Zobrazeno 1 - 10
of 22
pro vyhledávání: '"Lammertsma, E.I."'
Autor:
Lammertsma, E.I., Troelstra, S.R., Flores, J.-A., Sangiorgi, F., Chemale Jr., F., do Carmo, D.A., Hoorn, C.
Publikováno v:
In Palaeogeography, Palaeoclimatology, Palaeoecology 1 October 2018 506:12-21
Publikováno v:
In Palaeogeography, Palaeoclimatology, Palaeoecology 1 January 2015 417:176-194
Autor:
van Soelen, E.E., Lammertsma, E.I., Cremer, H., Donders, T.H., Sangiorgi, F., Brooks, G.R., Larson, R.A., Sinninghe Damsté, J.S., Wagner-Cremer, F., Reichart, G.J.
Publikováno v:
In Estuarine, Coastal and Shelf Science 2010 86(2):216-224
Publikováno v:
Quaternary Research (United States), 3, 84, 287-300
Available proxy records from the Florida peninsula give a varying view on hydrological changes during the late Holocene. Here we evaluate the consistency and sensitivity of local wetland records in relation to hydrological changes over the past ~. 5.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::62ba9c2793007d5677662aa4d3352b84
http://resolver.tudelft.nl/uuid:022e8e68-eb5d-43a6-bf50-f4203bffaea9
http://resolver.tudelft.nl/uuid:022e8e68-eb5d-43a6-bf50-f4203bffaea9
Analysis of siliceous microfossils of a 79 cm long peat sediment core from Highlands Hammock State Park, Florida, revealed distinct changes in the local hydrology during the past 2,500 years. The coring site is a seasonally inundated forest where wat
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od_______101::93e45780d9f9b541da7a08074ee169b4
https://dspace.library.uu.nl/handle/1874/280996
https://dspace.library.uu.nl/handle/1874/280996
Autor:
Lammertsma, E.I., Coastal dynamics, Fluvial systems and Global change, Environmental Sciences, Palaeo-ecologie
As the concentration of atmospheric carbon dioxide (CO2) as well as global temperatures continue to increase, it is expected that sea level will rise and more extreme precipitation events will occur in the future. Moreover, warmer sea surface tempera
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=narcis______::30bb8472b5e70c0c632dd40d6a854c24
https://dspace.library.uu.nl/handle/1874/256109
https://dspace.library.uu.nl/handle/1874/256109
Autor:
Pearce, Ch., Cremer, H., Lammertsma, E.I., Wagner-Cremer, F., Coastal dynamics, Fluvial systems and Global change, Palaeo-ecologie, Dep Biologie
Publikováno v:
Journal of Paleolimnology, 1-13
Pearce, C, Cremer, H, Lammertsma, E & Wagner-Cremer, F 2011, ' A 2,500-year record of environmental change in Highlands Hammock State Park (Central Florida, U.S.A.) inferred from siliceous microfossils ', Journal of Paleolimnology . https://doi.org/10.1007/s10933-011-9557-2
Journal of Paleolimnology, 1, 49, 31-43
Journal of Paleolimnology, 49(1), 31
Pearce, C, Cremer, H, Lammertsma, E & Wagner-Cremer, F 2011, ' A 2,500-year record of environmental change in Highlands Hammock State Park (Central Florida, U.S.A.) inferred from siliceous microfossils ', Journal of Paleolimnology . https://doi.org/10.1007/s10933-011-9557-2
Journal of Paleolimnology, 1, 49, 31-43
Journal of Paleolimnology, 49(1), 31
Analysis of siliceous microfossils of a 79 cm long peat sediment core from Highlands Hammock State Park, Florida, revealed distinct changes in the local hydrology during the past 2,500 years. The coring site is a seasonally inundated forest where wat
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::55b96ac08993539df8a549eb66e57e4a
http://resolver.tudelft.nl/uuid:ef2ac3bd-54f0-4d61-9751-86071b3ca0e9
http://resolver.tudelft.nl/uuid:ef2ac3bd-54f0-4d61-9751-86071b3ca0e9
Autor:
Lammertsma, E.I., de Boer, H.J., Dekker, S.C., Dilcher, D.L., Lotter, A.F., Wagner-Cremer, F., Environmental Sciences, Palaeoecology, Sub Palaeoecology begr. 01-01-12, Section Environmental Sciences, Coastal dynamics, Fluvial systems and Global change
Publikováno v:
Proceedings of the National Academy of Sciences of the United States of America, 108(10), 4035. National Academy of Sciences
A principle response of C3 plants to increasing concentrations of atmospheric CO 2 ( CO 2 ) is to reduce transpirational water loss by decreasing stomatal conductance ( g s ) and simultaneously increase assimilation rates. Via this adaptation, vegeta
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::8e4ebbacf9cadc03e28ece895d8b6b7b
https://dspace.library.uu.nl/handle/1874/209217
https://dspace.library.uu.nl/handle/1874/209217
Autor:
Hoek, W.Z., Lammertsma, E.I., Bohncke, S.J.P., Bos, J.A.A., Bunnik, F., Kasse, C., Schokker, J., Westerhoff, W.
Publikováno v:
Netherlands Journal of Geosciences / Geologie en Mijnbouw; Jun2017, Vol. 96 Issue 2, p93-114, 22p
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