Postglacial transgression maximum documented by the core sediments of Xixi Wetland, East China
Constraining the timing of the postglacial transgression is of great significance to the origin of coastal wetlands distributed extensively in eastern China. The high-resolution chronological sequence from Xixi Wetland enabled us to explore interactions among the postglacial transgression, sedimenta...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Gu, Yansheng [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2017transfer abstract |
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| Schlagwörter: |
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| Umfang: |
12 |
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| Übergeordnetes Werk: |
Enthalten in: Biocompatible and noncytotoxic nucleoside-based AIEgens sensor for lighting-up nucleic acids - Xiao, Qiuyun ELSEVIER, 2021, the journal of the International Union for Quaternary Research, Amsterdam [u.a.] |
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| Übergeordnetes Werk: |
volume:436 ; year:2017 ; day:29 ; month:04 ; pages:84-95 ; extent:12 |
| Links: |
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| DOI / URN: |
10.1016/j.quaint.2016.10.030 |
|---|
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ELV036044040 |
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| 520 | |a Constraining the timing of the postglacial transgression is of great significance to the origin of coastal wetlands distributed extensively in eastern China. The high-resolution chronological sequence from Xixi Wetland enabled us to explore interactions among the postglacial transgression, sedimentary response, and human activities in the surrounding Hangzhou Bay. Diversities of 12 ostracods, 24 foraminifera and remains of oyster shells, gastropods, testate amoebae, diatoms, and vascular plants are indicative of the sedimentary facies. Grain size variables together with microfaunal records revealed seven stages of sedimentary evolution since the middle Late Pleistocene: initial riverbed, first transgression event, floodplain, early lagoon, shallow marine bay, late lagoon, and final freshwater marsh. The Xixi Basin experienced two distinct transgression events and sea-level changes inferred from assemblages of ostracods and foraminifera. The first transgression event is a minor transgression related to the moderate intensity of Asian Monsoon and moderately high sea level during the early MIS 3. The second large-scale transgression event established the sedimentary pattern of the modern Xixi Basin. The finding of the transgression maximum in the early Holocene (about 11.0–7.0 cal ka BP) highlighted the problem of reliable time of high sea level, which is tightly related to the strong Asian Monsoon intensity and global rising sea level. Subsequent changes in the sedimentary environment played a key role on the Neolithic human activities around the Hangzhou Bay. The origin of the Xixi Wetland reflected the combined effects of a sand barrier and rising human activities since the middle Holocene. | ||
| 520 | |a Constraining the timing of the postglacial transgression is of great significance to the origin of coastal wetlands distributed extensively in eastern China. The high-resolution chronological sequence from Xixi Wetland enabled us to explore interactions among the postglacial transgression, sedimentary response, and human activities in the surrounding Hangzhou Bay. Diversities of 12 ostracods, 24 foraminifera and remains of oyster shells, gastropods, testate amoebae, diatoms, and vascular plants are indicative of the sedimentary facies. Grain size variables together with microfaunal records revealed seven stages of sedimentary evolution since the middle Late Pleistocene: initial riverbed, first transgression event, floodplain, early lagoon, shallow marine bay, late lagoon, and final freshwater marsh. The Xixi Basin experienced two distinct transgression events and sea-level changes inferred from assemblages of ostracods and foraminifera. The first transgression event is a minor transgression related to the moderate intensity of Asian Monsoon and moderately high sea level during the early MIS 3. The second large-scale transgression event established the sedimentary pattern of the modern Xixi Basin. The finding of the transgression maximum in the early Holocene (about 11.0–7.0 cal ka BP) highlighted the problem of reliable time of high sea level, which is tightly related to the strong Asian Monsoon intensity and global rising sea level. Subsequent changes in the sedimentary environment played a key role on the Neolithic human activities around the Hangzhou Bay. The origin of the Xixi Wetland reflected the combined effects of a sand barrier and rising human activities since the middle Holocene. | ||
| 650 | 7 | |a Grain size |2 Elsevier | |
| 650 | 7 | |a Postglacial transgression maximum |2 Elsevier | |
| 650 | 7 | |a Microfaunal records |2 Elsevier | |
| 650 | 7 | |a Sedimentary environment |2 Elsevier | |
| 650 | 7 | |a Xixi Wetland |2 Elsevier | |
| 650 | 7 | |a Core sediments |2 Elsevier | |
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| 700 | 1 | |a Qin, Yangmin |4 oth | |
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10.1016/j.quaint.2016.10.030 doi GBV00000000000094A.pica (DE-627)ELV036044040 (ELSEVIER)S1040-6182(16)30508-0 DE-627 ger DE-627 rakwb eng 550 550 DE-600 540 VZ 6,25 ssgn ASIEN DE-1a fid 35.00 bkl 35.04 bkl Gu, Yansheng verfasserin aut Postglacial transgression maximum documented by the core sediments of Xixi Wetland, East China 2017transfer abstract 12 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Constraining the timing of the postglacial transgression is of great significance to the origin of coastal wetlands distributed extensively in eastern China. The high-resolution chronological sequence from Xixi Wetland enabled us to explore interactions among the postglacial transgression, sedimentary response, and human activities in the surrounding Hangzhou Bay. Diversities of 12 ostracods, 24 foraminifera and remains of oyster shells, gastropods, testate amoebae, diatoms, and vascular plants are indicative of the sedimentary facies. Grain size variables together with microfaunal records revealed seven stages of sedimentary evolution since the middle Late Pleistocene: initial riverbed, first transgression event, floodplain, early lagoon, shallow marine bay, late lagoon, and final freshwater marsh. The Xixi Basin experienced two distinct transgression events and sea-level changes inferred from assemblages of ostracods and foraminifera. The first transgression event is a minor transgression related to the moderate intensity of Asian Monsoon and moderately high sea level during the early MIS 3. The second large-scale transgression event established the sedimentary pattern of the modern Xixi Basin. The finding of the transgression maximum in the early Holocene (about 11.0–7.0 cal ka BP) highlighted the problem of reliable time of high sea level, which is tightly related to the strong Asian Monsoon intensity and global rising sea level. Subsequent changes in the sedimentary environment played a key role on the Neolithic human activities around the Hangzhou Bay. The origin of the Xixi Wetland reflected the combined effects of a sand barrier and rising human activities since the middle Holocene. Constraining the timing of the postglacial transgression is of great significance to the origin of coastal wetlands distributed extensively in eastern China. The high-resolution chronological sequence from Xixi Wetland enabled us to explore interactions among the postglacial transgression, sedimentary response, and human activities in the surrounding Hangzhou Bay. Diversities of 12 ostracods, 24 foraminifera and remains of oyster shells, gastropods, testate amoebae, diatoms, and vascular plants are indicative of the sedimentary facies. Grain size variables together with microfaunal records revealed seven stages of sedimentary evolution since the middle Late Pleistocene: initial riverbed, first transgression event, floodplain, early lagoon, shallow marine bay, late lagoon, and final freshwater marsh. The Xixi Basin experienced two distinct transgression events and sea-level changes inferred from assemblages of ostracods and foraminifera. The first transgression event is a minor transgression related to the moderate intensity of Asian Monsoon and moderately high sea level during the early MIS 3. The second large-scale transgression event established the sedimentary pattern of the modern Xixi Basin. The finding of the transgression maximum in the early Holocene (about 11.0–7.0 cal ka BP) highlighted the problem of reliable time of high sea level, which is tightly related to the strong Asian Monsoon intensity and global rising sea level. Subsequent changes in the sedimentary environment played a key role on the Neolithic human activities around the Hangzhou Bay. The origin of the Xixi Wetland reflected the combined effects of a sand barrier and rising human activities since the middle Holocene. Grain size Elsevier Postglacial transgression maximum Elsevier Microfaunal records Elsevier Sedimentary environment Elsevier Xixi Wetland Elsevier Core sediments Elsevier Liu, Hongye oth Qin, Yangmin oth Enthalten in Elsevier Science Xiao, Qiuyun ELSEVIER Biocompatible and noncytotoxic nucleoside-based AIEgens sensor for lighting-up nucleic acids 2021 the journal of the International Union for Quaternary Research Amsterdam [u.a.] (DE-627)ELV005958261 volume:436 year:2017 day:29 month:04 pages:84-95 extent:12 https://doi.org/10.1016/j.quaint.2016.10.030 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U FID-ASIEN 35.00 Chemie: Allgemeines VZ 35.04 Ausbildung Beruf Organisationen Chemie VZ AR 436 2017 29 0429 84-95 12 045F 550 |
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10.1016/j.quaint.2016.10.030 doi GBV00000000000094A.pica (DE-627)ELV036044040 (ELSEVIER)S1040-6182(16)30508-0 DE-627 ger DE-627 rakwb eng 550 550 DE-600 540 VZ 6,25 ssgn ASIEN DE-1a fid 35.00 bkl 35.04 bkl Gu, Yansheng verfasserin aut Postglacial transgression maximum documented by the core sediments of Xixi Wetland, East China 2017transfer abstract 12 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Constraining the timing of the postglacial transgression is of great significance to the origin of coastal wetlands distributed extensively in eastern China. The high-resolution chronological sequence from Xixi Wetland enabled us to explore interactions among the postglacial transgression, sedimentary response, and human activities in the surrounding Hangzhou Bay. Diversities of 12 ostracods, 24 foraminifera and remains of oyster shells, gastropods, testate amoebae, diatoms, and vascular plants are indicative of the sedimentary facies. Grain size variables together with microfaunal records revealed seven stages of sedimentary evolution since the middle Late Pleistocene: initial riverbed, first transgression event, floodplain, early lagoon, shallow marine bay, late lagoon, and final freshwater marsh. The Xixi Basin experienced two distinct transgression events and sea-level changes inferred from assemblages of ostracods and foraminifera. The first transgression event is a minor transgression related to the moderate intensity of Asian Monsoon and moderately high sea level during the early MIS 3. The second large-scale transgression event established the sedimentary pattern of the modern Xixi Basin. The finding of the transgression maximum in the early Holocene (about 11.0–7.0 cal ka BP) highlighted the problem of reliable time of high sea level, which is tightly related to the strong Asian Monsoon intensity and global rising sea level. Subsequent changes in the sedimentary environment played a key role on the Neolithic human activities around the Hangzhou Bay. The origin of the Xixi Wetland reflected the combined effects of a sand barrier and rising human activities since the middle Holocene. Constraining the timing of the postglacial transgression is of great significance to the origin of coastal wetlands distributed extensively in eastern China. The high-resolution chronological sequence from Xixi Wetland enabled us to explore interactions among the postglacial transgression, sedimentary response, and human activities in the surrounding Hangzhou Bay. Diversities of 12 ostracods, 24 foraminifera and remains of oyster shells, gastropods, testate amoebae, diatoms, and vascular plants are indicative of the sedimentary facies. Grain size variables together with microfaunal records revealed seven stages of sedimentary evolution since the middle Late Pleistocene: initial riverbed, first transgression event, floodplain, early lagoon, shallow marine bay, late lagoon, and final freshwater marsh. The Xixi Basin experienced two distinct transgression events and sea-level changes inferred from assemblages of ostracods and foraminifera. The first transgression event is a minor transgression related to the moderate intensity of Asian Monsoon and moderately high sea level during the early MIS 3. The second large-scale transgression event established the sedimentary pattern of the modern Xixi Basin. The finding of the transgression maximum in the early Holocene (about 11.0–7.0 cal ka BP) highlighted the problem of reliable time of high sea level, which is tightly related to the strong Asian Monsoon intensity and global rising sea level. Subsequent changes in the sedimentary environment played a key role on the Neolithic human activities around the Hangzhou Bay. The origin of the Xixi Wetland reflected the combined effects of a sand barrier and rising human activities since the middle Holocene. Grain size Elsevier Postglacial transgression maximum Elsevier Microfaunal records Elsevier Sedimentary environment Elsevier Xixi Wetland Elsevier Core sediments Elsevier Liu, Hongye oth Qin, Yangmin oth Enthalten in Elsevier Science Xiao, Qiuyun ELSEVIER Biocompatible and noncytotoxic nucleoside-based AIEgens sensor for lighting-up nucleic acids 2021 the journal of the International Union for Quaternary Research Amsterdam [u.a.] (DE-627)ELV005958261 volume:436 year:2017 day:29 month:04 pages:84-95 extent:12 https://doi.org/10.1016/j.quaint.2016.10.030 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U FID-ASIEN 35.00 Chemie: Allgemeines VZ 35.04 Ausbildung Beruf Organisationen Chemie VZ AR 436 2017 29 0429 84-95 12 045F 550 |
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10.1016/j.quaint.2016.10.030 doi GBV00000000000094A.pica (DE-627)ELV036044040 (ELSEVIER)S1040-6182(16)30508-0 DE-627 ger DE-627 rakwb eng 550 550 DE-600 540 VZ 6,25 ssgn ASIEN DE-1a fid 35.00 bkl 35.04 bkl Gu, Yansheng verfasserin aut Postglacial transgression maximum documented by the core sediments of Xixi Wetland, East China 2017transfer abstract 12 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Constraining the timing of the postglacial transgression is of great significance to the origin of coastal wetlands distributed extensively in eastern China. The high-resolution chronological sequence from Xixi Wetland enabled us to explore interactions among the postglacial transgression, sedimentary response, and human activities in the surrounding Hangzhou Bay. Diversities of 12 ostracods, 24 foraminifera and remains of oyster shells, gastropods, testate amoebae, diatoms, and vascular plants are indicative of the sedimentary facies. Grain size variables together with microfaunal records revealed seven stages of sedimentary evolution since the middle Late Pleistocene: initial riverbed, first transgression event, floodplain, early lagoon, shallow marine bay, late lagoon, and final freshwater marsh. The Xixi Basin experienced two distinct transgression events and sea-level changes inferred from assemblages of ostracods and foraminifera. The first transgression event is a minor transgression related to the moderate intensity of Asian Monsoon and moderately high sea level during the early MIS 3. The second large-scale transgression event established the sedimentary pattern of the modern Xixi Basin. The finding of the transgression maximum in the early Holocene (about 11.0–7.0 cal ka BP) highlighted the problem of reliable time of high sea level, which is tightly related to the strong Asian Monsoon intensity and global rising sea level. Subsequent changes in the sedimentary environment played a key role on the Neolithic human activities around the Hangzhou Bay. The origin of the Xixi Wetland reflected the combined effects of a sand barrier and rising human activities since the middle Holocene. Constraining the timing of the postglacial transgression is of great significance to the origin of coastal wetlands distributed extensively in eastern China. The high-resolution chronological sequence from Xixi Wetland enabled us to explore interactions among the postglacial transgression, sedimentary response, and human activities in the surrounding Hangzhou Bay. Diversities of 12 ostracods, 24 foraminifera and remains of oyster shells, gastropods, testate amoebae, diatoms, and vascular plants are indicative of the sedimentary facies. Grain size variables together with microfaunal records revealed seven stages of sedimentary evolution since the middle Late Pleistocene: initial riverbed, first transgression event, floodplain, early lagoon, shallow marine bay, late lagoon, and final freshwater marsh. The Xixi Basin experienced two distinct transgression events and sea-level changes inferred from assemblages of ostracods and foraminifera. The first transgression event is a minor transgression related to the moderate intensity of Asian Monsoon and moderately high sea level during the early MIS 3. The second large-scale transgression event established the sedimentary pattern of the modern Xixi Basin. The finding of the transgression maximum in the early Holocene (about 11.0–7.0 cal ka BP) highlighted the problem of reliable time of high sea level, which is tightly related to the strong Asian Monsoon intensity and global rising sea level. Subsequent changes in the sedimentary environment played a key role on the Neolithic human activities around the Hangzhou Bay. The origin of the Xixi Wetland reflected the combined effects of a sand barrier and rising human activities since the middle Holocene. Grain size Elsevier Postglacial transgression maximum Elsevier Microfaunal records Elsevier Sedimentary environment Elsevier Xixi Wetland Elsevier Core sediments Elsevier Liu, Hongye oth Qin, Yangmin oth Enthalten in Elsevier Science Xiao, Qiuyun ELSEVIER Biocompatible and noncytotoxic nucleoside-based AIEgens sensor for lighting-up nucleic acids 2021 the journal of the International Union for Quaternary Research Amsterdam [u.a.] (DE-627)ELV005958261 volume:436 year:2017 day:29 month:04 pages:84-95 extent:12 https://doi.org/10.1016/j.quaint.2016.10.030 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U FID-ASIEN 35.00 Chemie: Allgemeines VZ 35.04 Ausbildung Beruf Organisationen Chemie VZ AR 436 2017 29 0429 84-95 12 045F 550 |
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10.1016/j.quaint.2016.10.030 doi GBV00000000000094A.pica (DE-627)ELV036044040 (ELSEVIER)S1040-6182(16)30508-0 DE-627 ger DE-627 rakwb eng 550 550 DE-600 540 VZ 6,25 ssgn ASIEN DE-1a fid 35.00 bkl 35.04 bkl Gu, Yansheng verfasserin aut Postglacial transgression maximum documented by the core sediments of Xixi Wetland, East China 2017transfer abstract 12 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Constraining the timing of the postglacial transgression is of great significance to the origin of coastal wetlands distributed extensively in eastern China. The high-resolution chronological sequence from Xixi Wetland enabled us to explore interactions among the postglacial transgression, sedimentary response, and human activities in the surrounding Hangzhou Bay. Diversities of 12 ostracods, 24 foraminifera and remains of oyster shells, gastropods, testate amoebae, diatoms, and vascular plants are indicative of the sedimentary facies. Grain size variables together with microfaunal records revealed seven stages of sedimentary evolution since the middle Late Pleistocene: initial riverbed, first transgression event, floodplain, early lagoon, shallow marine bay, late lagoon, and final freshwater marsh. The Xixi Basin experienced two distinct transgression events and sea-level changes inferred from assemblages of ostracods and foraminifera. The first transgression event is a minor transgression related to the moderate intensity of Asian Monsoon and moderately high sea level during the early MIS 3. The second large-scale transgression event established the sedimentary pattern of the modern Xixi Basin. The finding of the transgression maximum in the early Holocene (about 11.0–7.0 cal ka BP) highlighted the problem of reliable time of high sea level, which is tightly related to the strong Asian Monsoon intensity and global rising sea level. Subsequent changes in the sedimentary environment played a key role on the Neolithic human activities around the Hangzhou Bay. The origin of the Xixi Wetland reflected the combined effects of a sand barrier and rising human activities since the middle Holocene. Constraining the timing of the postglacial transgression is of great significance to the origin of coastal wetlands distributed extensively in eastern China. The high-resolution chronological sequence from Xixi Wetland enabled us to explore interactions among the postglacial transgression, sedimentary response, and human activities in the surrounding Hangzhou Bay. Diversities of 12 ostracods, 24 foraminifera and remains of oyster shells, gastropods, testate amoebae, diatoms, and vascular plants are indicative of the sedimentary facies. Grain size variables together with microfaunal records revealed seven stages of sedimentary evolution since the middle Late Pleistocene: initial riverbed, first transgression event, floodplain, early lagoon, shallow marine bay, late lagoon, and final freshwater marsh. The Xixi Basin experienced two distinct transgression events and sea-level changes inferred from assemblages of ostracods and foraminifera. The first transgression event is a minor transgression related to the moderate intensity of Asian Monsoon and moderately high sea level during the early MIS 3. The second large-scale transgression event established the sedimentary pattern of the modern Xixi Basin. The finding of the transgression maximum in the early Holocene (about 11.0–7.0 cal ka BP) highlighted the problem of reliable time of high sea level, which is tightly related to the strong Asian Monsoon intensity and global rising sea level. Subsequent changes in the sedimentary environment played a key role on the Neolithic human activities around the Hangzhou Bay. The origin of the Xixi Wetland reflected the combined effects of a sand barrier and rising human activities since the middle Holocene. Grain size Elsevier Postglacial transgression maximum Elsevier Microfaunal records Elsevier Sedimentary environment Elsevier Xixi Wetland Elsevier Core sediments Elsevier Liu, Hongye oth Qin, Yangmin oth Enthalten in Elsevier Science Xiao, Qiuyun ELSEVIER Biocompatible and noncytotoxic nucleoside-based AIEgens sensor for lighting-up nucleic acids 2021 the journal of the International Union for Quaternary Research Amsterdam [u.a.] (DE-627)ELV005958261 volume:436 year:2017 day:29 month:04 pages:84-95 extent:12 https://doi.org/10.1016/j.quaint.2016.10.030 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U FID-ASIEN 35.00 Chemie: Allgemeines VZ 35.04 Ausbildung Beruf Organisationen Chemie VZ AR 436 2017 29 0429 84-95 12 045F 550 |
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10.1016/j.quaint.2016.10.030 doi GBV00000000000094A.pica (DE-627)ELV036044040 (ELSEVIER)S1040-6182(16)30508-0 DE-627 ger DE-627 rakwb eng 550 550 DE-600 540 VZ 6,25 ssgn ASIEN DE-1a fid 35.00 bkl 35.04 bkl Gu, Yansheng verfasserin aut Postglacial transgression maximum documented by the core sediments of Xixi Wetland, East China 2017transfer abstract 12 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Constraining the timing of the postglacial transgression is of great significance to the origin of coastal wetlands distributed extensively in eastern China. The high-resolution chronological sequence from Xixi Wetland enabled us to explore interactions among the postglacial transgression, sedimentary response, and human activities in the surrounding Hangzhou Bay. Diversities of 12 ostracods, 24 foraminifera and remains of oyster shells, gastropods, testate amoebae, diatoms, and vascular plants are indicative of the sedimentary facies. Grain size variables together with microfaunal records revealed seven stages of sedimentary evolution since the middle Late Pleistocene: initial riverbed, first transgression event, floodplain, early lagoon, shallow marine bay, late lagoon, and final freshwater marsh. The Xixi Basin experienced two distinct transgression events and sea-level changes inferred from assemblages of ostracods and foraminifera. The first transgression event is a minor transgression related to the moderate intensity of Asian Monsoon and moderately high sea level during the early MIS 3. The second large-scale transgression event established the sedimentary pattern of the modern Xixi Basin. The finding of the transgression maximum in the early Holocene (about 11.0–7.0 cal ka BP) highlighted the problem of reliable time of high sea level, which is tightly related to the strong Asian Monsoon intensity and global rising sea level. Subsequent changes in the sedimentary environment played a key role on the Neolithic human activities around the Hangzhou Bay. The origin of the Xixi Wetland reflected the combined effects of a sand barrier and rising human activities since the middle Holocene. Constraining the timing of the postglacial transgression is of great significance to the origin of coastal wetlands distributed extensively in eastern China. The high-resolution chronological sequence from Xixi Wetland enabled us to explore interactions among the postglacial transgression, sedimentary response, and human activities in the surrounding Hangzhou Bay. Diversities of 12 ostracods, 24 foraminifera and remains of oyster shells, gastropods, testate amoebae, diatoms, and vascular plants are indicative of the sedimentary facies. Grain size variables together with microfaunal records revealed seven stages of sedimentary evolution since the middle Late Pleistocene: initial riverbed, first transgression event, floodplain, early lagoon, shallow marine bay, late lagoon, and final freshwater marsh. The Xixi Basin experienced two distinct transgression events and sea-level changes inferred from assemblages of ostracods and foraminifera. The first transgression event is a minor transgression related to the moderate intensity of Asian Monsoon and moderately high sea level during the early MIS 3. The second large-scale transgression event established the sedimentary pattern of the modern Xixi Basin. The finding of the transgression maximum in the early Holocene (about 11.0–7.0 cal ka BP) highlighted the problem of reliable time of high sea level, which is tightly related to the strong Asian Monsoon intensity and global rising sea level. Subsequent changes in the sedimentary environment played a key role on the Neolithic human activities around the Hangzhou Bay. The origin of the Xixi Wetland reflected the combined effects of a sand barrier and rising human activities since the middle Holocene. Grain size Elsevier Postglacial transgression maximum Elsevier Microfaunal records Elsevier Sedimentary environment Elsevier Xixi Wetland Elsevier Core sediments Elsevier Liu, Hongye oth Qin, Yangmin oth Enthalten in Elsevier Science Xiao, Qiuyun ELSEVIER Biocompatible and noncytotoxic nucleoside-based AIEgens sensor for lighting-up nucleic acids 2021 the journal of the International Union for Quaternary Research Amsterdam [u.a.] (DE-627)ELV005958261 volume:436 year:2017 day:29 month:04 pages:84-95 extent:12 https://doi.org/10.1016/j.quaint.2016.10.030 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U FID-ASIEN 35.00 Chemie: Allgemeines VZ 35.04 Ausbildung Beruf Organisationen Chemie VZ AR 436 2017 29 0429 84-95 12 045F 550 |
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ddc 550 ddc 540 ssgn 6,25 fid ASIEN bkl 35.00 bkl 35.04 Elsevier Grain size Elsevier Postglacial transgression maximum Elsevier Microfaunal records Elsevier Sedimentary environment Elsevier Xixi Wetland Elsevier Core sediments |
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Biocompatible and noncytotoxic nucleoside-based AIEgens sensor for lighting-up nucleic acids |
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Postglacial transgression maximum documented by the core sediments of Xixi Wetland, East China |
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Constraining the timing of the postglacial transgression is of great significance to the origin of coastal wetlands distributed extensively in eastern China. The high-resolution chronological sequence from Xixi Wetland enabled us to explore interactions among the postglacial transgression, sedimentary response, and human activities in the surrounding Hangzhou Bay. Diversities of 12 ostracods, 24 foraminifera and remains of oyster shells, gastropods, testate amoebae, diatoms, and vascular plants are indicative of the sedimentary facies. Grain size variables together with microfaunal records revealed seven stages of sedimentary evolution since the middle Late Pleistocene: initial riverbed, first transgression event, floodplain, early lagoon, shallow marine bay, late lagoon, and final freshwater marsh. The Xixi Basin experienced two distinct transgression events and sea-level changes inferred from assemblages of ostracods and foraminifera. The first transgression event is a minor transgression related to the moderate intensity of Asian Monsoon and moderately high sea level during the early MIS 3. The second large-scale transgression event established the sedimentary pattern of the modern Xixi Basin. The finding of the transgression maximum in the early Holocene (about 11.0–7.0 cal ka BP) highlighted the problem of reliable time of high sea level, which is tightly related to the strong Asian Monsoon intensity and global rising sea level. Subsequent changes in the sedimentary environment played a key role on the Neolithic human activities around the Hangzhou Bay. The origin of the Xixi Wetland reflected the combined effects of a sand barrier and rising human activities since the middle Holocene. |
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Constraining the timing of the postglacial transgression is of great significance to the origin of coastal wetlands distributed extensively in eastern China. The high-resolution chronological sequence from Xixi Wetland enabled us to explore interactions among the postglacial transgression, sedimentary response, and human activities in the surrounding Hangzhou Bay. Diversities of 12 ostracods, 24 foraminifera and remains of oyster shells, gastropods, testate amoebae, diatoms, and vascular plants are indicative of the sedimentary facies. Grain size variables together with microfaunal records revealed seven stages of sedimentary evolution since the middle Late Pleistocene: initial riverbed, first transgression event, floodplain, early lagoon, shallow marine bay, late lagoon, and final freshwater marsh. The Xixi Basin experienced two distinct transgression events and sea-level changes inferred from assemblages of ostracods and foraminifera. The first transgression event is a minor transgression related to the moderate intensity of Asian Monsoon and moderately high sea level during the early MIS 3. The second large-scale transgression event established the sedimentary pattern of the modern Xixi Basin. The finding of the transgression maximum in the early Holocene (about 11.0–7.0 cal ka BP) highlighted the problem of reliable time of high sea level, which is tightly related to the strong Asian Monsoon intensity and global rising sea level. Subsequent changes in the sedimentary environment played a key role on the Neolithic human activities around the Hangzhou Bay. The origin of the Xixi Wetland reflected the combined effects of a sand barrier and rising human activities since the middle Holocene. |
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Constraining the timing of the postglacial transgression is of great significance to the origin of coastal wetlands distributed extensively in eastern China. The high-resolution chronological sequence from Xixi Wetland enabled us to explore interactions among the postglacial transgression, sedimentary response, and human activities in the surrounding Hangzhou Bay. Diversities of 12 ostracods, 24 foraminifera and remains of oyster shells, gastropods, testate amoebae, diatoms, and vascular plants are indicative of the sedimentary facies. Grain size variables together with microfaunal records revealed seven stages of sedimentary evolution since the middle Late Pleistocene: initial riverbed, first transgression event, floodplain, early lagoon, shallow marine bay, late lagoon, and final freshwater marsh. The Xixi Basin experienced two distinct transgression events and sea-level changes inferred from assemblages of ostracods and foraminifera. The first transgression event is a minor transgression related to the moderate intensity of Asian Monsoon and moderately high sea level during the early MIS 3. The second large-scale transgression event established the sedimentary pattern of the modern Xixi Basin. The finding of the transgression maximum in the early Holocene (about 11.0–7.0 cal ka BP) highlighted the problem of reliable time of high sea level, which is tightly related to the strong Asian Monsoon intensity and global rising sea level. Subsequent changes in the sedimentary environment played a key role on the Neolithic human activities around the Hangzhou Bay. The origin of the Xixi Wetland reflected the combined effects of a sand barrier and rising human activities since the middle Holocene. |
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Postglacial transgression maximum documented by the core sediments of Xixi Wetland, East China |
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The high-resolution chronological sequence from Xixi Wetland enabled us to explore interactions among the postglacial transgression, sedimentary response, and human activities in the surrounding Hangzhou Bay. Diversities of 12 ostracods, 24 foraminifera and remains of oyster shells, gastropods, testate amoebae, diatoms, and vascular plants are indicative of the sedimentary facies. Grain size variables together with microfaunal records revealed seven stages of sedimentary evolution since the middle Late Pleistocene: initial riverbed, first transgression event, floodplain, early lagoon, shallow marine bay, late lagoon, and final freshwater marsh. The Xixi Basin experienced two distinct transgression events and sea-level changes inferred from assemblages of ostracods and foraminifera. The first transgression event is a minor transgression related to the moderate intensity of Asian Monsoon and moderately high sea level during the early MIS 3. The second large-scale transgression event established the sedimentary pattern of the modern Xixi Basin. The finding of the transgression maximum in the early Holocene (about 11.0–7.0 cal ka BP) highlighted the problem of reliable time of high sea level, which is tightly related to the strong Asian Monsoon intensity and global rising sea level. Subsequent changes in the sedimentary environment played a key role on the Neolithic human activities around the Hangzhou Bay. The origin of the Xixi Wetland reflected the combined effects of a sand barrier and rising human activities since the middle Holocene.</subfield></datafield><datafield tag="650" ind1=" " ind2="7"><subfield code="a">Grain size</subfield><subfield code="2">Elsevier</subfield></datafield><datafield tag="650" ind1=" " ind2="7"><subfield code="a">Postglacial transgression maximum</subfield><subfield code="2">Elsevier</subfield></datafield><datafield tag="650" ind1=" " ind2="7"><subfield code="a">Microfaunal records</subfield><subfield code="2">Elsevier</subfield></datafield><datafield tag="650" ind1=" " ind2="7"><subfield code="a">Sedimentary environment</subfield><subfield code="2">Elsevier</subfield></datafield><datafield tag="650" ind1=" " ind2="7"><subfield code="a">Xixi Wetland</subfield><subfield code="2">Elsevier</subfield></datafield><datafield tag="650" ind1=" " ind2="7"><subfield code="a">Core sediments</subfield><subfield code="2">Elsevier</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Liu, Hongye</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Qin, Yangmin</subfield><subfield code="4">oth</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="n">Elsevier Science</subfield><subfield code="a">Xiao, Qiuyun ELSEVIER</subfield><subfield code="t">Biocompatible and noncytotoxic nucleoside-based AIEgens sensor for lighting-up nucleic acids</subfield><subfield code="d">2021</subfield><subfield code="d">the journal of the International Union for Quaternary Research</subfield><subfield code="g">Amsterdam [u.a.]</subfield><subfield code="w">(DE-627)ELV005958261</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:436</subfield><subfield code="g">year:2017</subfield><subfield code="g">day:29</subfield><subfield code="g">month:04</subfield><subfield code="g">pages:84-95</subfield><subfield code="g">extent:12</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://doi.org/10.1016/j.quaint.2016.10.030</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_U</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ELV</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_U</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">FID-ASIEN</subfield></datafield><datafield tag="936" ind1="b" ind2="k"><subfield code="a">35.00</subfield><subfield code="j">Chemie: Allgemeines</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="936" ind1="b" ind2="k"><subfield code="a">35.04</subfield><subfield code="j">Ausbildung</subfield><subfield code="j">Beruf</subfield><subfield code="j">Organisationen</subfield><subfield code="x">Chemie</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">436</subfield><subfield code="j">2017</subfield><subfield code="b">29</subfield><subfield code="c">0429</subfield><subfield code="h">84-95</subfield><subfield code="g">12</subfield></datafield><datafield tag="953" ind1=" " ind2=" "><subfield code="2">045F</subfield><subfield code="a">550</subfield></datafield></record></collection>
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