Articles | Volume 17, issue 4
https://doi.org/10.5194/cp-17-1735-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/cp-17-1735-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
24 Aug 2021
Research article |
| 24 Aug 2021
| 24 Aug 2021
Signals of Holocene climate transition amplified by anthropogenic land-use changes in the westerly–Indian monsoon realm
Nicole Burdanowitz
CORRESPONDING AUTHOR
Institute for Geology, Universität Hamburg, Bundesstraße 55,
20146 Hamburg, Germany
Tim Rixen
Institute for Geology, Universität Hamburg, Bundesstraße 55,
20146 Hamburg, Germany
Leibniz-Zentrum für Marine Tropenforschung (ZMT),
Fahrenheitstraße 6, 28359 Bremen, Germany
Birgit Gaye
Institute for Geology, Universität Hamburg, Bundesstraße 55,
20146 Hamburg, Germany
Kay-Christian Emeis
Institute for Geology, Universität Hamburg, Bundesstraße 55,
20146 Hamburg, Germany
Institute of Coastal Research, Helmholtz Center Geesthacht,
Max-Planck-Straße 1, 21502 Geesthacht, Germany
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Preprint withdrawn
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Tim Rixen, Birgit Gaye, Kay-Christian Emeis, and Venkitasubramani Ramaswamy
Biogeosciences Discuss., https://doi.org/10.5194/bg-2017-317, https://doi.org/10.5194/bg-2017-317, 2017
Manuscript not accepted for further review
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Sediment trap experiments showed that in the river-influenced regions of the Indian Ocean lithogenic matter supplied from land controls the organic carbon export into the deep sea via its ballast effect in sinking particles. Carbonate produced by plankton is the main ballast material in the open ocean. The ballast effect increases the CO2 uptake of the organic carbon pump by enhancing the amount of nutrients used to bind CO2 and by favouring the sedimentation of organic matter.
Nele Tim, Eduardo Zorita, Birgit Hünicke, Xing Yi, and Kay-Christian Emeis
Ocean Sci., 12, 807–823, https://doi.org/10.5194/os-12-807-2016, https://doi.org/10.5194/os-12-807-2016, 2016
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The impact of external climate forcing on the four eastern boundary upwelling systems is investigated for the recent past and future. Under increased radiative forcing, upwelling-favourable winds should strengthen due to unequal heating of land and oceans. However, coastal upwelling simulated in ensembles of climate simulations do not show any imprint of external forcing neither for the past millennium nor for the future, with the exception of the strongest future scenario.
Denise Müller, Hermann W. Bange, Thorsten Warneke, Tim Rixen, Moritz Müller, Aazani Mujahid, and Justus Notholt
Biogeosciences, 13, 2415–2428, https://doi.org/10.5194/bg-13-2415-2016, https://doi.org/10.5194/bg-13-2415-2016, 2016
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Estuaries act as sources of the greenhouse gases nitrous oxide (N2O) and methane (CH4) to the atmosphere. We provide first measurements of N2O and CH4 in two estuaries in north-western Borneo, a region which is dominated by peatlands. We show that N2O and CH4 concentrations in these estuaries are moderate despite high organic carbon loads, that nutrient enhancement does not lead to enhanced N2O emissions, and that the wet season dominates the variability of the emissions in these systems.
D. Müller, T. Warneke, T. Rixen, M. Müller, A. Mujahid, H. W. Bange, and J. Notholt
Biogeosciences, 13, 691–705, https://doi.org/10.5194/bg-13-691-2016, https://doi.org/10.5194/bg-13-691-2016, 2016
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We studied organic carbon and the dissolved greenhouse gases carbon dioxide (CO2) and carbon monoxide (CO) in two estuaries in Sarawak, Malaysia, whose coast is covered by carbon-rich peatlands. The estuaries received terrestrial organic carbon from peat-draining tributaries. A large fraction was converted to CO2 and a minor fraction to CO. Both gases were released to the atmosphere. This shows how these estuaries function as efficient filters between land and ocean in this important region.
D. Müller, T. Warneke, T. Rixen, M. Müller, S. Jamahari, N. Denis, A. Mujahid, and J. Notholt
Biogeosciences, 12, 5967–5979, https://doi.org/10.5194/bg-12-5967-2015, https://doi.org/10.5194/bg-12-5967-2015, 2015
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Tropical peatlands are an important source of organic carbon to rivers. However, due to the remoteness of these ecosystems, data are scarce. We present the first combined assessment of both lateral organic carbon fluxes and CO2 emissions from an undisturbed tropical peat-draining river. Compared to the organic carbon concentrations, CO2 fluxes to the atmosphere were actually relatively moderate, which we attributed to the short water residence time.
T. Rixen, A. Baum, B. Gaye, and B. Nagel
Biogeosciences, 11, 5733–5747, https://doi.org/10.5194/bg-11-5733-2014, https://doi.org/10.5194/bg-11-5733-2014, 2014
A. Flohr, A. K. van der Plas, K.-C. Emeis, V. Mohrholz, and T. Rixen
Biogeosciences, 11, 885–897, https://doi.org/10.5194/bg-11-885-2014, https://doi.org/10.5194/bg-11-885-2014, 2014
B. Gaye, B. Nagel, K. Dähnke, T. Rixen, N. Lahajnar, and K.-C. Emeis
Biogeosciences, 10, 7689–7702, https://doi.org/10.5194/bg-10-7689-2013, https://doi.org/10.5194/bg-10-7689-2013, 2013
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Clim. Past, 9, 1065–1087, https://doi.org/10.5194/cp-9-1065-2013, https://doi.org/10.5194/cp-9-1065-2013, 2013
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Clim. Past, 7, 815–829, https://doi.org/10.5194/cp-7-815-2011, https://doi.org/10.5194/cp-7-815-2011, 2011
Cited articles
Ait Brahim, Y., Wassenburg, J. A., Sha, L., Cruz, F. W., Deininger, M.,
Sifeddine, A., Bouchaou, L., Spötl, C., Edwards, R. L., and Cheng, H.:
North Atlantic Ice-Rafting, Ocean and Atmospheric Circulation During the
Holocene: Insights From Western Mediterranean Speleothems, Geophys. Res.
Lett., 46, 7614–7623, https://doi.org/10.1029/2019GL082405, 2019.
Andruleit, H., Rogalla, U., and Stäger, S.: From living communities to
fossil assembages: Origin and fate of coccolithophorids in northern Arabian
Sea, Micropaleontology, 50, 5–21, 2004.
Anoop, A., Prasad, S., Krishnan, R., Naumann, R., and Dulski, P.: Intensified
monsoon and spatiotemporal changes in precipitation patterns in the NW
Himalaya during the early-mid Holocene, Quatern. Int., 313–314,
74–84, https://doi.org/10.1016/j.quaint.2013.08.014, 2013.
Ansari, M. H. and Vink, A.: Vegetation history and palaeoclimate of the past
30 kyr in Pakistan as inferred from the palynology of continental margin
sediments off the Indus Delta, Rev. Palaeobot. Palyno., 145, 201–216,
https://doi.org/10.1016/j.revpalbo.2006.10.005, 2007.
Ashok, K., Guan, Z., and Yamagata, T.: Impact of the Indian Ocean dipole on
the relationship between the Indian monsoon rainfall and ENSO, Geophys. Res.
Lett., 28, 4499–4502, https://doi.org/10.1029/2001GL013294, 2001.
Ashok, K., Guan, Z., Saji, N. H., and Yamagata, T.: Individual and Combined
Influences of ENSO and the Indian Ocean Dipole on the Indian Summer Monsoon,
J. Climate, 17, 3141–3155, https://doi.org/10.1175/1520-0442(2004)017<3141:IACIOE>2.0.CO;2, 2004.
Avnimelech, Y., Ritvo, G., Meijer, L. E., and Kochba, M.: Water content,
organic carbon and dry bulk density in flooded sediments, Aquacult. Eng.,
25, 25–33, https://doi.org/10.1016/S0144-8609(01)00068-1, 2001.
Band, S., Yadava, M. G., Lone, M. A., Shen, C. C., Sree, K., and Ramesh, R.:
High-resolution mid-Holocene Indian Summer Monsoon recorded in a stalagmite
from the Kotumsar Cave, Central India, Quatern. Int., 479, 19–24,
https://doi.org/10.1016/j.quaint.2018.01.026, 2018.
Banerji, U. S., Arulbalaji, P., and Padmalal, D.: Holocene climate
variability and Indian Summer Monsoon: An overview, Holocene, 30, 744–773,
https://doi.org/10.1177/0959683619895577, 2020.
Banse, K. and McClain, C. R.: Winter blooms of phytoplankton in the Arabian
Sea as observed by the Coastal Zone Color Scanner, Mar. Ecol. Prog. Ser.,
34, 201–211, https://doi.org/10.3354/meps034201, 1986.
Behera, S. K. and Ratnam, J. V.: Quasi-asymmetric response of the Indian
summer monsoon rainfall to opposite phases of the IOD, Sci. Rep., 8, 123,
https://doi.org/10.1038/s41598-017-18396-6, 2018.
Blake, G. R. and Hartge, K. H.: Bulk Density, Methods Soil Anal., 363–375,
https://doi.org/10.2136/sssabookser5.1.2ed.c13, 1986.
Blunier, T., Chappellaz, J., Schwander, J., Stauffer, B., and Raynaud, D.:
Variations in atmospheric methane concentration during the Holocene epoch,
Nature, 374, 46–49, https://doi.org/10.1038/374046a0, 1995.
Böll, A., Lückge, A., Munz, P., Forke, S., Schulz, H., Ramaswamy,
V., Rixen, T., Gaye, B., and Emeis, K. C.: Late Holocene primary productivity
and sea surface temperature variations in the northeastern Arabian Sea:
Implications for winter monsoon variability, Paleoceanography, 29, 778–794,
https://doi.org/10.1002/2013PA002579, 2014.
Böll, A., Schulz, H., Munz, P., Rixen, T., Gaye, B., and Emeis, K. C.:
Contrasting sea surface temperature of summer and winter monsoon variability
in the northern Arabian Sea over the last 25 ka, Palaeogeogr. Palaeocl., 426, 10–21, https://doi.org/10.1016/j.palaeo.2015.02.036, 2015.
Bond, G., Kromer, B., Beer, J., Muscheler, R., Evans, M. N., Showers, W.,
Hoffmann, S., Lotti-Bond, R., Hajdas, I., and Bonani, G.: Persistent solar
influence on North Atlantic climate during the Holocene, Science, 294,
2130–2136, https://doi.org/10.1126/science.1065680, 2001.
Bosmans, J. H. C., Drijfhout, S. S., Tuenter, E., Lourens, L. J., Hilgen, F. J., and Weber, S. L.: Monsoonal response to mid-holocene orbital forcing in a high resolution GCM, Clim. Past, 8, 723–740, https://doi.org/10.5194/cp-8-723-2012, 2012.
Bosmans, J. H. C., Hilgen, F. J., Tuenter, E., and Lourens, L. J.: Obliquity forcing of low-latitude climate, Clim. Past, 11, 1335–1346, https://doi.org/10.5194/cp-11-1335-2015, 2015.
Boyd, C. E.: Bottom Soils, Sediment, and Pond Aquaculture, 1st edn., Springer US, Boston, MA, USA, 348, https://doi.org/10.1007/978-1-4615-1785-6, 1995.
Burdanowitz, N., Gaye, B., Hilbig, L., Lahajnar, N., Lückge, A., Rixen,
T., and Emeis, K. C.: Holocene monsoon and sea level-related changes of
sedimentation in the northeastern Arabian Sea, Deep-Sea Res. Pt. II, 166, 6–18, https://doi.org/10.1016/j.dsr2.2019.03.003, 2019a.
Burdanowitz, N., Gaye, B., Hilbig, L., Lahajnar, N., Lückge, A., Rixen, T., and Emeis, K.-C.: Grain sizes and geochemistry of Holocene sediments in the Arabian Sea, PANGAEA [data set], https://doi.org/10.1594/PANGAEA.900973, 2019b.
Burdanowitz, N., Rixen, T., Gaye, B., and Emeis, K.-C.: Grain sizes and geochemistry of Holocene sediments in the Arabian Sea, PANGAEA [data set], https://doi.org/10.1594/PANGAEA.925909, 2020.
Bush, R. T. and McInerney, F. A.: Leaf wax n-alkane distributions in and
across modern plants: Implications for paleoecology and chemotaxonomy,
Geochim. Cosmochim. Ac., 117, 161–179, https://doi.org/10.1016/j.gca.2013.04.016,
2013.
Carr, A. S., Boom, A., Grimes, H. L., Chase, B. M., Meadows, M. E., and
Harris, A.: Leaf wax n-alkane distributions in arid zone South African flora:
Environmental controls, chemotaxonomy and palaeoecological implications,
Org. Geochem., 67, 72–84, https://doi.org/10.1016/j.orggeochem.2013.12.004, 2014.
Cheng, H., Fleitmann, D., Edwards, R. L., Wang, X., Cruz, F. W., Auler, A.
S., Mangini, A., Wang, Y., Kong, X., Burns, S. J., and Matter, A.: Timing and
structure of the 8.2 kyr B.P. event inferred from δ18O records of
stalagmites from China, Oman, and Brazil, Geology, 37, 1007–1010,
https://doi.org/10.1130/G30126A.1, 2009.
Clemens, S. C. and Prell, W. L.: A 350,000 year summer-monsoon multi-proxy
stack from the Owen Ridge, Northern Arabian Sea, Mar. Geol., 201,
35–51, https://doi.org/10.1016/S0025-3227(03)00207-X, 2003.
Clift, P. D. and Plumb, R. A.: The Asian Monsoon: Causes, History and
Effects, Cambridge University Press, Cambridge, UK, 2008.
Dallmeyer, A. and Claussen, M.: The influence of land cover change in the Asian monsoon region on present-day and mid-Holocene climate, Biogeosciences, 8, 1499–1519, https://doi.org/10.5194/bg-8-1499-2011, 2011.
Dallmeyer, A., Claussen, M., Wang, Y., and Herzschuh, U.: Spatial variability
of Holocene changes in the annual precipitation pattern: a model-data
synthesis for the Asian monsoon region, Clim. Dynam., 40, 2919–2936,
https://doi.org/10.1007/s00382-012-1550-6, 2013.
Davis, B. A. S. and Brewer, S.: Orbital forcing and role of the latitudinal
insolation/temperature gradient, Clim. Dynam., 32, 143–165,
https://doi.org/10.1007/s00382-008-0480-9, 2009.
Dietze, E., Hartmann, K., Diekmann, B., IJmker, J., Lehmkuhl, F., Opitz, S.,
Stauch, G., Wünnemann, B., and Borchers, A.: An end-member algorithm for
deciphering modern detrital processes from lake sediments of Lake Donggi
Cona, NE Tibetan Plateau, China, Sediment. Geol., 243, 169–180,
https://doi.org/10.1016/j.sedgeo.2011.09.014, 2012.
Dimri, A. P., Yasunari, T., Kotlia, B. S., Mohanty, U. C., and Sikka, D. R.:
Indian winter monsoon: Present and past, Earth-Sci. Rev., 163, 297–322,
https://doi.org/10.1016/j.earscirev.2016.10.008, 2016.
Dixit, Y., Hodell, D. A., Sinha, R., and Petrie, C. A.: Abrupt weakening of
the Indian summer monsoon at 8.2 kyr B.P., Earth Planet. Sc. Lett., 391,
16–23, https://doi.org/10.1016/j.epsl.2014.01.026, 2014.
Durcan, J. A., Thomas, D. S. G. G., Gupta, S., Pawar, V., Singh, R. N., and
Petrie, C. A.: Holocene landscape dynamics in the Ghaggar-Hakra
palaeochannel region at the northern edge of the Thar Desert, northwest
India, Quatern. Int., 501, 317–327, https://doi.org/10.1016/j.quaint.2017.10.012, 2019.
ESRI: ArcGIS Desktop: Release 10.8 [software], Environmental Systems
Research Institute, Redlands, CA, USA, 2019.
Fallah, B., Sodoudi, S., Russo, E., Kirchner, I., and Cubasch, U.: Towards
modeling the regional rainfall changes over Iran due to the climate forcing
of the past 6000 years, Quatern. Int., 429, 119–128,
https://doi.org/10.1016/j.quaint.2015.09.061, 2017.
Fleitmann, D., Burns, S. J., Mangini, A., Mudelsee, M., Kramers, J., Villa,
I., Neff, U., Al-Subbary, A. A., Buettner, A., Hippler, D., and Matter, A.:
Holocene ITCZ and Indian monsoon dynamics recorded in stalagmites from Oman
and Yemen (Socotra), Quaternary Sci. Rev., 26, 170–188,
https://doi.org/10.1016/j.quascirev.2006.04.012, 2007.
Forke, S., Rixen, T., Burdanowitz, N., Ramaswamy, V., Munz, P.,
Wilhelms-dick, D., Vogt, C., Kasten, S., and Gaye, B.: Sources of laminated
sediments in the northeastern Arabian Sea off Pakistan and implications for
sediment transport mechanisms during the late Holocene, Holocene, 29,
130–144, https://doi.org/10.1177/0959683618804627, 2019.
Fuller, D. Q., van Etten, J., Manning, K., Castillo, C., Kingwell-Banham,
E., Weisskopf, A., Qin, L., Sato, Y.-I., and Hijmans, R. J.: The contribution
of rice agriculture and livestock pastoralism to prehistoric methane levels:
An archaeological assessment, Holocene, 21, 743–759,
https://doi.org/10.1177/0959683611398052, 2011.
Gadgil, S.: The Indian Monsoon and its variability, Annu. Rev. Earth Pl.
Sc., 31, 429–467, https://doi.org/10.1146/annurev.earth.31.100901.141251, 2003.
Gaye, B., Böll, A., Segschneider, J., Burdanowitz, N., Emeis, K.-C., Ramaswamy, V., Lahajnar, N., Lückge, A., and Rixen, T.: Glacial–interglacial changes and Holocene variations in Arabian Sea denitrification, Biogeosciences, 15, 507–527, https://doi.org/10.5194/bg-15-507-2018, 2018.
General Bathymetric Chart of the Oceans (GEBCO): Gridded bathymetric data sets are global terrain models for ocean and land. A global 30 arc-second interval grid, The GEBCO_2014 Grid, version 20150318 [data set], available at: http://www.gebco.net/ (last access: 4 January 2017), 2014.
Giesche, A., Staubwasser, M., Petrie, C. A., and Hodell, D. A.: Indian winter and summer monsoon strength over the 4.2 ka BP event in foraminifer isotope records from the Indus River delta in the Arabian Sea, Clim. Past, 15, 73–90, https://doi.org/10.5194/cp-15-73-2019, 2019.
Giosan, L., Clift, P. D., Macklin, M. G., Fuller, D. Q., Constantinescu, S.,
Durcan, J. A., Stevens, T., Duller, G. A. T., Tabrez, A. R., Gangal, K.,
Adhikari, R., Alizai, A., Filip, F., VanLaningham, S., and Syvitski, J. P.
M.: Fluvial landscapes of the Harappan civilization, P. Natl. Acad. Sci.
USA, 109, E1688–E1694, https://doi.org/10.1073/pnas.1112743109, 2012.
Giosan, L., Orsi, W. D., Coolen, M., Wuchter, C., Dunlea, A. G., Thirumalai, K., Munoz, S. E., Clift, P. D., Donnelly, J. P., Galy, V., and Fuller, D. Q.: Neoglacial climate anomalies and the Harappan metamorphosis, Clim. Past, 14, 1669–1686, https://doi.org/10.5194/cp-14-1669-2018, 2018.
Goslin, J., Fruergaard, M., Sander, L., Gał ka, M., Menviel, L.,
Monkenbusch, J., Thibault, N., and Clemmensen, L. B.: Holocene centennial to
millennial shifts in North-Atlantic storminess and ocean dynamics, Sci.
Rep., 8, 12778, https://doi.org/10.1038/s41598-018-29949-8, 2018.
Gourlan, A. T., Albarede, F., Achyuthan, H., and Campillo, S.: The marine
record of the onset of farming around the Arabian Sea at the dawn of the
Bronze Age, Holocene, 30, 878–887, https://doi.org/10.1177/0959683620902218,
2020.
Herzschuh, U.: Palaeo-moisture evolution in monsoonal Central Asia during
the last 50,000 years, Quaternary Sci. Rev., 25, 163–178,
https://doi.org/10.1016/j.quascirev.2005.02.006, 2006.
Hou, J., Huang, Y., Zhao, J., Liu, Z., Colman, S., and An, Z.: Large Holocene
summer temperature oscillations and impact on the peopling of the
northeastern Tibetan Plateau, Geophys. Res. Lett., 43, 1323–1330,
https://doi.org/10.1002/2015GL067317, 2016.
Hunt, K. M. R., Turner, A. G., and Shaffrey, L. C.: The evolution,
seasonality and impacts of western disturbances, Q. J. Roy. Meteorol. Soc.,
144, 278–290, https://doi.org/10.1002/qj.3200, 2018.
Hussain, B. A., Mir, H., and Afzal, M.: Analysis of dust storms frequency
over Pakistan during 1961–2000, Pakisan J. Meteorol., 2, 49–68, 2005.
Ivory, S. J. and Lézine, A. M.: Climate and environmental change at the
end of the Holocene Humid Period: A pollen record off Pakistan, C.
R. Geosci., 341, 760–769, https://doi.org/10.1016/j.crte.2008.12.009, 2009.
Kaniewski, D., Van Campo, E., Guiot, J., Le Burel, S., Otto, T., and
Baeteman, C.: Environmental Roots of the Late Bronze Age Crisis, PLoS One,
8, e71004, https://doi.org/10.1371/journal.pone.0071004, 2013.
Kaskaoutis, D. G., Rashki, A., Houssos, E. E., Goto, D., and Nastos, P. T.:
Extremely high aerosol loading over Arabian Sea during June 2008: The
specific role of the atmospheric dynamics and Sistan dust storms, Atmos.
Environ., 94, 374–384, https://doi.org/10.1016/j.atmosenv.2014.05.012, 2014.
Kaskaoutis, D. G., Rashki, A., Francois, P., Dumka, U. C., Houssos, E. E.,
and Legrand, M.: Meteorological regimes modulating dust outbreaks in
southwest Asia: The role of pressure anomaly and Inter-Tropical Convergence
Zone on the 1–3 July 2014 case, Aeolian Res., 18, 83–97,
https://doi.org/10.1016/j.aeolia.2015.06.006, 2015.
Klus, A., Prange, M., Varma, V., Tremblay, L. B., and Schulz, M.: Abrupt cold events in the North Atlantic Ocean in a transient Holocene simulation, Clim. Past, 14, 1165–1178, https://doi.org/10.5194/cp-14-1165-2018, 2018.
Kong, W., Swenson, L. M., and Chiang, J. C. H.: Seasonal Transitions and the Westerly Jet in the Holocene East Asian Summer Monsoon, J. Climate, 30, 3343–3365, https://doi.org/10.1175/JCLI-D-16-0087.1, 2017.
Kotlia, B. S., Singh, A. K., Joshi, L. M., and Dhaila, B. S.: Precipitation
variability in the Indian Central Himalaya during last ca. 4000 years
inferred from a speleothem record: Impact of Indian Summer Monsoon (ISM) and
Westerlies, Quatern. Int., 371, 244–253,
https://doi.org/10.1016/j.quaint.2014.10.066, 2015.
Krishnaswamy, J., Vaidyanathan, S., Rajagopalan, B., Bonell, M., Sankaran,
M., Bhalla, R. S., and Badiger, S.: Non-stationary and non-linear influence
of ENSO and Indian Ocean Dipole on the variability of Indian monsoon
rainfall and extreme rain events, Clim. Dynam., 45, 175–184,
https://doi.org/10.1007/s00382-014-2288-0, 2015.
Kuechler, R. R., Dupont, L. M., and Schefuß, E.: Hybrid insolation forcing of Pliocene monsoon dynamics in West Africa, Clim. Past, 14, 73–84, https://doi.org/10.5194/cp-14-73-2018, 2018.
Laskar, J., Robutel, P., Joutel, F., Gastineau, M., Correia, A. C. M., and
Levrard, B.: A long-term numerical solution for the insolation quantities of
the Earth, Astron. Astrophys., 428, 261–285,
https://doi.org/10.1051/0004-6361:20041335, 2004.
Lauterbach, S., Witt, R., Plessen, B., Dulski, P., Prasad, S., Mingram, J.,
Gleixner, G., Hettler-Riedel, S., Stebich, M., Schnetger, B., Schwalb, A.,
and Schwarz, A.: Climatic imprint of the mid-latitude Westerlies in the
Central Tian Shan of Kyrgyzstan and teleconnections to North Atlantic
climate variability during the last 6000 years, Holocene, 24,
970–984, https://doi.org/10.1177/0959683614534741, 2014.
Lee, J.-Y. and Wang, B.: Future change of global monsoon in the CMIP5, Clim.
Dynam., 42, 101–119, https://doi.org/10.1007/s00382-012-1564-0, 2014.
Leipe, C., Demske, D., and Tarasov, P. E.: A Holocene pollen record from the
northwestern Himalayan lake Tso Moriri: Implications for palaeoclimatic and
archaeological research, Quatern. Int., 348, 93–112,
https://doi.org/10.1016/j.quaint.2013.05.005, 2014.
Liu, F. and Feng, Z.: A dramatic climatic transition at ∼4000 cal. yr BP and its cultural responses in Chinese cultural domains,
Holocene, 22, 1181–1197, https://doi.org/10.1177/0959683612441839, 2012.
Lückge, A., Doose-Rolinski, H., Khan, A., Schulz, H., and von Rad, U.:
Monsoonal variability in the northeastern Arabian Sea during the past
5000 years: geochemical evidence from laminated sediments, Palaeogeogr.
Palaeocl., 167, 273–286,
https://doi.org/10.1016/S0031-0182(00)00241-8, 2001.
Lückge, A., Reinhardt, L., Andruleit, H., Doose-Rolinski, H., von Rad,
U., Schulz, H., and Treppke, U.: Formation of varve-like laminae off
Pakistan: decoding 5 years of sedimentation, Geol. Soc. London, Spec. Publ.,
195, 421–431, https://doi.org/10.1144/GSL.SP.2002.195.01.23, 2002.
Madhupratap, M., Kumar, S. P., Bhattathiri, P. M. A., Kumar, M. D.,
Raghukumar, S., Nair, K. K. C., and Ramaiah, N.: Mechanism of the biological
response to winter cooling in the northeastern Arabian Sea, Nature,
384, 549–552, https://doi.org/10.1038/384549a0, 1996.
Meyers, P. A. and Ishiwatari, R.: Lacustrine organic geochemistry – an
overview of indicators of organic matter sources and diagenesis in lake
sediments, Org. Geochem., 20, 867–900, https://doi.org/10.1016/0146-6380(93)90100-P,
1993.
Mohtadi, M., Prange, M., and Steinke, S.: Palaeoclimatic insights into
forcing and response of monsoon rainfall, Nature, 533, 191–199,
https://doi.org/10.1038/nature17450, 2016.
Moy, C. M., Seltzer, G. O., Rodbell, D. T., and Anderson, D. M.: Variability
of El Niño/Southern Oscillation activity at millennial timescales during
the Holocene epoch, Nature, 420, 162–165, https://doi.org/10.1038/nature01194,
2002.
Munz, P. M., Siccha, M., Lückge, A., Böll, A., Kucera, M., and
Schulz, H.: Decadal-resolution record of winter monsoon intensity over the
last two millennia from planktic foraminiferal assemblages in the
northeastern Arabian Sea, Holocene, 25, 1756–1771, https://doi.org/10.1177/0959683615591357, 2015.
Munz, P. M., Lückge, A., Siccha, M., Böll, A., Forke, S., Kucera, M.,
and Schulz, H.: The Indian winter monsoon and its response to external
forcing over the last two and a half centuries, Clim. Dynam., 49,
1801–1812, https://doi.org/10.1007/s00382-016-3403-1, 2017.
Nagashima, K., Tada, R., and Toyoda, S.: Westerly jet-East Asian summer monsoon connection during the Holocene, Geochem. Geophy. Geosy., 14, 5041–5053, https://doi.org/10.1002/2013GC004931, 2013.
Pease, P. P., Tchakerian, V. P., and Tindale, N. W.: Aerosols over the
Arabian Sea: geochemistry and source areas for aeolian desert dust, J. Arid
Environ., 39, 477–496, https://doi.org/10.1006/jare.1997.0368, 1998.
Petrie, C. A. and Bates, J.: `Multi-cropping', Intercropping and Adaptation
to Variable Environments in Indus South Asia, J. World Prehist., 30,
81–130, https://doi.org/10.1007/s10963-017-9101-z, 2017.
Petrie, C. A., Singh, R. N., Bates, J., Dixit, Y., French, C. A. I., Hodell,
D. A., Jones, P. J., Lancelotti, C., Lynam, F., Neogi, S., Pandey, A. K.,
Parikh, D., Pawar, V., Redhouse, D. I., and Singh, D. P.: Adaptation to
Variable Environments, Resilience to Climate Change: Investigating Land,
Water and Settlement in Indus Northwest India, Curr. Anthropol., 58,
1–30, https://doi.org/10.1086/690112, 2017.
Possehl, G. L.: The transformation of the Indus Civilization, J. World
Prehist., 11, 425–472, https://doi.org/10.1007/BF02220556, 1997.
Prahl, F. G., Muehlhausen, L. A., and Zahnle, D. L.: Further evaluation of
long-chain alkenones as indicators of paleoceanographic conditions, Geochim.
Cosmochim. Ac., 52, 2303–2310, https://doi.org/10.1016/0016-7037(88)90132-9, 1988.
Prasad, S. and Enzel, Y.: Holocene paleoclimates of India, Quaternary Res.,
66, 442–453, https://doi.org/10.1016/j.yqres.2006.05.008, 2006.
Prasad, S., Anoop, A., Riedel, N., Sarkar, S., Menzel, P., Basavaiah, N.,
Krishnan, R., Fuller, D., Plessen, B., Gaye, B., Röhl, U., Wilkes, H.,
Sachse, D., Sawant, R., Wiesner, M. G., and Stebich, M.: Prolonged monsoon
droughts and links to Indo-Pacific warm pool: A Holocene record from Lonar
Lake, central India, Earth Planet. Sc. Lett., 391, 171–182,
https://doi.org/10.1016/j.epsl.2014.01.043, 2014.
Prasad, S., Marwan, N., Eroglu, D., Goswami, B., Mishra, P. K., Gaye, B.,
Anoop, A., Basavaiah, N., Stebich, M., and Jehangir, A.: Holocene climate
forcings and lacustrine regime shifts in the Indian summer monsoon realm,
Earth Surf. Proc. Land., 45, 3842–3853, https://doi.org/10.1002/esp.5004, 2020.
Rajeevan, M. and Pai, D. S.: On the El Niño-Indian monsoon predictive
relationships, Geophys. Res. Lett., 34, L04704, https://doi.org/10.1029/2006GL028916, 2007.
Ramisch, A., Lockot, G., Haberzettl, T., Hartmann, K., Kuhn, G., Lehmkuhl,
F., Schimpf, S., Schulte, P., Stauch, G., Wang, R., Wünnemann, B., Yan,
D., Zhang, Y., and Diekmann, B.: A persistent northern boundary of Indian
Summer Monsoon precipitation over Central Asia during the Holocene, Sci.
Rep., 6, 25791, https://doi.org/10.1038/srep25791, 2016.
Rao, Z., Wu, Y., Zhu, Z., Jia, G., and Henderson, A.: Is the maximum carbon
number of long-chain n-alkanes an indicator of grassland or forest? Evidence
from surface soils and modern plants, Chinese Sci. Bull., 56, 1714–1720,
https://doi.org/10.1007/s11434-011-4418-y, 2011.
Rashki, A., Kaskaoutis, D. G., Rautenbach, C. J. deW., Eriksson, P. G.,
Qiang, M., and Gupta, P.: Dust storms and their horizontal dust loading in
the Sistan region, Iran, Aeolian Res., 5, 51–62,
https://doi.org/10.1016/j.aeolia.2011.12.001, 2012.
Rawat, S., Gupta, A. K., Sangode, S. J., Srivastava, P., and Nainwal, H. C.:
Late Pleistocene–Holocene vegetation and Indian summer monsoon record from
the Lahaul, Northwest Himalaya, India, Quaternary Sci. Rev., 114, 167–181,
https://doi.org/10.1016/j.quascirev.2015.01.032, 2015.
Reichart, G.-J.: Late quaternary variability of the Arabian Sea monsoon and
oxygen minimum zone, PhD thesis, Utrecht University, Utrecht, the Netherlands, 1997.
Reichart, G. J., Lourens, L. J., and Zachariasse, W. J.: Temporal variability
in the northern Arabian Sea oxygen minimum zone (OMZ) during the last
225,000 years, Paleoceanography, 13, 607–621, https://doi.org/10.1029/98PA02203,
1998.
Rixen, T., Gaye, B., and Emeis, K.-C.: The monsoon, carbon fluxes, and the
organic carbon pump in the northern Indian Ocean, Prog. Oceanogr., 175,
24–39, https://doi.org/10.1016/j.pocean.2019.03.001, 2019.
Rommerskirchen, F., Plader, A., Eglinton, G., Chikaraishi, Y., and
Rullkötter, J.: Chemotaxonomic significance of distribution and stable
carbon isotopic composition of long-chain alkanes and alkan-1-ols in C4
grass waxes, Org. Geochem., 37, 1303–1332,
https://doi.org/10.1016/j.orggeochem.2005.12.013, 2006.
Ruddiman, W. F. and Thomson, J. S.: The case for human causes of increased
atmospheric CH4 over the last 5000 years, Quaternary Sci. Rev., 20,
1769–1777, https://doi.org/10.1016/S0277-3791(01)00067-1, 2001.
Schott, W., von Stackelberg, U., Eckhardt, F. J., Mattiat, B., Peters, J.,
and Zobel, B.: Geologische Untersuchungen an Sedimenten des
indisch-pakistanischen Kontinentalrandes (Arabisches Meer), Geol. Rundsch.,
60, 264–275, https://doi.org/10.1007/BF01820944, 1970.
Schulz, H., Von Rad, U., and Von Stackelberg, U.: Laminated sediments from
the oxygen-minimum zone of the northeastern Arabian Sea, Geol. Soc. London,
Spec. Publ., 116, 185–207, https://doi.org/10.1144/GSL.SP.1996.116.01.16, 1996.
Sirocko, F., Sarnthein, M., Lange, H., and Erlenkeuser, H.: Atmospheric
summer circulation and coastal upwelling in the Arabian Sea during the
Holocene and the last glaciation, Quaternary Res., 36, 72–93,
https://doi.org/10.1016/0033-5894(91)90018-Z, 1991.
Sonzogni, C., Bard, E., Rostek, F., Lafont, R., Rosell-Mele, A., and
Eglinton, G.: Core-top calibration of the alkenone index vs sea surface
temperature in the Indian Ocean, Deep-Sea Res. Pt. II,
44, 1445–1460, https://doi.org/10.1016/S0967-0645(97)00010-6, 1997.
Srivastava, P., Agnihotri, R., Sharma, D., Meena, N., Sundriyal, Y. P.,
Saxena, A., Bhushan, R., Sawlani, R., Banerji, U. S., Sharma, C., Bisht, P.,
Rana, N., and Jayangondaperumal, R.: 8000-year monsoonal record from Himalaya
revealing reinforcement of tropical and global climate systems since
mid-Holocene, Sci. Rep., 7, 14515, https://doi.org/10.1038/s41598-017-15143-9, 2017.
Staubwasser, M. and Sirocko, F.: On the formation of laminated sediments on
the continental margin off Pakistan: the effects of sediment provenance and
sediment redistribution, Mar. Geol., 172, 43–56,
https://doi.org/10.1016/S0025-3227(00)00119-5, 2001.
Staubwasser, M., Sirocko, F., Grootes, P. M., and Erlenkeuser, H.: South
Asian monsoon climate change and radiocarbon in the Arabian Sea during early
and middle Holocene, Paleoceanography, 17, 1063, https://doi.org/10.1029/2000PA000608,
2002.
Staubwasser, M., Sirocko, F., Grootes, P. M., and Segl, M.: Climate change at
the 4.2 ka BP termination of the Indus valley civilization and Holocene
south Asian monsoon variability, Geophys. Res. Lett., 30, 1425,
https://doi.org/10.1029/2002GL016822, 2003.
Stow, D. A. V., Tabrez, A. R., and Prins, M. A.: Quaternary sedimentation on
the Makran margin: turbidity current-hemipelagic interaction in an active
slope-apron system, Geol. Soc. London, Spec. Publ., 195, 219–236,
https://doi.org/10.1144/GSL.SP.2002.195.01.12, 2002.
Sun, D., Bloemendal, J., Rea, D. K., Vandenberghe, J., Jiang, F., An, Z., and
Su, R.: Grain-size distribution function of polymodal sediments in hydraulic
and aeolian environments, and numerical partitioning of the sedimentary
components, Sediment. Geol., 152, 263–277,
https://doi.org/10.1016/S0037-0738(02)00082-9, 2002.
Tindale, N. W. and Pease, P. P.: Aerosols over the Arabian Sea: Atmospheric
transport pathways and concentrations of dust and sea salt, Deep.-Res. Pt.
II, 46, 1577–1595,
https://doi.org/10.1016/S0967-0645(99)00036-3, 1999.
Torrence, C. and Compo, G. P.: A practical guide to wavelet analysis, B.
Am. Meteorol. Soc., 79, 61–78, 1998.
Ummenhofer, C. C., Gupta, A. Sen, Li, Y., Taschetto, A. S., and England, M.
H.: Multi-decadal modulation of the El Niño-Indian monsoon relationship
by Indian Ocean variability, Environ. Res. Lett., 6, 34006,
https://doi.org/10.1088/1748-9326/6/3/034006, 2011.
Vogts, A., Moossen, H., Rommerskirchen, F., and Rullkötter, J.:
Distribution patterns and stable carbon isotopic composition of alkanes and
alkan-1-ols from plant waxes of African rain forest and savanna C3 species,
Org. Geochem., 40, 1037–1054, https://doi.org/10.1016/j.orggeochem.2009.07.011,
2009.
von Rad, U., Schulz, H., Khan, A. A., Ansari, M., Berner, U., Čepek, P.,
Cowie, G., Dietrich, P., Erlenkeuser, H., Geyh, M., Jennerjahn, T.,
Lückge, A., Marchig, V., Riech, V., Rösch, H., Schäfer, P.,
Schulte, S., Sirocko, F., Tahir, M., and Weiss, W.: Sampling the oxygen
minimum zone off Pakistan: glacial-interglacial variations of anoxia and
productivity (preliminary results, sonne 90 cruise), Mar. Geol., 125,
7–19, https://doi.org/10.1016/0025-3227(95)00051-Y, 1995.
von Rad, U., Khan, A. A., Berger, W. H., Rammlmair, D., and Treppke, U.:
Varves, turbidites and cycles in upper Holocene sediments (Makran slope,
northern Arabian Sea), Geol. Soc. London, Spec. Publ., 195, 387–406,
https://doi.org/10.1144/GSL.SP.2002.195.01.21, 2002.
Wang, J., Sun, L., Chen, L., Xu, L., Wang, Y., and Wang, X.: The abrupt
climate change near 4,400 yr BP on the cultural transition in Yuchisi, China
and its global linkage, Sci. Rep., 6, 27723, https://doi.org/10.1038/srep27723, 2016.
Wang, P. X., Wang, B., Cheng, H., Fasullo, J., Guo, Z. T., Kiefer, T., and
Liu, Z. Y.: The global monsoon across time scales: Mechanisms and
outstanding issues, Earth-Sci. Rev., 174, 84–121,
https://doi.org/10.1016/j.earscirev.2017.07.006, 2017.
Weiss, H., Courty, M.-A., Wetterstrom, W., Guichard, F., Senior, L., Meadow,
R., and Curnow, A.: The Genesis and Collapse of Third Millennium North
Mesopotamian Civilization, Science, 261, 995–1004,
https://doi.org/10.1126/science.261.5124.995, 1993.
Wirth, S. B., Glur, L., Gilli, A., and Anselmetti, F. S.: Holocene flood frequency across the Central Alps – solar forcing and evidence for variations in North Atlantic atmospheric circulation, Quat. Sci. Rev., 80, 112–128, https://doi.org/10.1016/j.quascirev.2013.09.002, 2013.
Wright, R. P., Bryson, R. A., and Schuldenrein, J.: Water supply and history:
Harappa and the Beas regional survey, Antiquity, 82, 37–48,
https://doi.org/10.1017/S0003598X00096423, 2008.
Yadav, R. K., Rupa Kumar, K., and Rajeevan, M.: Increasing influence of ENSO
and decreasing influence of AO/NAO in the recent decades over northwest
India winter precipitation, J. Geophys. Res.-Atmos., 114, D12112,
https://doi.org/10.1029/2008JD011318, 2009.
Zhang, X., Jin, L., Chen, J., Lu, H., and Chen, F.: Lagged response of summer
precipitation to insolation forcing on the northeastern Tibetan Plateau
during the Holocene, Clim. Dynam., 50, 3117–3129,
https://doi.org/10.1007/s00382-017-3784-9, 2018.
Zhao, J., An, C.-B., Huang, Y., Morrill, C., and Chen, F.-H.: Contrasting
early Holocene temperature variations between monsoonal East Asia and
westerly dominated Central Asia, Quaternary Sci. Rev., 178, 14–23,
https://doi.org/10.1016/j.quascirev.2017.10.036, 2017.
Short summary
To study the interaction of the westerlies and Indian summer monsoon (ISM) during the Holocene, we used paleoenvironmental reconstructions using a sediment core from the northeast Arabian Sea. We found a climatic transition period between 4.6 and 3 ka BP during which the ISM shifted southwards and the influence of Westerlies became prominent. Our data indicate a stronger influence of agriculture activities and enhanced soil erosion, adding to Bond event impact after this transition period.
To study the interaction of the westerlies and Indian summer monsoon (ISM) during the Holocene,...
