ecss.2004.04.015
[16]	Gonzalez-Farias F, Mee L D. 1988. Effect of mangrove humic-like substances on biodegradation rate of detritus. Journal of Experimental Marine Biology and Ecology, 119(1): 1–13. doi: 10.1016/0022-0981(88)90148-7
[17]	Graham M C, Eaves M A, Farmer J G, et al. 2001. A study of carbon and nitrogen stable isotope and elemental ratios as potential indicators of source and fate of organic matter in sediments of the Forth Estuary, Scotland. Estuarine, Coastal and Shelf Science, 52(3): 375–380. doi: 10.1006/ecss.2000.0742
[18]	He Yingxue, Lin Feng, Chen Min, et al. 2014. Carbon and nitrogen isotopic composition of particulate organic matter in the northern Beibu Gulf in spring. Journal of Xiamen University: Natural Science (in Chinese), 53(3): 246–251
[19]	Hu Jianfang, Peng Ping’an, Jia Guodong, et al. 2006. Distribution and sources of organic carbon, nitrogen and their isotopes in sediments of the subtropical Pearl River estuary and adjacent shelf, Southern China. Marine Chemistry, 98(2–4): 274–285. doi: 10.1016/j.marchem.2005.03.008
[20]	Huang Y, Street-Perrott F A, Metcalfe S E, et al. 2001. Climate change as the dominant control on glacial-interglacial variations in C₃ and C₄ plant abundance. Science, 293(5535): 1647–1651. doi: 10.1126/science.1060143
[21]	Jia Mingming, Wang Zongming, Zhang Yuanzhi, et al. 2015. Landsat-based estimation of mangrove forest loss and restoration in Guangxi province, China, influenced by human and natural factors. IEEE Journal of Selected Topics in Applied Earth Observations and Remote Sensing, 8(1): 311–323. doi: 10.1109/JSTARS.2014.2333527
[22]	Lamb A L, Wilson G P, Leng M J. 2006. A review of coastal palaeoclimate and relative sea-level reconstructions using δ¹³C and C/N ratios in organic material. Earth-Science Reviews, 75(1–4): 29–57. doi: 10.1016/j.earscirev.2005.10.003
[23]	Li Zhen, Saito Y, Mao Limi, et al. 2012. Mid-Holocene Mangrove succession and its response to sea-level change in the upper Mekong River delta, Cambodia. Quaternary Research, 78(2): 386–399. doi: 10.1016/j.yqres.2012.07.001
[24]	Li Zhen, Zhang Zhiying, Li Jie, et al. 2008. Pollen distribution in surface sediments of a mangrove system, Yingluo Bay, Guangxi, China. Review of Palaeobotany and Palynology, 152(1–2): 21–31. doi: 10.1016/j.revpalbo.2008.04.001
[25]	Lynch J C, Meriwether J R, McKee B A, et al. 1989. Recent accretion in mangrove ecosystems based on ¹³⁷Cs and ²¹⁰Pb. Estuaries, 12(4): 284–299. doi: 10.2307/1351907
[26]	Macko S A, Engel M H, Parker P L. 1993. Early diagenesis of organic matter in sediments: assessment of mechanisms and preservation by the use of isotopic molecular approaches. In: Engel M H, Macko S A, eds. Organic Geochemistry: Principles and Applications. Topics in Geobiology. New York: Plenum Press, 211–224
[27]	Meng Xianwei, Xia Peng, Li Zhen, et al. 2016. Mangrove degradation and response to anthropogenic disturbance in the Maowei Sea (SW China) since 1926 AD: Mangrove-derived OM and pollen. Organic Geochemistry, 98: 166–175. doi: 10.1016/j.orggeochem.2016.06.001
[28]	Meng Xianwei, Xia Peng, Li Zhen, et al. 2017. Mangrove development and its response to Asian monsoon in the Yingluo Bay (SW China) over the last 2000 years. Estuaries and Coasts, 40(2): 540–552. doi: 10.1007/s12237-016-0156-3
[29]	Monacci N M, Meier-Grünhagen U, Finney B P, et al. 2009. Mangrove ecosystem changes during the Holocene at Spanish Lookout Cay, Belize. Palaeogeography, Palaeoclimatology, Palaeoecology, 280(1–2): 37–46. doi: 10.1016/j.palaeo.2009.05.013
[30]	Moore W S. 1984. Radium isotope measurements using germanium detectors. Nuclear Instruments and Methods in Physics Research, 223(2–3): 407–411. doi: 10.1016/0167-5087(84)90683-5
[31]	Parkinson R W, DeLaune R D, White J R. 1994. Holocene sea-level rise and the fate of mangrove forests within the wider Caribbean region. Journal of Coastal Research, 10(4): 1077–1086
[32]	Pessenda L C R, Vidotto E, De Oliveira P E, et al. 2012. Late Quaternary vegetation and coastal environmental changes at Ilha do Cardoso mangrove, Southeastern Brazil. Palaeogeography, Palaeoclimatology, Palaeoecology, 363–364: 57–68. doi: 10.1016/j.palaeo.2012.08.014
[33]	Ramaswamy V, Gaye B, Shirodkar P V, et al. 2008. Distribution and sources of organic carbon, nitrogen and their isotopic signatures in sediments from the Ayeyarwady (Irrawaddy) continental shelf, northern Andaman Sea. Marine Chemistry, 111(3–4): 137–150. doi: 10.1016/j.marchem.2008.04.006
[34]	Rao Zhiguo, Zhu Zhaoyu, Jia Guodong, et al. 2010. Relationship between climatic conditions and the relative abundance of modern C₃ and C₄ plants in three regions around the North Pacific. Chinese Science Bulletin, 55(18): 1931–1936. doi: 10.1007/s11434-010-3101-z
[35]	Robertson A I, Alongi D M. 2016. Massive turnover rates of fine root detrital carbon in tropical Australian mangroves. Oecologia, 180(3): 841–851. doi: 10.1007/s00442-015-3506-0
[36]	Schultz D, Calder J A. 1976. Organic carbon ¹³C/¹²C variations in estuarine sediments. Geochimica et Cosmochimica Acta, 40: 381–385. doi: 10.1016/0016-7037(76)90002-8
[37]	Tue N T, Hamaoka H, Sogabe A, et al. 2011. The application of δ¹³C and C/N ratios as indicators of organic carbon sources and paleoenvironmental change of the mangrove ecosystem from Ba Lat Estuary, Red River, Vietnam. Environmental Earth Sciences, 64(5): 1475–1486. doi: 10.1007/s12665-011-0970-7
[38]	Versteegh G J M, Schefuß E, Dupont L, et al. 2004. Taraxerol and Rhizophora pollen as proxies for tracking past mangrove ecosystems. Geochimica et Cosmochimica Acta, 68(3): 411–422. doi: 10.1016/S0016-7037(03)00456-3
[39]	Vilegas J H Y, Lanças F M, Vilegas W, et al. 1997. Further triterpenes, steroids and furocoumarins from Brazilian medicinal plants of Dorstenia genus (Moraceae). Journal of the Brazilian Chemical Society, 8(5): 529–535. doi: 10.1590/S0103-50531997000500016
[40]	Wang Guoan, Feng Xiahong, Han J, et al. 2008. Paleovegetation reconstruction using δ¹³C of soil organic matter. Biogeosciences, 5: 1325–1337. doi: 10.5194/bg-5-1325-2008
[41]	Wei Lili, Yan Chongling, Wu Guirong, et al. 2008. Variation of δ¹³C in Aegiceras corniculatum seedling induced by cadmium application. Ecotoxicology, 17(6): 480–484. doi: 10.1007/s10646-008-0201-5
[42]	Wooller M J, Morgan R, Fowell S, et al. 2007. A multiproxy peat record of Holocene mangrove palaeoecology from Twin Cays, Belize. The Holocene, 17(8): 1129–1139. doi: 10.1177/0959683607082553
[43]	Wooller M, Smallwood B, Scharler U, et al. 2003. A taphonomic study of δ¹³C and δ¹⁵N values in Rhizophora mangle leaves for a multi-proxy approach to mangrove palaeoecology. Organic Geochemistry, 34(9): 1259–1295. doi: 10.1016/S0146-6380(03)00116-5
[44]	Xia Peng, Meng Xianwei, Feng Aiping, et al. 2015a. Sediment compaction rates in mangrove swamps of Guangxi and its mangrove migration response to sea-level rise. Acta Sedimentologica Sinica (in Chinese), 33(3): 551–560
[45]	Xia Peng, Meng Xianwei, Li Zhen, et al. 2015b. Mangrove development and its response to environmental change in Yingluo Bay (SW China) during the last 150 years: Stable carbon isotopes and mangrove pollen. Organic Geochemistry, 85: 32–41. doi: 10.1016/j.orggeochem.2015.04.003
[46]	Xia Peng, Meng Xianwei, Li Zhen, et al. 2017. Organic carbon isotope and pollen evidence for mangrove development and response to human activity in Guangxi (Southwest China) over the last 140 years. Acta Oceanologica Sinica, 36(2): 11–21. doi: 10.1007/s13131-016-0849-2
[47]	Yamamuro M. 2000. Chemical tracers of sediment organic matter origins in two coastal lagoons. Journal of Marine Systems, 26(2): 127–134. doi: 10.1016/S0924-7963(00)00049-X
[48]	Yulianto E, Sukapti W S, Rahardjo A T, et al. 2004. Mangrove shoreline responses to Holocene environmental change, Makassar Strait, Indonesia. Review of Palaeobotany and Palynology, 131(3–4): 251–268. doi: 10.1016/j.revpalbo.2004.03.009