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  • Ablabesmyia; AGE; Ceratopogonidae; Chaoborus; Chironomids; Chironomini indeterminata; Chironomus anthracinus-type; Chironomus plumosus-type; Cladopelma lateralis-type; Cladotanytarsus mancus-type; Cladotanytarsus-type A; Corynoneura edwardsi-type; Counting; Counting, microscope; Cricotopus bicinctus-type; Cricotopus cylindraceus-type; Cricotopus laricomalis-type; Cricotopus obnixus-type; CrookedPond_CP1a; Cryptochironomus; Demicryptochironomus; DEPTH, sediment/rock; Dicrotendipes nervosus-type; drought; Einfeldia; Endochironomus albipennis-type; Endochironomus impar-type; Georthocladius; Glyptotendipes barbipes-type; Glyptotendipes severini-type; Guttipelopia; Hand-held piston corer; Heterotrissocladius grimshawi-type; Heterotrissocladius marcidus-type; Heterotrissocladius subpilosus-type; HH_PC; Labrundinia; Lake core; Lauterborniella/Zavreliella; Limnophyes; Micropsectra insignilobus-type; Microtendipes pedellus-type; Nanocladius; Nilothauma; Oliveridia; ORDINAL NUMBER; Orthocladiinae indeterminata; Pagastiella; Parachironomus varus-type; Parakiefferiella bathophila-type; Parakiefferiella-type A; Parametriocnemus/Paraphaenocladius; Paratanytarsus penicillatus-type; Paratendipes albimanus-type; Paratendipes nudisquama-type; Polypedilum nubeculosum-type; Procladius; Psectrocladius calcaratus-type; Psectrocladius flavus-type; Psectrocladius sordidellus-type; Pseudochironomus; Pseudosmittia; Stempellina; Stempellinella/Zavrelia; Stenochironomus; Stictochironomus rosenschoeldi-type; Synorthocladius; Tanypodinae indeterminata; Tanytarsini indeterminata; Tanytarsus glabrescens-type; Tanytarsus indeterminata; Tanytarsus lugens-type; Tanytarsus mendax-type; Tanytarsus pallidicornis-type; Thienemanniella; Thienemannimyia; Tribelos; United States; Unniella; Xenochironomus; Zalutschia-type B; Zalutschia zalutschicola  (1)
  • Sea surface temperature  (1)
Document type
Keywords
  • Ablabesmyia; AGE; Ceratopogonidae; Chaoborus; Chironomids; Chironomini indeterminata; Chironomus anthracinus-type; Chironomus plumosus-type; Cladopelma lateralis-type; Cladotanytarsus mancus-type; Cladotanytarsus-type A; Corynoneura edwardsi-type; Counting; Counting, microscope; Cricotopus bicinctus-type; Cricotopus cylindraceus-type; Cricotopus laricomalis-type; Cricotopus obnixus-type; CrookedPond_CP1a; Cryptochironomus; Demicryptochironomus; DEPTH, sediment/rock; Dicrotendipes nervosus-type; drought; Einfeldia; Endochironomus albipennis-type; Endochironomus impar-type; Georthocladius; Glyptotendipes barbipes-type; Glyptotendipes severini-type; Guttipelopia; Hand-held piston corer; Heterotrissocladius grimshawi-type; Heterotrissocladius marcidus-type; Heterotrissocladius subpilosus-type; HH_PC; Labrundinia; Lake core; Lauterborniella/Zavreliella; Limnophyes; Micropsectra insignilobus-type; Microtendipes pedellus-type; Nanocladius; Nilothauma; Oliveridia; ORDINAL NUMBER; Orthocladiinae indeterminata; Pagastiella; Parachironomus varus-type; Parakiefferiella bathophila-type; Parakiefferiella-type A; Parametriocnemus/Paraphaenocladius; Paratanytarsus penicillatus-type; Paratendipes albimanus-type; Paratendipes nudisquama-type; Polypedilum nubeculosum-type; Procladius; Psectrocladius calcaratus-type; Psectrocladius flavus-type; Psectrocladius sordidellus-type; Pseudochironomus; Pseudosmittia; Stempellina; Stempellinella/Zavrelia; Stenochironomus; Stictochironomus rosenschoeldi-type; Synorthocladius; Tanypodinae indeterminata; Tanytarsini indeterminata; Tanytarsus glabrescens-type; Tanytarsus indeterminata; Tanytarsus lugens-type; Tanytarsus mendax-type; Tanytarsus pallidicornis-type; Thienemanniella; Thienemannimyia; Tribelos; United States; Unniella; Xenochironomus; Zalutschia-type B; Zalutschia zalutschicola  (1)
  • Sea surface temperature  (1)
  • Holocene  (3)
  • Climate change  (1)
  • Common era  (1)
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Years
  • 1
    Publication Date: 2024-04-17
    Description: This dataset provides chironomid counts for the Holocene sediment sequence retrieved from Crooked Pond (United States). Sediment cores were retrieved from the lake using a 1-m long handheld piston corer deployed from a floating coring platform during field work in May 2009. Volumetric samples were obtained from splits of the core and processed in the laboratory (University of New Brunswick, Canada) using standard protocols. Chironomid counts are presented against both depth (cm) and age (cal yr. BP). A total of 58 downcore 1-cm-thick samples were analysed, ranging between 477.5cm depth (9056 cal yr BP) and 0.5cm depth (the present). The chironomid record provides information about changes in the chironomid fauna as well as in within-lake conditions. The dataset was produced to inform on the exact age and duration of a major lake-level lowstand during the mid-Holocene. This lowstand was compared to palynological transitions determined on pollen samples from an older core sequence derived from the same coring location.
    Keywords: Ablabesmyia; AGE; Ceratopogonidae; Chaoborus; Chironomids; Chironomini indeterminata; Chironomus anthracinus-type; Chironomus plumosus-type; Cladopelma lateralis-type; Cladotanytarsus mancus-type; Cladotanytarsus-type A; Corynoneura edwardsi-type; Counting; Counting, microscope; Cricotopus bicinctus-type; Cricotopus cylindraceus-type; Cricotopus laricomalis-type; Cricotopus obnixus-type; CrookedPond_CP1a; Cryptochironomus; Demicryptochironomus; DEPTH, sediment/rock; Dicrotendipes nervosus-type; drought; Einfeldia; Endochironomus albipennis-type; Endochironomus impar-type; Georthocladius; Glyptotendipes barbipes-type; Glyptotendipes severini-type; Guttipelopia; Hand-held piston corer; Heterotrissocladius grimshawi-type; Heterotrissocladius marcidus-type; Heterotrissocladius subpilosus-type; HH_PC; Labrundinia; Lake core; Lauterborniella/Zavreliella; Limnophyes; Micropsectra insignilobus-type; Microtendipes pedellus-type; Nanocladius; Nilothauma; Oliveridia; ORDINAL NUMBER; Orthocladiinae indeterminata; Pagastiella; Parachironomus varus-type; Parakiefferiella bathophila-type; Parakiefferiella-type A; Parametriocnemus/Paraphaenocladius; Paratanytarsus penicillatus-type; Paratendipes albimanus-type; Paratendipes nudisquama-type; Polypedilum nubeculosum-type; Procladius; Psectrocladius calcaratus-type; Psectrocladius flavus-type; Psectrocladius sordidellus-type; Pseudochironomus; Pseudosmittia; Stempellina; Stempellinella/Zavrelia; Stenochironomus; Stictochironomus rosenschoeldi-type; Synorthocladius; Tanypodinae indeterminata; Tanytarsini indeterminata; Tanytarsus glabrescens-type; Tanytarsus indeterminata; Tanytarsus lugens-type; Tanytarsus mendax-type; Tanytarsus pallidicornis-type; Thienemanniella; Thienemannimyia; Tribelos; United States; Unniella; Xenochironomus; Zalutschia-type B; Zalutschia zalutschicola
    Type: Dataset
    Format: text/tab-separated-values, 4060 data points
    Location Call Number Limitation Availability
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  • 2
    Publication Date: 2022-05-25
    Description: © The Author(s), 2015. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Earth's Future 3 (2015): 49–65, doi:10.1002/2014EF000274.
    Description: How climate controls hurricane variability has critical implications for society is not well understood. In part, our understanding is hampered by the short and incomplete observational hurricane record. Here we present a synthesis of intense-hurricane activity from the western North Atlantic over the past two millennia, which is supported by a new, exceptionally well-resolved record from Salt Pond, Massachusetts (USA). At Salt Pond, three coarse grained event beds deposited in the historical interval are consistent with severe hurricanes in 1991 (Bob), 1675, and 1635 C.E., and provide modern analogs for 32 other prehistoric event beds. Two intervals of heightened frequency of event bed deposition between 1400 and 1675 C.E. (10 events) and 150 and 1150 C.E. (23 events), represent the local expression of coherent regional patterns in intense-hurricane–induced event beds. Our synthesis indicates that much of the western North Atlantic appears to have been active between 250 and 1150 C.E., with high levels of activity persisting in the Caribbean and Gulf of Mexico until 1400 C.E. This interval was one with relatively warm sea surface temperatures (SSTs) in the main development region (MDR). A shift in activity to the North American east coast occurred ca. 1400 C.E., with more frequent severe hurricane strikes recorded from The Bahamas to New England between 1400 and 1675 C.E. A warm SST anomaly along the western North Atlantic, rather than within the MDR, likely contributed to the later active interval being restricted to the east coast.
    Description: Funding was provided by US National Science Foundation (awards 0903020 and 1356708), the Risk Prediction Initiative at the Bermuda Institute for Ocean Sciences (BIOS), US Department of Energy National Institute for Climate Change Research, National Oceanic and Atmospheric Administration (award NA11OAR431010), and the Dalio Explore Fund.
    Keywords: Tropical cyclones ; Climate change ; Holocene ; Common era ; Sea surface temperature
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Format: application/pdf
    Location Call Number Limitation Availability
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