Fingerprint of tropical climate variability and sea level in sediments of the Cariaco Basin during the last glacial period

Gaudenz Deplazes, Anna Nele Meckler, Larry C Peterson, Yvonne Hamann, Beat Aeschlimann, Detlef Günther, Alfredo Martínez-García, Gerald H. Haug

Research output: Contribution to journalArticle

Abstract

High-resolution palaeorecords of climate are critical to improving current understanding of climate variability, its sensitivity and impact on the environment in the past and in the future. Sediments from the Cariaco Basin off the coast of Venezuela have proven to be sensitive recorders of tropical palaeoclimate variability down to an annual scale. However, the fingerprint of climate and sea level in the sediments of the last glacial period is still not completely understood. In this study, lamination analysis of sediments from the Cariaco Basin is extended to the last glacial period. Detailed sedimentological and geochemical analysis (laser ablation–inductively coupled plasma–mass spectrometry) reveals couplets of light-coloured, terrigenous-rich and dark-coloured, biogenic opal-rich laminae, which are interpreted to reflect the seasonal migration of the Intertropical Convergence Zone. In addition, a previously undescribed, nearly pure terrigenous lamina type is observed, which is referred to hereafter as a ‘C-layer’. The C-layers in the sedimentary sequence are interpreted as flood layers that originate from local rivers. The occurrence of these C-layers is investigated for two core locations in the Cariaco Basin over the last 110 kyr by continuous X-ray fluorescence scanning. Dansgaard–Oeschger oscillations are most clearly traced by proxies reflecting productivity and marine organic matter content of the sediment. In contrast, the abundance of terrigenous material differs at times between the two sites. On an interglacial to glacial timescale, the ability to record events causing C-layers is likely to be influenced by changes in sea level and source proximity. On a millennial scale, both sediment cores contain more C-layers during warmer interstadials compared with colder stadials during Marine Isotope Stage 3. This finding implies that interstadials were not only wetter than stadials, but probably also characterized by increased rainfall variability, leading to an enhanced frequency of flooding events in the hinterland of the Cariaco Basin.

Original languageEnglish (US)
JournalSedimentology
DOIs
StatePublished - Jan 1 2019
Externally publishedYes

Fingerprint

Last Glacial
sea level
basin
interstadial
sediment
climate
marine isotope stage
intertropical convergence zone
lamination
opal
X-ray fluorescence
sedimentary sequence
paleoclimate
interglacial
sediment core
spectrometry
tropical climate
flooding
laser
oscillation

Keywords

  • Cariaco Basin
  • Caribbean Sea
  • flooding events
  • glacial/interglacial climate
  • sea-level oscillations
  • varved marine sediments

ASJC Scopus subject areas

  • Geology
  • Stratigraphy

Cite this

Fingerprint of tropical climate variability and sea level in sediments of the Cariaco Basin during the last glacial period. / Deplazes, Gaudenz; Meckler, Anna Nele; Peterson, Larry C; Hamann, Yvonne; Aeschlimann, Beat; Günther, Detlef; Martínez-García, Alfredo; Haug, Gerald H.

In: Sedimentology, 01.01.2019.

Research output: Contribution to journalArticle

Deplazes, Gaudenz ; Meckler, Anna Nele ; Peterson, Larry C ; Hamann, Yvonne ; Aeschlimann, Beat ; Günther, Detlef ; Martínez-García, Alfredo ; Haug, Gerald H. / Fingerprint of tropical climate variability and sea level in sediments of the Cariaco Basin during the last glacial period. In: Sedimentology. 2019.
@article{68677e3dc69d46e4a6cfadac4ca2d626,
title = "Fingerprint of tropical climate variability and sea level in sediments of the Cariaco Basin during the last glacial period",
abstract = "High-resolution palaeorecords of climate are critical to improving current understanding of climate variability, its sensitivity and impact on the environment in the past and in the future. Sediments from the Cariaco Basin off the coast of Venezuela have proven to be sensitive recorders of tropical palaeoclimate variability down to an annual scale. However, the fingerprint of climate and sea level in the sediments of the last glacial period is still not completely understood. In this study, lamination analysis of sediments from the Cariaco Basin is extended to the last glacial period. Detailed sedimentological and geochemical analysis (laser ablation–inductively coupled plasma–mass spectrometry) reveals couplets of light-coloured, terrigenous-rich and dark-coloured, biogenic opal-rich laminae, which are interpreted to reflect the seasonal migration of the Intertropical Convergence Zone. In addition, a previously undescribed, nearly pure terrigenous lamina type is observed, which is referred to hereafter as a ‘C-layer’. The C-layers in the sedimentary sequence are interpreted as flood layers that originate from local rivers. The occurrence of these C-layers is investigated for two core locations in the Cariaco Basin over the last 110 kyr by continuous X-ray fluorescence scanning. Dansgaard–Oeschger oscillations are most clearly traced by proxies reflecting productivity and marine organic matter content of the sediment. In contrast, the abundance of terrigenous material differs at times between the two sites. On an interglacial to glacial timescale, the ability to record events causing C-layers is likely to be influenced by changes in sea level and source proximity. On a millennial scale, both sediment cores contain more C-layers during warmer interstadials compared with colder stadials during Marine Isotope Stage 3. This finding implies that interstadials were not only wetter than stadials, but probably also characterized by increased rainfall variability, leading to an enhanced frequency of flooding events in the hinterland of the Cariaco Basin.",
keywords = "Cariaco Basin, Caribbean Sea, flooding events, glacial/interglacial climate, sea-level oscillations, varved marine sediments",
author = "Gaudenz Deplazes and Meckler, {Anna Nele} and Peterson, {Larry C} and Yvonne Hamann and Beat Aeschlimann and Detlef G{\"u}nther and Alfredo Mart{\'i}nez-Garc{\'i}a and Haug, {Gerald H.}",
year = "2019",
month = "1",
day = "1",
doi = "10.1111/sed.12567",
language = "English (US)",
journal = "Sedimentology",
issn = "0037-0746",
publisher = "Wiley-Blackwell",

}

TY - JOUR

T1 - Fingerprint of tropical climate variability and sea level in sediments of the Cariaco Basin during the last glacial period

AU - Deplazes, Gaudenz

AU - Meckler, Anna Nele

AU - Peterson, Larry C

AU - Hamann, Yvonne

AU - Aeschlimann, Beat

AU - Günther, Detlef

AU - Martínez-García, Alfredo

AU - Haug, Gerald H.

PY - 2019/1/1

Y1 - 2019/1/1

N2 - High-resolution palaeorecords of climate are critical to improving current understanding of climate variability, its sensitivity and impact on the environment in the past and in the future. Sediments from the Cariaco Basin off the coast of Venezuela have proven to be sensitive recorders of tropical palaeoclimate variability down to an annual scale. However, the fingerprint of climate and sea level in the sediments of the last glacial period is still not completely understood. In this study, lamination analysis of sediments from the Cariaco Basin is extended to the last glacial period. Detailed sedimentological and geochemical analysis (laser ablation–inductively coupled plasma–mass spectrometry) reveals couplets of light-coloured, terrigenous-rich and dark-coloured, biogenic opal-rich laminae, which are interpreted to reflect the seasonal migration of the Intertropical Convergence Zone. In addition, a previously undescribed, nearly pure terrigenous lamina type is observed, which is referred to hereafter as a ‘C-layer’. The C-layers in the sedimentary sequence are interpreted as flood layers that originate from local rivers. The occurrence of these C-layers is investigated for two core locations in the Cariaco Basin over the last 110 kyr by continuous X-ray fluorescence scanning. Dansgaard–Oeschger oscillations are most clearly traced by proxies reflecting productivity and marine organic matter content of the sediment. In contrast, the abundance of terrigenous material differs at times between the two sites. On an interglacial to glacial timescale, the ability to record events causing C-layers is likely to be influenced by changes in sea level and source proximity. On a millennial scale, both sediment cores contain more C-layers during warmer interstadials compared with colder stadials during Marine Isotope Stage 3. This finding implies that interstadials were not only wetter than stadials, but probably also characterized by increased rainfall variability, leading to an enhanced frequency of flooding events in the hinterland of the Cariaco Basin.

AB - High-resolution palaeorecords of climate are critical to improving current understanding of climate variability, its sensitivity and impact on the environment in the past and in the future. Sediments from the Cariaco Basin off the coast of Venezuela have proven to be sensitive recorders of tropical palaeoclimate variability down to an annual scale. However, the fingerprint of climate and sea level in the sediments of the last glacial period is still not completely understood. In this study, lamination analysis of sediments from the Cariaco Basin is extended to the last glacial period. Detailed sedimentological and geochemical analysis (laser ablation–inductively coupled plasma–mass spectrometry) reveals couplets of light-coloured, terrigenous-rich and dark-coloured, biogenic opal-rich laminae, which are interpreted to reflect the seasonal migration of the Intertropical Convergence Zone. In addition, a previously undescribed, nearly pure terrigenous lamina type is observed, which is referred to hereafter as a ‘C-layer’. The C-layers in the sedimentary sequence are interpreted as flood layers that originate from local rivers. The occurrence of these C-layers is investigated for two core locations in the Cariaco Basin over the last 110 kyr by continuous X-ray fluorescence scanning. Dansgaard–Oeschger oscillations are most clearly traced by proxies reflecting productivity and marine organic matter content of the sediment. In contrast, the abundance of terrigenous material differs at times between the two sites. On an interglacial to glacial timescale, the ability to record events causing C-layers is likely to be influenced by changes in sea level and source proximity. On a millennial scale, both sediment cores contain more C-layers during warmer interstadials compared with colder stadials during Marine Isotope Stage 3. This finding implies that interstadials were not only wetter than stadials, but probably also characterized by increased rainfall variability, leading to an enhanced frequency of flooding events in the hinterland of the Cariaco Basin.

KW - Cariaco Basin

KW - Caribbean Sea

KW - flooding events

KW - glacial/interglacial climate

KW - sea-level oscillations

KW - varved marine sediments

UR - http://www.scopus.com/inward/record.url?scp=85061915347&partnerID=8YFLogxK

UR - http://www.scopus.com/inward/citedby.url?scp=85061915347&partnerID=8YFLogxK

U2 - 10.1111/sed.12567

DO - 10.1111/sed.12567

M3 - Article

AN - SCOPUS:85061915347

JO - Sedimentology

JF - Sedimentology

SN - 0037-0746

ER -